{"pageNumber":"5935","pageRowStart":"148350","pageSize":"25","recordCount":184563,"records":[{"id":70233074,"text":"70233074 - 1977 - Mercury in oil shale from the mahogany zone of the Green River formation, eastern Utah and western Colorado","interactions":[],"lastModifiedDate":"2022-07-15T16:14:25.497854","indexId":"70233074","displayToPublicDate":"1977-03-01T11:06:46","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Mercury in oil shale from the mahogany zone of the Green River formation, eastern Utah and western Colorado","docAbstract":"<p>Mercury has been reported in concentrations as high as 4 parts per million from oil shale in the Green River Formation near the Federal oil-shale prototype lease-tracts U-a and U-b in eastern Utah. This high concentration of mercury if present throughout a minable zone, would be of concern in commercial oil-shale operations processing large volumes of shale. Using an improved analytical method, surface samples from eastern Utah previously reported to contain high concentrations of mercury were reanalyzed, and an additional 183 drill core samples from the Mahogany zone and adjacent beds were analyzed. The reanalyzed samples averaged slightly more than 0.35 ppm mercury and the drill-core samples averaged 0.37 ppm. The products from a Fischer assay of 100-gram sample of oil shale, found to yield 35 gallons pier ton of oil and 43 ppm of mercury, were analyzed for their mercury content. The spent shale contained only 2 percent of the total mercury in the assay products and the gas fraction contained about 58 percent. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Donnell, J., and Shaw, V.E., 1977, Mercury in oil shale from the mahogany zone of the Green River formation, eastern Utah and western Colorado: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 221-226.","productDescription":"6 p.","startPage":"221","endPage":"226","costCenters":[],"links":[{"id":403821,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403820,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Green River Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.7314453125,\n              39.29179704377487\n            ],\n            [\n              -107.3638916015625,\n              39.29179704377487\n            ],\n            [\n              -107.3638916015625,\n              41.025499378313754\n            ],\n            [\n              -109.7314453125,\n              41.025499378313754\n            ],\n            [\n              -109.7314453125,\n              39.29179704377487\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Donnell, John R.","contributorId":84330,"corporation":false,"usgs":true,"family":"Donnell","given":"John R.","affiliations":[],"preferred":false,"id":846685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, Van E.","contributorId":146896,"corporation":false,"usgs":true,"family":"Shaw","given":"Van","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":846686,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232982,"text":"70232982 - 1977 - Land use and land cover changes: A framework for monitoring","interactions":[],"lastModifiedDate":"2022-07-14T15:46:14.365889","indexId":"70232982","displayToPublicDate":"1977-03-01T10:40:44","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Land use and land cover changes: A framework for monitoring","docAbstract":"<p>Information on the rate and kind of change in the use of land resources is essential to-the proper planning, management, and regulation of the use of such resources. Starting in 1975, the U.S. Geological Survey has been engaged in mapping and inventory of land use and land cover at a scale of 1:250000 with plans to change to new 1:100000 base maps as they become available. Such scales are-appropriate for acquiring benchmark or baseline data on land use and land cover on a nationwide basis with a reasonable degree of standardization and accuracy, within a practical time frame of 6 to 7 years, and at a reasonable level of detail in categorization. Changes in land use and land cover occur at highly variable rates from place to place. Thus variations, in the intervals between updates of land use and land cover data should be carefully evaluated in order to provide an appropriate frame of reference for the systematic updating of such data. A methodological framework is needed for monitoring changes in land use and land cover that will be timely, relatively inexpensive, and appropriate for widely varying needs at national, interstate-regional, state, multicounty, county, and city levels. In this article a partial framework for monitoring land use and land cover changes is provided with opportunity to extend its use to greater levels of detail in categorization and shorter intervals of frequency when needed for selected areas.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Anderson, J.R., 1977, Land use and land cover changes: A framework for monitoring: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 143-153.","productDescription":"11 p.","startPage":"143","endPage":"153","costCenters":[],"links":[{"id":403766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403765,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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States\"}}]}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Anderson, James R.","contributorId":20213,"corporation":false,"usgs":true,"family":"Anderson","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":846613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233061,"text":"70233061 - 1977 - Blades of olivine in ultramafic rock from northern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2022-07-15T16:05:59.833213","indexId":"70233061","displayToPublicDate":"1977-03-01T10:37:53","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Blades of olivine in ultramafic rock from northern Sierra Nevada, California","docAbstract":"<p>Blades of olivine in random arrangement crystallized in a small body of serpentine just north of the Grizzly pluton as a result of contact metamorphism. Interstitial minerals are talc, chlorite, and minor amount of cummingtonite.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Hietanen, A., 1977, Blades of olivine in ultramafic rock from northern Sierra Nevada, California: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 217-219.","productDescription":"3 p.","startPage":"217","endPage":"219","costCenters":[],"links":[{"id":403818,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403809,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Rock Creek, Sierra Nevada, Spring Valley Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.41875267028809,\n              39.989549903780365\n            ],\n            [\n              -121.35764122009277,\n              39.989549903780365\n            ],\n            [\n              -121.35764122009277,\n              40.01525729596965\n            ],\n            [\n              -121.41875267028809,\n              40.01525729596965\n            ],\n            [\n              -121.41875267028809,\n              39.989549903780365\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hietanen, Anna","contributorId":43841,"corporation":false,"usgs":true,"family":"Hietanen","given":"Anna","affiliations":[],"preferred":false,"id":846679,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233059,"text":"70233059 - 1977 - Pleistocene fishes from Alameda County, California","interactions":[],"lastModifiedDate":"2022-07-15T15:36:36.362775","indexId":"70233059","displayToPublicDate":"1977-03-01T10:27:50","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Pleistocene fishes from Alameda County, California","docAbstract":"<p> Six types of freshwater fishes were recovered from an early Pleistocene (Irvingtonian) locality on the east side of San Francisco Bay, Alameda County, Calif. The fauna includes one centrarchid, one salmonid, three cyprinids, and one catostomid. The fauna indicates fluvial and slow-moving or lacustrine aquatic environments. One of the cyprinids and the catostomid are assigned to provisional genera because of the inadequate amount of material available for study and the obvious differences between these fossils and known fossil or recent fishes. They are new additions to the Pleistocene fish fauna of California. Paleogeographic distribution of some of these fishes indicates former fluvial or lacustrine connections between Utah, Idaho, Oregon, Washington, Nevada, and California. The Pliocene and Pleistocene fossil fish faunas indicate the widespread occurrence of genera now endemic to California. A similar picture is presented by the molluscan evidence. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Casteel, R.W., and Adam, D.P., 1977, Pleistocene fishes from Alameda County, California: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 209-215.","productDescription":"7 p.","startPage":"209","endPage":"215","costCenters":[],"links":[{"id":403806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403805,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Alameda 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Richard W.","contributorId":28241,"corporation":false,"usgs":true,"family":"Casteel","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":846674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adam, David P.","contributorId":36132,"corporation":false,"usgs":true,"family":"Adam","given":"David","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":846675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70233055,"text":"70233055 - 1977 - Electrical soundings near Yellow Creek, Rio Blanco County, Colorado","interactions":[],"lastModifiedDate":"2022-07-15T15:24:19.929894","indexId":"70233055","displayToPublicDate":"1977-03-01T10:15:21","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Electrical soundings near Yellow Creek, Rio Blanco County, Colorado","docAbstract":"<p>Ten vertical electrical soundings were made in the Piceance Creek Basin in October 1974-5 along Yellow Creek, 2 in Big Duck Creek, and 1 each along Corral Gulch, on the hill in sec. 20, 1 kilometre northwest of 84 Ranch, and along the White River between the mouths of Yellow and Piceance Creeks. Interpretations of these soundings indicate that the anisotropy of the upper oil shales decreases from 2 in the basin center to 1 at a location on its flank. This decrease could result from a greater number of vertical water-filled fractures in the upper shales near the edge of the basin. On the other hand, the anisotropy coefficient for the lower shales increases from 2 to around 9 along the same section, indicating the presence of an increasing number of isolated horizontal aquifers in the lower shales on the basin flank. It is speculated that this trend for the lower shales reverses nearer the basin edge in the area of recharge of these splintered horizontal aquifers.