{"pageNumber":"5048","pageRowStart":"126175","pageSize":"25","recordCount":165579,"records":[{"id":70230851,"text":"pp1124F - 1980 - Palladium, platinum, and rhodium concentrations in mafic and ultramafic rocks from the Zhob Valley and Dargai complexes, Pakistan","interactions":[],"lastModifiedDate":"2022-04-26T13:50:34.007151","indexId":"pp1124F","displayToPublicDate":"1980-12-31T08:39:43","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1124","chapter":"F","title":"Palladium, platinum, and rhodium concentrations in mafic and ultramafic rocks from the Zhob Valley and Dargai complexes, Pakistan","docAbstract":"<p>The Zhob Valley and Dargai complexes, Pakistan, consist of harzburgite and dunite tectonites containing chromite deposits, pyroxenite, wehrlite, and gabbro. Both are ophiolite complexes. Palladium, platinum, and rhodium were found in concentrations of up to 170, 200, and 22 parts per billion, respectively. Average concentrations for both complexes and all rock types collected are 28 ppb palladium, 33 ppb platinum, and 9 ppb rhodium. The Pt:Pt+Pd ranges from 0.41 to 0.67 and averages 0.57. The concentration levels and ratios of these metals are similar to other alpine ultramafic bodies that have been analyzed by modern techniques.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to mineralogy and petrology, 1979","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1124F","usgsCitation":"Page, N.J., Haffty, J., and Ahmad, Z., 1980, Palladium, platinum, and rhodium concentrations in mafic and ultramafic rocks from the Zhob Valley and Dargai complexes, Pakistan: U.S. Geological Survey Professional Paper 1124, iii, 6 p., https://doi.org/10.3133/pp1124F.","productDescription":"iii, 6 p.","costCenters":[],"links":[{"id":399662,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":399660,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1124a-f/report.pdf"}],"country":"Pakistan","otherGeospatial":"Zhob Valley complex","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              67.5,\n              31\n            ],\n            [\n              68.25,\n              31\n            ],\n            [\n              68.25,\n              30.5\n            ],\n            [\n              67.5,\n              30.5\n            ],\n            [\n              67.5,\n              31\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Page, Norman J.","contributorId":46492,"corporation":false,"usgs":true,"family":"Page","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":841458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haffty, Joseph","contributorId":79450,"corporation":false,"usgs":true,"family":"Haffty","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":841459,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ahmad, Zaki","contributorId":85205,"corporation":false,"usgs":true,"family":"Ahmad","given":"Zaki","email":"","affiliations":[],"preferred":false,"id":841460,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70230767,"text":"pp1124D - 1980 - Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Final and Gila Counties, Arizona","interactions":[{"subject":{"id":70230767,"text":"pp1124D - 1980 - Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Final and Gila Counties, Arizona","indexId":"pp1124D","publicationYear":"1980","noYear":false,"chapter":"D","title":"Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Final and Gila Counties, Arizona"},"predicate":"IS_PART_OF","object":{"id":4929,"text":"pp1124AF - 1980 - Shorter contributions to mineralogy and petrology, 1979","indexId":"pp1124AF","publicationYear":"1980","noYear":false,"chapter":"A-F","title":"Shorter contributions to mineralogy and petrology, 1979"},"id":1}],"isPartOf":{"id":4929,"text":"pp1124AF - 1980 - Shorter contributions to mineralogy and petrology, 1979","indexId":"pp1124AF","publicationYear":"1980","noYear":false,"title":"Shorter contributions to mineralogy and petrology, 1979"},"lastModifiedDate":"2022-04-26T13:28:18.516584","indexId":"pp1124D","displayToPublicDate":"1980-12-31T08:19:13","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1124","chapter":"D","title":"Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Final and Gila Counties, Arizona","docAbstract":"<p>Specimens of tuff in the Ray-San Manuel area, southeastern Arizona, have been X-rayed to determine the present approximate mineralogic composition and the type and degree of alteration of the tuffs. Some of the tuffs consist largely of glass or have been partly or completely altered to calcium montmorillonite; many of them have been almost completely zeolitized or contain a zeolite and some clay. Only three zeolitized specimens contain a little glass. With four exceptions, the zeolitie is clinoptilolite; the exceptions are one altered to chabazite, one to mordenite, one to erionite, and one to erionite, clinoptilolite, and