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Campbell, D.L., 1977, Electrical soundings near Yellow Creek, Rio Blanco County, Colorado: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 193-205.","productDescription":"13 p.","startPage":"193","endPage":"205","costCenters":[],"links":[{"id":403804,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403803,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Rio Blanco County","otherGeospatial":"Yellow Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.74542236328125,\n              39.6437675734185\n            ],\n            [\n              -108.18923950195312,\n              39.6437675734185\n            ],\n            [\n              -108.18923950195312,\n              40.23026664265011\n            ],\n            [\n              -108.74542236328125,\n              40.23026664265011\n            ],\n            [\n              -108.74542236328125,\n              39.6437675734185\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Campbell, David L.","contributorId":95447,"corporation":false,"usgs":true,"family":"Campbell","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":846673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233051,"text":"70233051 - 1977 - Geology and Rb-Sr age of Precambrian W Puritan Quartz Monzonite, northern Michigan","interactions":[],"lastModifiedDate":"2022-07-15T15:13:40.019423","indexId":"70233051","displayToPublicDate":"1977-03-01T10:01:07","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Geology and Rb-Sr age of Precambrian W Puritan Quartz Monzonite, northern Michigan","docAbstract":"<p>The Puritan Quartz Monzonite, in the western part of the Upper Peninsula of Michigan, composes a batholith at least 50 kilometres long and as much as 20 km wide on the south side of the Gogebic iron range. It is associated with subaqueous metavolcanic rocks assigned to the Precambrian W Ramsey Formation and with a complex gneissic unit of the same age. The quartz monzonite has a Rb-Sr isochron age of 2,710±140 million years and an initial <sup>87</sup>Sr/<sup>86</sup>Sr of 0.7015±0.0017. The scatter of data points in excess of analytical error is interpreted as indicating that minor cataclasis and retrograde metamorphism produced slight open-system behavior in Precambrian X (circa 1,800 m.y.) time. The Puritan Quartz Monzonite and associated volcanic rocks are equated with similar Precambrian W greenstone-granite complexes in northern Minnesota, and clearly are a part of the Precambrian W greenstone terrane, as defined previously for the Lake Superior region.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Sims, P., Peterman, Z.E., and Prinz, W.C., 1977, Geology and Rb-Sr age of Precambrian W Puritan Quartz Monzonite, northern Michigan: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 185-192.","productDescription":"8 p.","startPage":"185","endPage":"192","costCenters":[],"links":[{"id":403801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403800,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"Gogebic iron range, Lake Gogebic, Upper Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.53994750976562,\n              46.40093514439044\n            ],\n            [\n              -89.5111083984375,\n              46.44069599413034\n            ],\n            [\n              -89.52621459960938,\n              46.49082901981415\n            ],\n            [\n              -89.59075927734375,\n              46.5635815342227\n            ],\n            [\n              -89.53445434570312,\n              46.580574564531695\n            ],\n            [\n              -89.53994750976562,\n              46.60228013300284\n            ],\n            [\n              -89.89700317382812,\n              46.76620587423741\n            ],\n            [\n              -89.9945068359375,\n              46.707852594536355\n            ],\n            [\n              -90.03570556640624,\n              46.677710064644344\n            ],\n            [\n              -90.21560668945311,\n              46.638122462379656\n            ],\n            [\n              -90.30624389648438,\n              46.6088844501943\n            ],\n            [\n              -90.3350830078125,\n              46.612657984230204\n            ],\n            [\n              -90.42022705078125,\n              46.565469911631475\n            ],\n            [\n              -90.41473388671875,\n              46.34123949998618\n            ],\n            [\n              -90.11672973632812,\n              46.334602622976156\n            ],\n            [\n              -89.54544067382812,\n              46.22735299655779\n            ],\n            [\n              -89.53994750976562,\n              46.40093514439044\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":846670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":167699,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell","email":"peterman@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":846671,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prinz, W. C.","contributorId":82670,"corporation":false,"usgs":true,"family":"Prinz","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":846672,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70233046,"text":"70233046 - 1977 - Metamorphic rocks of the Yakutat-St. Elias area, south-central Alaska","interactions":[],"lastModifiedDate":"2022-07-15T14:59:28.258206","indexId":"70233046","displayToPublicDate":"1977-03-01T09:51:22","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Metamorphic rocks of the Yakutat-St. Elias area, south-central Alaska","docAbstract":"<p>Metamorphic rocks in the Yakutat-St. Elias area range in grade from zeolite to amphibolite facies. Radiometric age determinations on selected metamorphic rocks have helped to identify two major metamorphic events, one in Late Cretaceous time that was characterized by penetrative deformation, and one in the Miocene Epoch that resulted in widespread recrystallization and igneous intrusions. Mapped facies units show many discontinuities across major faults, and their distribution indicates major differential uplift between several structurally bound crustal blocks within a strongly deformed mobile belt west of the Art Lewis fault. Late Cretaceous metamorphic gradients indicate that the blocks have been tilted to the west or northwest parallel to their general structural grain. As mineral assemblages that were recrystallized during Miocene time occur on both sides of the Fairweather fault, large-scale, post-Miocene strike-slip movement along the fault is not indicated.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Hudson, T., Plafker, G., and Turner, D.L., 1977, Metamorphic rocks of the Yakutat-St. Elias area, south-central Alaska: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 173-184.","productDescription":"12 p.","startPage":"173","endPage":"184","costCenters":[],"links":[{"id":403799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403797,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"St. Elias, Yakutat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -141.0205078125,\n              60.32150850738404\n            ],\n            [\n              -141.13037109375,\n              59.772991625706695\n            ],\n            [\n              -140.745849609375,\n              59.701013531997326\n            ],\n            [\n              -140.3173828125,\n              59.68438118751815\n            ],\n            [\n              -139.74609375,\n              59.81168490365651\n            ],\n            [\n              -139.74609375,\n              59.85033331585688\n            ],\n            [\n              -139.70214843749997,\n              59.9054675732672\n            ],\n            [\n              -139.6142578125,\n              59.7619281579702\n            ],\n            [\n              -139.647216796875,\n              59.62332522313024\n            ],\n            [\n              -139.76806640625,\n              59.567723306212955\n            ],\n            [\n              -139.866943359375,\n              59.52317553544798\n            ],\n            [\n              -139.306640625,\n              59.338792483494494\n            ],\n            [\n              -138.746337890625,\n              59.147769484619786\n            ],\n            [\n              -138.482666015625,\n              59.085738569819505\n            ],\n            [\n              -137.999267578125,\n              58.90464570302001\n            ],\n            [\n              -137.999267578125,\n              59.439489583059725\n            ],\n            [\n              -138.66943359375,\n              59.81168490365651\n            ],\n            [\n              -138.702392578125,\n              59.91097597079679\n            ],\n            [\n              -139.075927734375,\n              60.01546201341472\n            ],\n            [\n              -139.19677734375,\n              60.10319489936693\n            ],\n            [\n              -139.06494140625,\n              60.354130331374286\n            ],\n            [\n              -139.70214843749997,\n              60.343260013555195\n            ],\n            [\n              -139.98779296875,\n              60.19615576604439\n            ],\n            [\n              -140.47119140625,\n              60.32150850738404\n            ],\n            [\n              -140.537109375,\n              60.23435742267943\n            ],\n            [\n              -141.0205078125,\n              60.32150850738404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":846666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":846667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, Donald L.","contributorId":11604,"corporation":false,"usgs":true,"family":"Turner","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":846668,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70233036,"text":"70233036 - 1977 - Intrusive rocks of the Yakutat-St. Elias area, south-central Alaska","interactions":[],"lastModifiedDate":"2022-07-15T14:35:17.066585","indexId":"70233036","displayToPublicDate":"1977-03-01T09:23:16","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Intrusive rocks of the Yakutat-St. Elias area, south-central Alaska","docAbstract":"<p>Twenty-three plutons, exposed over a total area of nearly 1200 km<sup>2</sup>, have been studied in the Alaska part of the St. Elias Mountains between long 138° and 141°W. Results of potassium-argon age determinations combined with field relations, petrography, and major- and trace-element chemistry suggest six major intrusive events: (1) late Paleozoic gabbro to quartz diorite intruded Paleozoic metamorphic rocks that are probably equivalent to the Kaskawulsh Group in adjacent areas of Canada, (2) Triassic quartz diorite formed one small pluton in undated metamorphic rocks near Mt. St. Elias, (3) Jurassic tonalite and granite intruded upper Paleozoic(?) and lower Mesozoic(?) metamorphic rocks, (4) Late Cretaceous or Tertiary altered tonalite formed three widely separated plutons in metasedimentary rocks of Jurassic(?) and Cretaceous age in the Yakutat Group, (5) Eocene granodiorite and granite, and (6) late Cenozoic tonalite and granodiorite intruded both the Yakutat Group and upper Paleozoic(?) and lower Mesozoic(?) metamorphic rocks. The Paleozoic, Jurassic, and Cretaceous or Tertiary plutonic suites are restricted to particular geologic terranes, and the Jurassic and Eocene suites correlate with regional plutonic belts present elsewhere in southern Alaska. The distribution of the Tertiary plutons does not require large-scale horizontal displacements along the Fairweather and other major high-angle faults. The available data indicate that the mineral resource potential of the Yakutat-St. Elias area is low for those deposits that are generally related to magmatic processes. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Hudson, T., Plafker, G., and Lanphere, M.A., 1977, Intrusive rocks of the Yakutat-St. Elias area, south-central Alaska: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 155-172.","productDescription":"18 p.","startPage":"155","endPage":"172","costCenters":[],"links":[{"id":403791,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403789,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"St. Elias, Yakutat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -141.0205078125,\n              60.32150850738404\n            ],\n            [\n              -141.13037109375,\n              59.772991625706695\n            ],\n            [\n              -140.745849609375,\n              59.701013531997326\n            ],\n            [\n              -140.3173828125,\n              59.68438118751815\n            ],\n            [\n              -139.74609375,\n              59.81168490365651\n            ],\n            [\n              -139.74609375,\n              59.85033331585688\n            ],\n            [\n              -139.70214843749997,\n              59.9054675732672\n            ],\n            [\n              -139.6142578125,\n              59.7619281579702\n            ],\n            [\n              -139.647216796875,\n              59.62332522313024\n            ],\n            [\n              -139.76806640625,\n              59.567723306212955\n            ],\n            [\n              -139.866943359375,\n              59.52317553544798\n            ],\n            [\n              -139.306640625,\n              59.338792483494494\n            ],\n            [\n              -138.746337890625,\n              59.147769484619786\n            ],\n            [\n              -138.482666015625,\n              59.085738569819505\n            ],\n            [\n              -137.999267578125,\n              58.90464570302001\n            ],\n            [\n              -137.999267578125,\n              59.439489583059725\n            ],\n            [\n              -138.66943359375,\n              59.81168490365651\n            ],\n            [\n              -138.702392578125,\n              59.91097597079679\n            ],\n            [\n              -139.075927734375,\n              60.01546201341472\n            ],\n            [\n              -139.19677734375,\n              60.10319489936693\n            ],\n            [\n              -139.06494140625,\n              60.354130331374286\n            ],\n            [\n              -139.70214843749997,\n              60.343260013555195\n            ],\n            [\n              -139.98779296875,\n              60.19615576604439\n            ],\n            [\n              -140.47119140625,\n              60.32150850738404\n            ],\n            [\n              -140.537109375,\n              60.23435742267943\n            ],\n            [\n              -141.0205078125,\n              60.32150850738404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":846657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":846658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":846659,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009955,"text":"70009955 - 1977 - Delaware River: Evidence for its former extension to Wilmington Submarine Canyon","interactions":[],"lastModifiedDate":"2026-01-16T16:29:17.544502","indexId":"70009955","displayToPublicDate":"1977-02-04T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Delaware River: Evidence for its former extension to Wilmington Submarine Canyon","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Seismic-reflection profiles indicate that during the Pleistocene the Delaware River flowed across the continental shelf east of Delaware Bay and emptied into Wilmington Submarine Canyon. The ancestral valley (width, 3 to 8 kilometers; relief, 10 to 30 meters) is buried, is not reflected in the surface topography, and probably predates the formation of the present canyon head.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.195.4277.483","issn":"00368075","usgsCitation":"Twichell, D., Knebel, H., and Folger, D.W., 1977, Delaware River: Evidence for its former extension to Wilmington Submarine Canyon: Science, v. 195, no. 4277, p. 483-485, https://doi.org/10.1126/science.195.4277.483.","productDescription":"3 p.","startPage":"483","endPage":"485","costCenters":[],"links":[{"id":219204,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Delaware","otherGeospatial":"Delaware Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.77418738436643,\n              39.7369030436918\n            ],\n            [\n              -75.77418738436643,\n              38.43058282173703\n            ],\n            [\n              -74.88970281894306,\n              38.43058282173703\n            ],\n            [\n              -74.88970281894306,\n              39.7369030436918\n            ],\n            [\n              -75.77418738436643,\n              39.7369030436918\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"195","issue":"4277","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe5be4b0c8380cd4ecc6","contributors":{"authors":[{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":357520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knebel, H.J.","contributorId":79092,"corporation":false,"usgs":true,"family":"Knebel","given":"H.J.","affiliations":[],"preferred":false,"id":357519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Folger, D. W.","contributorId":97126,"corporation":false,"usgs":true,"family":"Folger","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":357521,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70200642,"text":"70200642 - 1977 - High temperature heat content and heat capacity of silicate glasses:  experimental determination and a model for calculation","interactions":[],"lastModifiedDate":"2018-10-25T14:21:11","indexId":"70200642","displayToPublicDate":"1977-02-01T14:20:32","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"High temperature heat content and heat capacity of silicate glasses:  experimental determination and a model for calculation","docAbstract":"<p>Knowledge of the thermodynamic properties of silicate melts is fundamental to quantitative characterization of igneous systems. This paper presents new data on one of these properties, heat content, for silicate glasses and supercooled silicate liquids and derives partial molar heat contents for the glasses. The high temperature heat contents of two FeO-rich synthetic silicate glasses and five glasses and three supercooled liquids prepared from igneous rocks ranging from basalt to rhyolite were measured by drop calorimetry. Heat capacities of