chabazite. The tuffs are mostly of airfall origin and of rhyolitic or probable rhyolitic composition and generally contain negligible percentages of crystal and lithic fragments. Two specimens are tuffaceous sedimentary rocks, and two are ash-flow tuffs. The tuffs range in age from early Pliocene or late Miocene to Oligocene. Some were deposited in lacustrine or playa environments; others were deposited in freshwater alluvial environments. All the beds examined in the lower Miocene and older formations have been zeolitized. Zeolitization of beds in younger formations depends on the environment of deposition. Zeolitized tuffs that contain at least 80 percent zeolite and are in beds more than one-third meter thick are considered potentially minable. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to mineralogy and petrology, 1979","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1124D","usgsCitation":"Krieger, M.H., 1980, Zeolitization of Tertiary tuffs in lacustrine and alluvial deposits in the Ray-San Manuel area, Final and Gila Counties, Arizona: U.S. Geological Survey Professional Paper 1124, iii, 11 p., https://doi.org/10.3133/pp1124D.","productDescription":"iii, 11 p.","costCenters":[],"links":[{"id":399638,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":399637,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1124a-f/report.pdf"}],"country":"United States","state":"Arizona","county":"Gila County, Pinal County","otherGeospatial":"San Manuel area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              32.625\n            ],\n            [\n              -110.5,\n              32.625\n            ],\n            [\n              -110.5,\n              33.25\n            ],\n            [\n              -111,\n              33.25\n            ],\n            [\n              -111,\n              32.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Krieger, Medora H.","contributorId":62188,"corporation":false,"usgs":true,"family":"Krieger","given":"Medora","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":841336,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188982,"text":"70188982 - 1980 - Lateral trends and vertical sequences in estuarine sediments, Willapa Bay, Washington","interactions":[],"lastModifiedDate":"2017-06-28T10:49:49","indexId":"70188982","displayToPublicDate":"1980-12-31T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Lateral trends and vertical sequences in estuarine sediments, Willapa Bay, Washington","docAbstract":"<p>Willapa Bay is a sizable estuary on the southern coast of Washington- Relatively unmodified in a geologic sense by human activity the bay provides an excellent example of modern depositional facies in an estuarine setting. </p><p>Studies of these deposits indicate that consistent lateral trends exist in sediment texture and sedimentary structures. The texture changes from sandy at the mouth of the bay to muddy in its upper parts. In any part of the bay , sediment is coarsest in the channel bottoms, where lag deposits accumulate. The sediment tends to fine in an upslope direction and is finest in supratidal flat deposits of silt and clay. </p><p>The nature of sedimentary structures depends on the combination of physical and biological processes and sediment textures. Bedforms exist wherever the bed is sandy. In the main tidal channels sandwaves and dunes up to 4 meters high occur. In tributary channels and at the margins of the main channel, at shallower depths and under less intense currents , the structures are generally less than a meter high. Current ripples occur in t he sandy bed of all of the tidal channels and in runoff channels cross the tidal flat. Symmetric long-crested ripples are produced by wave action over the sandy intertidal flat. </p><p>Internal structures in the bay's sediment depend not only on the nature of the bedform but also on the rate of bioturbation relative to physical processes. Under fields of large sandwaves or dunes, medium- to large-scale tabular and trough crossbedding predominates. This crossbedding generally is unidirectional, reflecting the locally dominant current (ebb or flood). Ripple bedding predominates elsewhere in sandy sediment within the channels. Where sand transport is diminished, as on the floor of the upper tributary channels, bioturbation exceeds the rate of production of physical structures and bedding is destroyed. The depositional banks in such areas tend to be sites of rapid sediment accumulation and bedding in the form of interlayered sand (commonly ripple bedded) and mud persists. On intertidal flats the sediment accumulates slowly and bioturbation erases nearly all physical structures. Bedding is preserved only where deposition is locally rapid , as in topographic depressions or on the depositional banks of runoff channels, or where faunal activity is inhibited, as beneath mounds of blue-green algae. The rate of sedimentation is slower still on the supratidal flats, but the general paucity of faunal activity allows the preservation of thin alternations of fine sand , silt or clay.