silicate liquids and the change in heat capacity at the glass transformation are discussed. <br></p>","language":"English","doi":"10.2475/ajs.277.2.109","usgsCitation":"Bacon, C.R., 1977, High temperature heat content and heat capacity of silicate glasses:  experimental determination and a model for calculation: American Journal of Science, v. 277, no. 2, p. 109-135, https://doi.org/10.2475/ajs.277.2.109.","productDescription":"27 p.","startPage":"109","endPage":"135","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":480617,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.2475/ajs.277.2.109","text":"External Repository"},{"id":358825,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"277","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bacon, Charles R. 0000-0002-2165-5618 cbacon@usgs.gov","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":2909,"corporation":false,"usgs":true,"family":"Bacon","given":"Charles","email":"cbacon@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":749831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233962,"text":"70233962 - 1977 - Reflection and refraction of type-II S waves in elastic and anelastic media","interactions":[],"lastModifiedDate":"2022-07-28T13:33:48.462327","indexId":"70233962","displayToPublicDate":"1977-02-01T08:29:23","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7571,"text":"Bulletin of Seismological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Reflection and refraction of type-II S waves in elastic and anelastic media","docAbstract":"<p>The general theory of viscoelasticity, which accounts for elastic as well as anelastic linear behavior of materials, predicts that two types of&nbsp;<i>S</i>&nbsp;waves propagate in anelastic earth materials. The particle motion for an inhomogeneous plane&nbsp;<i>S</i>&nbsp;wave of type I is elliptical in the plane defined by the directions of propagation and attenuation, while the particle motion for an inhomogeneous plane&nbsp;<i>S</i>&nbsp;wave of type II is linear perpendicular to this plane. The general theory predicts that an&nbsp;<i>S</i>-wave incident upon a plane boundary perpendicular to the plane defined by the directions of propagation and attenuation generates&nbsp;<i>S</i>&nbsp;waves only of the same type. General characteristics of the type-II&nbsp;<i>S</i> waves reflected and refracted at plane anelastic boundaries are:</p><p>(a) velocities and maximum attenuations which depend on the angle of incidence and frequency,</p><p>(b) maximum energy flow at a different velocity and in a different direction than phase propagation,</p><p>(c) energy flow across the boundary due to interaction of the incident and reflected waves.</p><p>The general theory predicts these characteristics for the waves whenever a plane type-II&nbsp;<i>S</i>&nbsp;wave interacts with a plane anelastic boundary such as a soil-bedrock, crust-mantle, or core-mantle interface. None of these characteristics are predicted for the plane&nbsp;<i>SH</i>&nbsp;waves described by elasticity theory.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0670010043","usgsCitation":"Borcherdt, R.D., 1977, Reflection and refraction of type-II S waves in elastic and anelastic media: Bulletin of Seismological Society of America, v. 67, no. 1, p. 43-67, https://doi.org/10.1785/BSSA0670010043.","productDescription":"25 p.","startPage":"43","endPage":"67","costCenters":[],"links":[{"id":404537,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"1","noUsgsAuthors":false,"publicationDate":"1977-02-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":847753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014096,"text":"1014096 - 1977 - A new host for Pleistophora ovariae (Microsporida)","interactions":[],"lastModifiedDate":"2025-04-30T16:46:00.307974","indexId":"1014096","displayToPublicDate":"1977-02-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"A new host for Pleistophora ovariae (Microsporida)","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Allen Press","doi":"10.2307/3280131","usgsCitation":"Nagel, M., and Hoffman, G.L., 1977, A new host for Pleistophora ovariae (Microsporida): Journal of Parasitology, v. 63, no. 1, p. 160-162, https://doi.org/10.2307/3280131.","productDescription":"3 p.","startPage":"160","endPage":"162","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129579,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -93.71886924701124,\n              38.21707405441765\n            ],\n            [\n              -93.71886924701124,\n              38.01677745033331\n            ],\n            [\n              -93.22851637945013,\n              38.116981579409384\n            ],\n            [\n              -92.60145591442377,\n              38.01677745033331\n            ],\n            [\n              -92.60145591442377,\n              38.21707405441765\n            ],\n            [\n              -93.1719550805126,\n              38.29853798647787\n            ],\n            [\n              -93.71886924701124,\n              38.21707405441765\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.60877016070945,\n              36.49683346433352\n            ],\n            [\n              -94.46299084589886,\n              35.31175006694599\n            ],\n            [\n              -94.60877016070945,\n              32.97770683603406\n            ],\n            [\n              -91.03596143698991,\n              32.98536507540483\n            ],\n            [\n              -90.79442609239385,\n              33.9672727871569\n            ],\n            [\n              -90.06981486394116,\n              35.30430729339946\n            ],\n            [\n              -89.75080285062971,\n              35.99297747345833\n            ],\n            [\n              -90.3751487519523,\n              36.02777812812913\n            ],\n            [\n              -90.10626391024843,\n              36.460196165165016\n            ],\n            [\n              -94.60877016070945,\n              36.49683346433352\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ac142","contributors":{"authors":[{"text":"Nagel, M.L.","contributorId":56181,"corporation":false,"usgs":true,"family":"Nagel","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":319780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319781,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208057,"text":"70208057 - 1977 - Composition of Pacific Ocean ferromanganese nodules","interactions":[],"lastModifiedDate":"2020-01-25T10:59:31","indexId":"70208057","displayToPublicDate":"1977-01-25T10:53:34","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Composition of Pacific Ocean ferromanganese nodules","docAbstract":"<p><span>Bulk composition of ferromanganese nodules from the pelagic environment of the Pacific Ocean is apparently related to nodule-growth rate, sediment-accumulation rate, and biologic productivity in the overlying seawater. Nodules with a high&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Mn</mtext><mtext>Fe</mtext></math>\"><span class=\"MJX_Assistive_MathML\">MnFe</span></span></span><span>&nbsp;ratio and high Ni and Cu concentrations tend to occur in areas where primary productivity in the surface layer of the ocean is high and the sediment-accumulation rate low. Nodules with a low&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Mn</mtext><mtext>Fe</mtext></math>\"><span class=\"MJX_Assistive_MathML\">MnFe</span></span></span><span>&nbsp;ratio and low Ni and Cu concentrations occur in areas either where sediment-accumulation rate is high or biologic productivity is low. They may have a&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Mn</mtext><mtext>Fe</mtext></math>\"><span class=\"MJX_Assistive_MathML\">MnFe</span></span></span><span>&nbsp;ratio as low as one and accrete at rates as low as&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>1</mtext><mtext>mm</mtext><mtext>10</mtext><msup><mi></mi><mn>6</mn></msup><mtext>yrs</mtext></math>\"><span class=\"MJX_Assistive_MathML\">1mm106yrs</span></span></span><span>. Nodules with a larger&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Mn</mtext><mtext>Fe</mtext></math>\"><span class=\"MJX_Assistive_MathML\">MnFe</span></span></span><span>&nbsp;ratio apparently have growth rates that are greater by as much as a factor of 10.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(77)90036-6","usgsCitation":"Piper, D.Z., and Williamson, M., 1977, Composition of Pacific Ocean ferromanganese nodules: Marine Geology, v. 23, no. 4, p. 285-303, https://doi.org/10.1016/0025-3227(77)90036-6.","productDescription":"46","startPage":"285","endPage":"303","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":371550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Pacific Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -223.2421875,\n              29.53522956294847\n            ],\n            [\n              -224.296875,\n              11.867350911459308\n            ],\n            [\n              -204.609375,\n              0.3515602939922709\n            ],\n            [\n              -187.3828125,\n              -14.944784875088372\n            ],\n            [\n              -179.296875,\n              -33.137551192346145\n            ],\n            [\n              -175.078125,\n              -49.610709938074216\n            ],\n            [\n              -111.796875,\n              -54.162433968067795\n            ],\n            [\n              -86.1328125,\n              -42.81152174509788\n            ],\n            [\n              -90,\n              -2.811371193331128\n            ],\n            [\n              -111.4453125,\n              18.979025953255267\n            ],\n            [\n              -130.078125,\n              42.5530802889558\n            ],\n            [\n              -136.40625,\n              49.83798245308484\n            ],\n            [\n              -171.9140625,\n              54.36775852406841\n            ],\n            [\n              -204.609375,\n              49.15296965617042\n            ],\n            [\n              -223.2421875,\n              29.53522956294847\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"23","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Piper, David Z. dzpiper@usgs.gov","contributorId":2452,"corporation":false,"usgs":true,"family":"Piper","given":"David","email":"dzpiper@usgs.gov","middleInitial":"Z.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":780290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williamson, M.E.","contributorId":53954,"corporation":false,"usgs":true,"family":"Williamson","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":780291,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207916,"text":"70207916 - 1977 - Composition and phase chemistry of sulfide globules in basalt from the Mid-Atlantic Ridge rift valley near 37°N lat","interactions":[],"lastModifiedDate":"2020-01-20T11:36:05","indexId":"70207916","displayToPublicDate":"1977-01-20T11:26:42","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Composition and phase chemistry of sulfide globules in basalt from the Mid-Atlantic Ridge rift valley near 37°N lat","docAbstract":"<p>The electron microprobe was used to determine the bulk composition of immiscible sulfide globules trapped in the glass phase of 25 fresh submarine basalt samples from the Mid-Atlantic Ridge. Twenty-three samples represent a spectrum of primitive through differentiated tholeiites from the FAMOUS dive area; two are differentiated basalts from the Reykjanes Ridge. The analyzed globules range in diameter from 11 to 233 µm. On the average, they constitute only 0.0022 volume percent of the rocks and contain less than 1.5 percent of the sulfur. Compositions of the globules change with differentiation as measured by Fe/(Fe+Mg) or TiO<sub>2</sub><span>&nbsp;</span>content of the host glass. Globules in glass containing 0.66 to 1.0 wt percent TiO<sub>2</sub><span>&nbsp;</span>typically contain 20 to 26 wt percent Ni + Cu and have an average atomic Ni/Cu of 1.6. With differentiation toward 1.6 wt percent TiO<sub>2</sub>, Ni + Cu content of the globules falls to less than 10 wt percent and atomic Ni/Cu falls to 0.4.</p><p>Sulfur content of the host glasses shows a strong correlation with FeO content, increasing from 840 ppm to 1,370 ppm as FeO content increases from 8.0 to 12.6 wt percent. Reference to experimental studies shows that this relationship is consistent with sulfur saturation of the host glass at liquidus temperatures. Crystal fractionation is considered to be the dominant factor in keeping the differentiating melt at sulfur saturation.</p><p>The sulfide globules may have persisted in the basaltic melt from its place of formation by partial melting in the mantle, or they may have exsolved from the melt as it became sulfur-saturated in a high-level magma chamber. Globule abundance and composition indicate adjustment to the composition of the melt in which they were trapped. Material balance calculations suggest that one-third of the Cu and commensurate amounts of S, Ni, and Fe have settled from the magma as immiscible globules.</p><p>The sulfide globules contain less than 4 wt percent magnetite, compatible with low f<sub>o2</sub><span>&nbsp;</span>in the magma. Three sulfide phases coexisted in the globules at about 600 °C: monosulfide solid solution, intermediate solid solution, and pentlandite. At lower temperatures, the intermediate solid solution has broken down, and the monosulfide solid solution has exsolved a second generation of pentlandite.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1977)88<587:CAPCOS>2.0.CO;2","usgsCitation":"Czamanske, G., and Moore, J.G., 1977, Composition and phase chemistry of sulfide globules in basalt from the Mid-Atlantic Ridge rift valley near 37°N lat: GSA Bulletin, v. 88, no. 4, p. 587-599, https://doi.org/10.1130/0016-7606(1977)88<587:CAPCOS>2.0.CO;2.","productDescription":"13 p.","startPage":"587","endPage":"599","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mid-Atlantic Ridge rift valley near 37°N lat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -44.736328125,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              29.22889003019423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Czamanske, G.","contributorId":61185,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.","affiliations":[],"preferred":false,"id":779770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":779771,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207915,"text":"70207915 - 1977 - Compositional variations of young basalts in the Mid-Atlantic Ridge rift valley near lat 36°49′N","interactions":[],"lastModifiedDate":"2020-01-20T11:25:57","indexId":"70207915","displayToPublicDate":"1977-01-20T11:08:30","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Compositional variations of young basalts in the Mid-Atlantic Ridge rift valley near lat 36°49′N","docAbstract":"<p>Fifty acoustically positioned samples of fresh basalt were collected by the submersible<span>&nbsp;</span><i>Alvin</i><span>&nbsp;</span>from the median valley of the Mid-Atlantic Ridge during the French American Mid-Ocean Undersea Study (FAMOUS) in the summer of 1974. The samples show regular compositional variations from the center of the rift valley (central lava flows) out to the rift valley walls (flank lava flows). The central lava samples show higher ratios of olivine relative to clinopyroxene and plagioclase phenocrysts and contain chrome spinel. Glasses of the flank lava samples are enriched in SiO<sub>2</sub>, TiO<sub>2</sub>, K<sub>2</sub>O, H<sub>2</sub>O, and FeO/MgO relative to central lava samples.</p><p>Studies of the thickness of palagonite and manganese crusts indicate that the flank lava flows are considerably younger than the inferred spreading age of the crust on which they occur. Flank lavas are generally older than central lavas, but notable exceptions occur.</p><p>The composition of the flank lava glass can be derived by the removal of approximately 29 wt percent of analyzed phenocrysts (in the ratio 5.7 plagioclase, 2.5 olivine, 1.8 clinopyroxene) from the central lava glass. In addition, other processes (possibly involving volatile transfer) must enrich the flank lavas in K<sub>2</sub>O, TiO<sub>2</sub>, and H<sub>2</sub>O.</p><p>A model is proposed whereby this crystal fractionation occurs in a shallow, narrow (6-km-wide) magma chamber underlying the median valley. The chamber is compositionally zoned, and central lavas are fed from dikes tapping its hotter axial zone, whereas flank lavas are fed from the cooler, differentiated melt on the margins. The nature of the chemical variations in the lavas permits an estimate of the composition and thickness of the cumulates forming at the base of the chamber.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1977)88<556:CVOYBI>2.0.CO;2","usgsCitation":"Bryan, W., and Moore, J.G., 1977, Compositional variations of young basalts in the Mid-Atlantic Ridge rift valley near lat 36°49′N: GSA Bulletin, v. 88, no. 4, p. 556-570, https://doi.org/10.1130/0016-7606(1977)88<556:CVOYBI>2.0.CO;2.","productDescription":"15 p.","startPage":"556","endPage":"570","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371370,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mid-Atlantic Ridge rift valley near lat 36°49′N","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -44.736328125,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              29.22889003019423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bryan, W.B.","contributorId":100412,"corporation":false,"usgs":true,"family":"Bryan","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":779768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":779769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207883,"text":"70207883 - 1977 - Sheeted dikes, gabbro, and pillow basalt in flysch of coastal southern Alaska","interactions":[],"lastModifiedDate":"2020-01-16T14:02:08","indexId":"70207883","displayToPublicDate":"1977-01-16T13:56:49","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sheeted dikes, gabbro, and pillow basalt in flysch of coastal southern Alaska","docAbstract":"<p><span>A Paleocene to Eocene(?) mafic sequence of igneous rocks on Knight Island and a Cretaceous mafic and ultramafic sequence of the Resurrection Peninsula in coastal southern Alaska are characterized by pillow basalts, sheeted dikes, and gabbro intrusions. At both localities, pillow basalts are interbedded with flysch, and the gabbros intrude both the sheeted dikes and the immediately overlying sedimentary rocks. At the Resurrection Peninsula, small bodies of serpentinized dunite are present in the gabbro, and overlying low-grade metasedimentary rocks and mafic tuffs are interbedded with sedimentary rocks. At Knight Island the sheeted dikes intrude Paleocene and Eocene(?) sedimentary rocks. These igneous rocks have petrographic features similar to those of oceanic tholeiites and have some of the characteristics of ophiolites. They apparently were formed near the continental margin, because both sequences intrude and are interlayered with flysch. We believe the igneous rocks were intruded along faults (perhaps leaky transform faults) of ocean floor that happened to be near the continental margin; the faults were oriented parallel to the depositional strike and subsequent deformational strike of the Valdez(?) and Orca Groups.