</p><p> The lateral migration of the tidal channels produces vertical sequences in which topographically higher facies are superposed on one another. Near the mouth of the estuary the upward sequence: lag deposit — crossbedded sand — ripple or planar-bedded sand is typical. The crossbedding shows a general upward decrease in thickness and a progression from trough to tabular units. In the main tidal channel - in the central estuary and in sandy tributary channels, the typical vertical sequence resembles that near the mouth , with the exception that the sequence is capped by bioturbated sandy or muddy tide flat deposits. In the upper estuary , where muddy sediment predominates, a typical sequence shows the progression-. bioturbated lag deposit — gently dipping interlaminated sand and mud layers of the accretionary bank — bioturbated mud flat deposits — thinly laminated fine supratidal deposits. </p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Pacific Coast Paleogreography Symposium 4: Quarternary Depositional Environments of the Pacific Coast","conferenceDate":"April 9, 1980","language":"English","publisher":"SEPM Society for Sedimentary Geology","usgsCitation":"Clifton, H.E., and Phillips, L., 1980, Lateral trends and vertical sequences in estuarine sediments, Willapa Bay, Washington, Pacific Coast Paleogreography Symposium 4: Quarternary Depositional Environments of the Pacific Coast, April 9, 1980, p. 55-71.","productDescription":"17 p.","startPage":"55","endPage":"71","costCenters":[],"links":[{"id":343067,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River, Willapa Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.81018066406249,\n              45.91103315853962\n            ],\n            [\n              -123.03039550781249,\n              45.91103315853962\n            ],\n            [\n              -123.03039550781249,\n              47.23262467463881\n            ],\n            [\n              -124.81018066406249,\n              47.23262467463881\n            ],\n            [\n              -124.81018066406249,\n              45.91103315853962\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"596611cfe4b0d1f9f05cef36","contributors":{"authors":[{"text":"Clifton, H. Edward","contributorId":46503,"corporation":false,"usgs":true,"family":"Clifton","given":"H.","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":702204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, L.","contributorId":63556,"corporation":false,"usgs":true,"family":"Phillips","given":"L.","email":"","affiliations":[],"preferred":false,"id":702205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70197813,"text":"70197813 - 1980 - The Klamath Mountains","interactions":[],"lastModifiedDate":"2023-08-30T14:35:38.152906","indexId":"70197813","displayToPublicDate":"1980-12-31T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5712,"text":"Bulletin de la Société Géologique de France","active":true,"publicationSubtype":{"id":10}},"title":"The Klamath Mountains","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Societe Geologique de France","doi":"10.2113/gssgfbull.S7-XXII.4.527","usgsCitation":"Irwin, W., 1980, The Klamath Mountains: Bulletin de la Société Géologique de France, v. 22, no. 4, p. 527-532, https://doi.org/10.2113/gssgfbull.S7-XXII.4.527.","productDescription":"6 p.","startPage":"527","endPage":"532","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355224,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon","otherGeospatial":"Klamath Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.5871538816491,\n              43.95898875152997\n            ],\n            [\n              -124.5871538816491,\n              40.034210951991014\n            ],\n            [\n              -121.03949999132685,\n              40.034210951991014\n            ],\n            [\n              -121.03949999132685,\n              43.95898875152997\n            ],\n            [\n              -124.5871538816491,\n              43.95898875152997\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"22","issue":"4","noUsgsAuthors":false,"publicationDate":"1980-01-01","publicationStatus":"PW","contributors":{"editors":[{"text":"Aubouin, J.","contributorId":19296,"corporation":false,"usgs":true,"family":"Aubouin","given":"J.","email":"","affiliations":[],"preferred":false,"id":738631,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Blanchet, Richard