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1977)5<377:SDGAPB>2.0.CO;2","usgsCitation":"Tysdal, R.G., Case, J.E., Winkler, G.R., and Clark, S.H., 1977, Sheeted dikes, gabbro, and pillow basalt in flysch of coastal southern Alaska: Geology, v. 5, no. 6, p. 377-383, https://doi.org/10.1130/0091-7613(1977)5<377:SDGAPB>2.0.CO;2.","productDescription":"7 p.","startPage":"377","endPage":"383","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":371320,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Coastal southern Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.86328125,\n              55.87531083569679\n            ],\n            [\n              -143.61328125,\n              55.87531083569679\n            ],\n            [\n              -143.61328125,\n              62.02152819100765\n            ],\n            [\n              -154.86328125,\n              62.02152819100765\n            ],\n            [\n              -154.86328125,\n              55.87531083569679\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Tysdal, Russell G.","contributorId":1700,"corporation":false,"usgs":true,"family":"Tysdal","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":true,"id":779628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Case, J. E.","contributorId":56625,"corporation":false,"usgs":true,"family":"Case","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":779629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winkler, G. R.","contributorId":17964,"corporation":false,"usgs":true,"family":"Winkler","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":779630,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, S. H. B.","contributorId":95052,"corporation":false,"usgs":true,"family":"Clark","given":"S.","email":"","middleInitial":"H. B.","affiliations":[],"preferred":false,"id":779631,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70207858,"text":"70207858 - 1977 - The effects of the α‐β phase transformation on the creep properties of hydrolytically‐weakened synthetic quartz","interactions":[],"lastModifiedDate":"2020-07-09T15:39:11.310576","indexId":"70207858","displayToPublicDate":"1977-01-15T16:53:38","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"The effects of the α‐β phase transformation on the creep properties of hydrolytically‐weakened synthetic quartz","docAbstract":"<p>Nine rectangular prisms of hydro‐thermally‐grown synthetic quartz crystals with 900 atomic ppm H<sup>+</sup><span>&nbsp;</span>were loaded in compression at 1400 bars stress and temperatures between 403 and 764°C. The<span>&nbsp;</span><span>a</span><span>&nbsp;</span>and<span>&nbsp;</span><span>c</span><span>&nbsp;</span>directions were at 45° to the compression direction, and the slip system<span>&nbsp;</span><img class=\"section_image\" src=\"https://agupubs.onlinelibrary.wiley.com/cms/attachment/c98da4d3-4ef0-4f5a-b811-6af47325a68f/grl497-math-0001.gif\" alt=\"urn:x-wiley:00948276:media:grl497:grl497-math-0001\" data-mce-src=\"https://agupubs.onlinelibrary.wiley.com/cms/attachment/c98da4d3-4ef0-4f5a-b811-6af47325a68f/grl497-math-0001.gif\"><span>&nbsp;</span>appears to operate over the entire range of temperatures. The strain vs. time curves were sigmoidal in shape; an incubation stage of accelerating creep rates was followed by a hardening stage in which creep rates decreased with time. The creep rate (⋵) vs. temperature (T) data were found to fit very well an Arrehenius law of the form</p><div id=\"grl497-disp-0001\" class=\"inline-equation\"><span class=\"inline-equation__construct\"><img class=\"\" title=\"urn:x-wiley:00948276:media:grl497:grl497-math-0002\" src=\"https://agupubs.onlinelibrary.wiley.com/cms/attachment/6dc60836-8174-4751-bb22-63671a79377b/grl497-math-0002.gif\" alt=\"urn:x-wiley:00948276:media:grl497:grl497-math-0002\" data-mce-src=\"https://agupubs.onlinelibrary.wiley.com/cms/attachment/6dc60836-8174-4751-bb22-63671a79377b/grl497-math-0002.gif\"></span></div><p><span>where E* is the activation energy for creep. E* is 38.9 ± 2.1 kcal/mole in the α field and 14.3 ± 4.7 kcal/mole in the β field. An offset in the maximum strain rates occurs at the transition temperature, with the β phase creeping at less than half the rate of the α phase. It is suggested that the changes in creep parameters are due to the effects of the inversion on the rates of oxygen diffusion associated with the dissolved water, which hydrolytically weakens the crystals. The α‐β transformation involves rather subtle structural changes. No bond breaking occurs and the change in density is rather small. The transformations responsible for the transition zone of the mantle are reconstructive (involving extensive bond breaking and complete atomic reorganization) and the density changes are large. Thus the potential for large effects of these transformations on creep properties is even greater.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/GL004i003p00097","usgsCitation":"Kirby, S.H., 1977, The effects of the α‐β phase transformation on the creep properties of hydrolytically‐weakened synthetic quartz: Geophysical Research Letters, v. 4, no. 3, p. 97-100, https://doi.org/10.1029/GL004i003p00097.","productDescription":"4 p.","startPage":"97","endPage":"100","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":371287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"3","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Kirby, Stephen H. 0000-0003-1636-4688 skirby@usgs.gov","orcid":"https://orcid.org/0000-0003-1636-4688","contributorId":2752,"corporation":false,"usgs":true,"family":"Kirby","given":"Stephen","email":"skirby@usgs.gov","middleInitial":"H.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":779548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207857,"text":"70207857 - 1977 - Mechanical twinning in diopside Ca(Mg,Fe)Si2O6: Structural mechanism and associated crystal defects","interactions":[],"lastModifiedDate":"2020-07-09T15:44:07.275704","indexId":"70207857","displayToPublicDate":"1977-01-15T16:48:14","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3066,"text":"Physics and Chemistry of Minerals","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Mechanical twinning in diopside Ca(Mg,Fe)Si<sub>2</sub>O<sub>6</sub>: Structural mechanism and associated crystal defects","title":"Mechanical twinning in diopside Ca(Mg,Fe)Si2O6: Structural mechanism and associated crystal defects","docAbstract":"<p>iopside twins mechanically on two planes, (100) and (001), and the associated macroscopic twinning strains are identical (Raleigh and Talbot, 1967). An analysis based on crystal structural arguments predicts that both twin mechanisms involve shearing of the (100) octahedral layers (containing Ca<sup>2+</sup>, Mg<sup>2+</sup><span>&nbsp;</span>and Fe<sup>2+</sup><span>&nbsp;</span>ions) by a magnitude of<span>&nbsp;</span><i>c</i>/2. Small adjustments or shuffles occur in the adjacent layers containing the [SiO<sub>4</sub>]<sup>4−</sup><span>&nbsp;</span>tetrahedral chains. While the (100) twins are conventional with shear parallel to the composition plane, this analysis predicts that (001) twins form by a mechanism closely related to kinking.</p><p>A polycrystalline diopside specimen was compressed 8% at a temperature of 400° C, a pressure of 16 kilobars, and a compressive strain rate of about 10<sup>−4</sup>/s. Transmission electron microscopy on this specimen has revealed four basic lamellar features:</p><ol class=\"u-list-style-none\"><li><span class=\"u-custom-list-number\">1)</span><p>(100) mechanical twin lamellae;</p></li><li><span class=\"u-custom-list-number\">2)</span><p>(100) glide bands containing unit dislocations;</p></li><li><span class=\"u-custom-list-number\">3)</span><p>(001) twin lamellae;</p></li><li><span class=\"u-custom-list-number\">4)</span><p>(101) lamellar features, not as yet identified.</p></li></ol><p>The (001) twins often contain remnant (100) lamellae of untwinned host. Twinning dislocations occur in these (100) lamellae and in the (001) twin boundaries with very high densities. Diffraction contrast experiments indicate that the twinning dislocations associated with both twin laws glide on (100) with Burgers vector<span>&nbsp;</span><strong>b</strong>=<i>X</i><span>&nbsp;</span>[001] where<span>&nbsp;</span><i>X</i><span>&nbsp;</span>is probably equal to 1/2 on the basis of the structural analysis.</p><p>Parallels are drawn between mechanical twinning in clinopyroxenes and clinoamphiboles. The exclusive natural occurrence of basal twins in shock-loaded clinopyroxenes and of analogous (<span class=\"mathjax-tex\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mrow class=&quot;MJX-TeXAtom-ORD&quot;><mover><mn>1</mn><mo stretchy=&quot;false&quot;>&amp;#x00AF;</mo></mover></mrow></math>\"><span id=\"MathJax-Span-1\" class=\"math\"><span><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"texatom\"><span id=\"MathJax-Span-4\" class=\"mrow\"><span id=\"MathJax-Span-5\" class=\"munderover\"><span id=\"MathJax-Span-6\" class=\"mn\">1</span><span id=\"MathJax-Span-7\" class=\"mo\">¯</span></span></span></span></span></span></span><span class=\"MJX_Assistive_MathML\">1¯</span></span></span>01) twins in clinoamphiboles is given a simple explanation in terms of the relative difficulty of the “kinking” mechanism as compared to direct glide parallel to the composition plane.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF00307315","usgsCitation":"Kirby, S.H., and Christie, J., 1977, Mechanical twinning in diopside Ca(Mg,Fe)Si2O6: Structural mechanism and associated crystal defects: Physics and Chemistry of Minerals, v. 1, p. 137-163, https://doi.org/10.1007/BF00307315.","productDescription":"27 p.","startPage":"137","endPage":"163","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":371286,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kirby, Stephen H. 0000-0003-1636-4688 skirby@usgs.gov","orcid":"https://orcid.org/0000-0003-1636-4688","contributorId":2752,"corporation":false,"usgs":true,"family":"Kirby","given":"Stephen","email":"skirby@usgs.gov","middleInitial":"H.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":779546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christie, J.M.","contributorId":21672,"corporation":false,"usgs":true,"family":"Christie","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":779547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70198917,"text":"70198917 - 1977 - Geology of the Waynesboro East and Waynesboro West Quadrangles, Virginia","interactions":[],"lastModifiedDate":"2019-05-21T10:43:21","indexId":"70198917","displayToPublicDate":"1977-01-03T15:27:31","publicationYear":"1977","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Geology of the Waynesboro East and Waynesboro West Quadrangles, Virginia","docAbstract":"<p>The Waynesboro East and Waynesboro West Quadrangles comprise an area of approximately 117 square miles (304 sq km) in portions of Albemarle, Augusta, and Nelson counties in north-central Virginia. Included in the quadrangles are portions of the Piedmont, Blue Ridge, and Valley and Ridge physiographic provinces and two major regional structures - the Blue Ridge anticlinoriurm and the Massanutten synclinorium.</p><p>The rocks of the Blue Ridge anticlorium are complexly folded and faulted and consist of five sequences, the oldest being the Precambrian gneisses that include the Lovingston and Pedlar formations. Unconformably overlying these rocks or in fault contact with them is a sequence of Precambrian(?) stratified rock units including the metamorphosed, fluvial, sedimentary, and basic volcanic strata of the Swift Run and Catoctin formations. These are overlain by a sequence of Cambrian clastic rocks that include the Weverton, Harpers, and Antietarn formations. The Massanutten synclinorium within the study area is formed from the overlying Cambrian and Ordovician carbonate sequence that includes the Shady, Waynesboro, Elbrook, Conococheague, Chepultepec, Beekmantown, New Market, and Lincolnshire formations. These carbonate rocks are overlain by the Ordovician clastic sequence of the Martinsburg Formation. Many of these rock units are locally intruded by diabase dikes of Triassic age and are IocalIy covered by alluvial Quaternary sediments.</p><p>The intensity of deformation increases from northwest to southeast with recumbent folds, thrust faults, and zones of cataclastic rocks present in the southeastern half of the area. All of the rocks are altered with the metamorphic rank being somewhat greater to the southeast.</p><p>Sources of agricultural limestone, limestone aggregate, and in limited quantities high-calcium Iimestone are present. Ceramic clay, crushed stone. sand and gravel, and iron and manganese have been produced in small quantities.</p><p>Fourteen environmental geologic units having similar geologic factors - bedrock, residuum, and soil properties - affecting land modification have been delineated. Each is briefly evaluated with respect to slope stability, erodibility, and response to excavation or other types of land modification. Rockfall, karst. cave areas, and floodprone regions have been delineated.</p>","largerWorkTitle":"Virginia Division of Mineral Resources Publication","publisher":"Commonwealth of Virginia, Dept. of Conservation and Economic Development, Division of Mineral Resources","publisherLocation":"Charlottesville, VA","usgsCitation":"Gathright, T.M., Henika, W.S., and Sullivan, J.L., 1977, Geology of the Waynesboro East and Waynesboro West Quadrangles, Virginia, v. 3, 53 p.","productDescription":"53 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356748,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":356747,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.dmme.virginia.gov/commercedocs/PUB_3.pdf","text":"Document"}],"country":"United States","state":"Virginia","county":"Albemarle County, Augusta County, Nelson County","city":"Waynesboro","otherGeospatial":"Waynesboro East quadrangle, Waynesboro West Quadrangle","volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gathright, Thomas M. II","contributorId":207266,"corporation":false,"usgs":false,"family":"Gathright","given":"Thomas","suffix":"II","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":743415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henika, William S.","contributorId":178188,"corporation":false,"usgs":false,"family":"Henika","given":"William","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":743416,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sullivan, John L.","contributorId":207277,"corporation":false,"usgs":false,"family":"Sullivan","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":743417,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30043,"text":"wri7761 - 1977 - The effect of the Faka Union Canal system on water levels in the Fakahatchee Strand, Collier County, Florida","interactions":[],"lastModifiedDate":"2022-01-06T16:35:14.160273","indexId":"wri7761","displayToPublicDate":"1977-01-01T21:30:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-61","title":"The effect of the Faka Union Canal system on water levels in the Fakahatchee Strand, Collier County, Florida","docAbstract":"<p>The Faka Union Canal system, constructed in the western Big Cypress Swamp, Fla., in the early 1970's, lies about 3.5 miles west of the centerline of the Fakahatchee Strand, a forested water course which the State of Florida has designated as an Area of Critical State Concern in order to conserve natural resources. Between 1970 and 1975 the canal system annually discharged to the Gulf of Mexico from 143,200 to 275,600 acre-feet of freshwater. Discharge lowered ground-water levels as much as 4 feet near the eastern canal and created a water-level gradient that indicates water flowed from the Fakahatchee Strand west toward the canal during most of the year. In June 1975, water from early summer rains was impounded in the eastern canal upstream of the control structure at Janes Scenic Drive, and, as water levels rose in this reach, water flowed from the canal into the aquifer and around the control structure.</p><p>The annual low-water level in the center of the Fakahatchee Strand declined from nearly 3 feet above mean sea level in 1972 to 1 foot above mean sea level in 1974. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7761","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Swayze, L.J., and McPherson, B.F., 1977, The effect of the Faka Union Canal system on water levels in the Fakahatchee Strand, Collier County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-61, iii, 19 p., https://doi.org/10.3133/wri7761.","productDescription":"iii, 19 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":2477,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0061/wri7761.pdf","text":"Report","size":"885 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":159292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0061/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Collier County","otherGeospatial":"Fakahatchee Strand, Faka Union Canal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.25326538085938,\n              25.75413552707459\n            ],\n            [\n              -81.20407104492188,\n              25.75413552707459\n            ],\n            [\n              -81.20407104492188,\n              26.606946521203206\n            ],\n            [\n              -82.25326538085938,\n              26.606946521203206\n            ],\n            [\n              -82.25326538085938,\n              25.75413552707459\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62f633","contributors":{"authors":[{"text":"Swayze, Leo J.","contributorId":55437,"corporation":false,"usgs":true,"family":"Swayze","given":"Leo","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":202584,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26246,"text":"wri7733 - 1977 - Saline-water intrusion related to well construction in Lee County, Florida","interactions":[],"lastModifiedDate":"2022-01-05T19:02:45.909337","indexId":"wri7733","displayToPublicDate":"1977-01-01T21:30:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-33","title":"Saline-water intrusion related to well construction in Lee County, Florida","docAbstract":"<p>Ground water is the principle source of water supply in Lee County, Florida where an estimated 30,000 wells have been drilled since 1990. These wells ranges in depth from about 10 to 1,240 feet and tap the water table aquifer or one or more of the artesian water-bearing units or zones in the Tamiami Formation, the upper part of the Hawthorn Formation, the lower part of the Hawthorn Formation and the Tampa Limestone and the Suwannee Limestone. Before 1968, nearly all wells were constructed with galvanized or black iron pipe. Many of these wells are sources of saline-water intrusion into freshwater-bearing zones.</p><p>The water-bearing zones in the lower part of the Hawthorn Formation, Tampa Limestone, and Suwannee Limestone are artesian-they have higher water levels and usually contain water with a higher concentration of dissolved solids than do the aquifers occurring at shallower depths. The water from these deeper aquifers generally range in dissolved solids concentration from about 1,500 to 2,400 mg/L, and in chloride from about 500 to 1,00 mg/L. A maximum chloride concentration of 15,200 mg/L has been determined. Few of the 3,00 wells estimated to have been drilled to these zones contain sufficient casing to prevent upward flow into overlaying water-bearing zones. Because of water-level differentials, upward movement and lateral intrusion of saline water occurs principally into the upper part of the Hawthorn Formation where the chloride concentrations in water unaffected by saline-water intrusion ranges from about 80 to 150 mg/L. Where intrusion from deep artesian zones has occurred, the chloride concentration in water from the upper part of the Hawthorn Formation ranges from about 300 to more than 2,100 mg/L.