J.","contributorId":176663,"corporation":false,"usgs":false,"family":"Blanchet","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":738632,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Rangin, C.","contributorId":105853,"corporation":false,"usgs":true,"family":"Rangin","given":"C.","email":"","affiliations":[],"preferred":false,"id":738633,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738630,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197809,"text":"70197809 - 1980 - Tectonic relations of carbon dioxide discharges and earthquakes","interactions":[],"lastModifiedDate":"2018-06-20T15:33:06","indexId":"70197809","displayToPublicDate":"1980-12-31T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Tectonic relations of carbon dioxide discharges and earthquakes","docAbstract":"<p><span>CO</span><sub>2</sub><span>‐rich springs occur worldwide along major zones of seismicity. They are mostly in young orogenic belts, but some are in areas of rifting continental platforms. Analyses of<span>&nbsp;</span></span><sup>13</sup><span>C content indicate that much of the CO</span><sub>2</sub><span><span>&nbsp;</span>is derived from the mantle and that other important sources are the metamorphism of marine carbonate‐bearing sedimentary rocks and the degradation of organic material. The presence of calc‐silicate minerals, such as pumpellyite in metagraywacke, is evidence of former conversion of carbonate‐bearing rocks into calc‐silicate minerals and release of CO</span><sub>2</sub><span>. The CO</span><sub>2</sub><span><span>&nbsp;</span>pressure in fractured rocks of a fault zone reduces the effective normal stress and, if it is sufficiently great, allows the fault to slip. If the pressure were maintained at a sufficiently high level, the fault behavior might be characterized by frequent small earthquakes and aseismic creep such as occur along active segments of the San Andreas system. The presence of CO</span><sub>2</sub><span>‐rich springs may indicate a potentially hazardous seismic region. Monitoring of CO</span><sub>2</sub><span><span>&nbsp;</span>discharges could be useful in earthquake prediction.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB06p03115","usgsCitation":"Irwin, W., and Barnes, I., 1980, Tectonic relations of carbon dioxide discharges and earthquakes: Journal of Geophysical Research B: Solid Earth, v. 85, no. 6, p. 3115-3121, https://doi.org/10.1029/JB085iB06p03115.","productDescription":"7 p.","startPage":"3115","endPage":"3121","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355222,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"6","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":738616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70196625,"text":"70196625 - 1980 - Diatoms and stratigraphically significant silicoflagellates from the Atlantic Margin Coring Project and other Atlantic margin sites","interactions":[],"lastModifiedDate":"2018-04-20T14:00:19","indexId":"70196625","displayToPublicDate":"1980-12-31T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Diatoms and stratigraphically significant silicoflagellates from the Atlantic Margin Coring Project and other Atlantic margin sites","docAbstract":"<p>In 1976, 19 sites were cored along the U.S. Atlantic Continental Shelf and Slope by the Oceanographic Branch of the U.S. Geological Survey aboard the&nbsp;<i>Glomar Conception.&nbsp;</i>Only 6 sites contained siliceous microfossil assemblages of sufficient quantity and quality for biostratigraphic study. Two of the sites, AMCOR (Atlantic Margin Coring Project) 6002 and AMCOR 6011, contained good Miocene assemblages: a small Pleistocene assemblage occurred at the top of AMCOR 6002. A Late Miocene to Early Pliocene assemblage was encountered in AMCOR 6007B. AMCOR 6013, 6019, and 6021 contained Pleistocene assemblages. In addition to the AMCOR cores, 3 additional Atlantic Margin cores were studied. These were the JOIDES 1 (Caldrill) core, and Atlantic Slope Project (ASP) cores 10 and 22. JOIDES 1 contains a Middle Miocene assemblage similar to AMCOR 6002. ASP 10 contains a Lower Pliocene assemblage and ASP 22 contains a Middle to Late Oligocene and a Pleistocene assemblage. Siliceous assemblages at all sites consisted mainly of shallow shelf species, including brackish and marine benthics and occasionally freshwater forms. Although planktonic forms were present, they were few and most were extant cosmopolitan species. This makes it difficult to correlate the biostratigraphy of the sediments with siliceous microfossil zonations from other oceans. The only biostratigraphic zonations for Atlantic Shelf diatom assemblages are for the Miocene.