</p><p>Surface discharges of the saline water from wells tapping the lower part of the Hawthorn Formation and the Suwannee Limestone also had affected the water-table aquifer which normally contains water with 10 to 50 mg/L of chloride. In one area, the chloride concentration in water from the water table aquifer ranged from 200 to 590 mg/L as a result of intrusion.</p><p>In areas adjacent to tidal-water bodies, the water table aquifer contains water that is very saline, Where the wells in such areas have been constructed with metal casings, the metal corrodes when exposed to the saline water, and many ultimately develop holes. This permits saline water to leak into the well where the water level in the well is lower than the water table. The intrusion of saline water from the water-table aquifer into the upper part of the Hawthorn Formation is a major problem in parts of Cape Coral. Withdrawal of water from the upper part of the Hawthorn Formation has caused water levels to decline below the lowest annual position of the water table, so that downward leakage is perennial. In some coastal areas, wells that tap the upper part of the Hawthorn Formation contain water whose chloride concentration is as much as 9,500 mg/L.</p><p>Upward leakage of saline water from the deep artesian aquifers and downward leakage of saline water from the water-table aquifer can be prevented by proper well construction.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7733","collaboration":"Prepared in cooperation with the Board of County Commissioners of Lee County","usgsCitation":"Boggess, D.H., Missimer, T., and O’Donnell, T., 1977, Saline-water intrusion related to well construction in Lee County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-33, iv, 29 p., https://doi.org/10.3133/wri7733.","productDescription":"iv, 29 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science 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href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c9a6","contributors":{"authors":[{"text":"Boggess, Durward Hoye","contributorId":13243,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"Hoye","affiliations":[],"preferred":false,"id":196053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Missimer, T.M.","contributorId":41839,"corporation":false,"usgs":true,"family":"Missimer","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":196054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Donnell, T.H.","contributorId":69970,"corporation":false,"usgs":true,"family":"O’Donnell","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":196055,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70007446,"text":"70007446 - 1977 - The U.S. Geological Survey's Central Region headquarters, Denver, Colorado","interactions":[],"lastModifiedDate":"2012-02-17T00:10:14","indexId":"70007446","displayToPublicDate":"1977-01-01T17:27:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"The U.S. Geological Survey's Central Region headquarters, Denver, Colorado","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70007446","usgsCitation":"U.S. Geological Survey, 1977, The U.S. Geological Survey's Central Region headquarters, Denver, Colorado, 24 p., ill., 23 cm., https://doi.org/10.3133/70007446.","productDescription":"24 p., ill., 23 cm.","startPage":"1","endPage":"24","numberOfPages":"24","costCenters":[],"links":[{"id":258785,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70007446/report.pdf","size":"7520","linkFileType":{"id":1,"text":"pdf"}},{"id":258786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70007446/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba945e4b08c986b32215a"}
,{"id":70168651,"text":"70168651 - 1977 - Geohydrology of Muscatine Island, Muscatine County, Iowa","interactions":[],"lastModifiedDate":"2025-07-30T13:42:57.763237","indexId":"70168651","displayToPublicDate":"1977-01-01T17:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":148,"text":"Water Supply Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"Geohydrology of Muscatine Island, Muscatine County, Iowa","docAbstract":"<p>Muscatine Island is a wide segment of the west bank of the Mississippi River flood plain that covers about 50 square miles in Muscatine and Louisa Counties; the project area encompasses the 30 square miles in Muscatine County. The flood plain is underlain by thick, permeable alluvial deposits that comprise a water-table aquifer that is developed extensively for water supplies in the area. The aquifer consists principally of sand and gravel, interbedded with lenses of silt and clay. Its saturated thickness ranges from about 40 to 140 feet. The transmissivity and storage coefficients of the aquifer range from about 20,000 ft.<sup>2</sup>/day and 0.15. respectively, in the western part of the Island to about 39,500 ft.2/day and 0.24 in the eastern part. The amount of water stored in the aquifer, under normal conditions, is about 100 billion gallons.</p>\n<p>Discharge from the aquifer is principally by pumpage, which has increased from about 1 mgd (million gallons per day) in 1906 to about 37 mgd in 1970. About 2.5 mgd is normally lost to seepage and evapotranspiration along a 9-mile reach of Muscatine Slough in Muscatine County. About 0.9 mgd is discharged by evaporation from gravel pits.</p>\n<p>Recharge to the aquifer is by induced infiltration from the Mississippi River, seepage from the river during major flood events, precipitation, and seepage from the underlying limestone bedrock. Induced infiltration provides about 80 to 85 percent of the water withdrawn from the principal pumping centers along the river and also replaces about 70 to 80 percent of the water that is evaporated from the gravel pits; this amounted to about 30 mgd in 1971. Additional significant recharge from the river occurs during major floods, when prolonged high stages provide the head for considerable underflow to the aquifer. Recharge from precipitation on the Island was calculated to average about 6inches per year or about 0.3 mgd per square mile. Seepage from bedrock is significant and is attributed to the increased head differential between the alluvial and bedrock aquifers in the areas of major pumping.</p>\n<p>The chemical constituents of water from the aquifer are generally within the recommended limits established by the U. S. Public Health Service for drinking water.</p>\n<p>Stresses on the hydrologic system have affected the position and configuration of the water table and the chemical quality of the ground water. The large-scale withdrawals, which began at the principal pumping centers in 1946, have caused the water table to decline from about 1 foot in the interior of the Island to about 5 feet near the edges of the main pumping centers; the decline was more than 8 feet under the pumping centers. A slight increase in hardness of water from riverward wells in the pumping centers is attributed to the induced infiltration of slightly harder river water; a noticeable increase in hardness and iron content in water from landward wells is attributed to seepage of water from the bedrock. In the central irrigated area, which is underlain by very permeable, highly drained soils that are mulched with organic fertilizers, the nitrate content of the ground water is as high as 46 mg/l (milligrams per liter). Land-use practices have had, and probably will continue to have, an impact on the quality and quantity of water available in the system.</p>\n<p>The hydrologic system in 1971 was in dynamic equilibrium or in near-equilibrium with the stresses imposed on it to that date. This equilibrium would be disturbed by any additional stresses on the system and water levels would change until a new equilibrium was established. The effects of future stresses can be reasonably predicted by developing a digital model of the system. The data to develop such a model are available in this report. Continued and expanded monitoring of water levels would provide data for better model verification. Periodic monitoring of nitrate and other chemical constituents would permit early detection of changes in concentration before the concentrations reached excessive levels.</p>","language":"English","publisher":"State of Iowa","publisherLocation":"Des Moines, IA","collaboration":"Prepared in cooperation with the Iowa Geological Survey, the United States Geological Survey, and the Board of Water and Light Trustees of the City of Muscatine, Iowa","usgsCitation":"Hansen, R., and Steinhilber, W.L., 1977, Geohydrology of Muscatine Island, Muscatine County, Iowa: Water Supply Bulletin 11, viii, 60 p.","productDescription":"viii, 60 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318299,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70168651.JPG"},{"id":493177,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70168651/IGS_wsb_11.pdf","text":"Report","size":"2.95","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","county":"Muscatine","otherGeospatial":"Muscatine Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.23252868652344,\n              41.22773259388589\n            ],\n            [\n              -91.23252868652344,\n              41.45199070565348\n            ],\n            [\n              -90.98533630371094,\n              41.45199070565348\n            ],\n            [\n              -90.98533630371094,\n              41.22773259388589\n            ],\n            [\n              -91.23252868652344,\n              41.22773259388589\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56cc3fdce4b059daa47e45a4","contributors":{"authors":[{"text":"Hansen, R.E.","contributorId":57109,"corporation":false,"usgs":true,"family":"Hansen","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":621163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinhilber, W. 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