</p>","language":"English","publisher":"Micropaleontology Press","usgsCitation":"Abbott, W., 1980, Diatoms and stratigraphically significant silicoflagellates from the Atlantic Margin Coring Project and other Atlantic margin sites: Micropaleontology, v. 26, no. 1, p. 49-80.","productDescription":"32 p.","startPage":"49","endPage":"80","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":353628,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":353627,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.geoscienceworld.org/micropal/article-lookup/26/1/49"}],"geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -62.49023437499999,\n              43.13306116240612\n            ],\n            [\n              -74.8828125,\n              46.437856895024204\n            ],\n            [\n              -87.62695312499999,\n              26.194876675795218\n            ],\n            [\n              -75.234375,\n              21.53484700204879\n            ],\n            [\n              -62.49023437499999,\n              43.13306116240612\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff476ce4b0da30c1bfdb6f","contributors":{"authors":[{"text":"Abbott, W.H.","contributorId":20076,"corporation":false,"usgs":true,"family":"Abbott","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":733810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188676,"text":"70188676 - 1980 - Geology of a zone of metamorphic core complexes in southeastern Arizona ","interactions":[],"lastModifiedDate":"2017-06-21T08:50:11","indexId":"70188676","displayToPublicDate":"1980-12-31T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1784,"text":"Geological Society Memoir","active":true,"publicationSubtype":{"id":10}},"title":"Geology of a zone of metamorphic core complexes in southeastern Arizona ","docAbstract":"<p>An elongate northwest-trending zone of batholith-size metamorphic core complexes extends some 130 km from the Rincon Mountains to the Picacho Mountains in southeastern Arizona. The complexes are characterized by undeformed to gneissic granitic intrusions, gneissic to phyllonitic xenoliths and wall rocks derived mainly from Precambrian granitic rock, shallow-dipping foliation, and remarkably uniform directions of lineation. Parts of this zone have been recognized and studied extensively for more than 30 yr, but there remains a divergence of opinion about the age, depth of emplacement, and origin of the complexes. Field relations indicate that host rocks as young as or younger than Mesozoic were involved in cataclasis. K-Ar and fission-track ages indicate that the complexes were at temperatures uniformly in excess of 400°C in the middle Tertiary (20 to 30 m.y. ago) and that the bedrock between and very near the complexes was not thermally affected. Tertiary plutons characteristically associated with the high-grade metamorphic rocks are also cataclastically deformed, and stratigraphic depths to the top of metamorphic terranes were no more than 6 km and possibly less than 3 km. These and other data suggest to some that the complexes developed during intrusion of composite batholiths at shallow depth in an anisotropic stress field during the middle Tertiary. On the other hand, Rb-Sr and U-Th-Pb techniques yielded older ages (≥44 m.y.) for some samples. These and additional data suggest to others that major development of cataclasis preceded the middle Tertiary and included regional thrusting. </p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM153","usgsCitation":"Banks, N.G., 1980, Geology of a zone of metamorphic core complexes in southeastern Arizona : Geological Society Memoir, p. 177-215, https://doi.org/10.1130/MEM153.","productDescription":"39 p.","startPage":"177","endPage":"215","costCenters":[],"links":[{"id":342698,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","city":"Tucson","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.81359863281249,\n              31.90087807776307\n            ],\n            [\n              -110.357666015625,\n              31.90087807776307\n            ],\n            [\n              -110.27252197265625,\n              32.33355894864106\n            ],\n            [\n              -111.5167236328125,\n              33.201924189778936\n            ],\n            [\n              -111.6815185546875,\n              32.42170336417894\n            ],\n            [\n              -110.81359863281249,\n              31.90087807776307\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594b85bae4b062508e382bdb","contributors":{"authors":[{"text":"Banks, Norman G.","contributorId":89524,"corporation":false,"usgs":true,"family":"Banks","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":698873,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207205,"text":"70207205 - 1980 - Hydrology comes of age: Impact of the International Hydrological Decade","interactions":[],"lastModifiedDate":"2019-12-12T09:33:46","indexId":"70207205","displayToPublicDate":"1980-12-30T09:23:40","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology comes of age: Impact of the International Hydrological Decade","docAbstract":"<p><span>The IHD (International Hydrological Decade), 1965 to 1974, was conceived as a concerted international effort to bring into focus the badly fragmented subdiscipline of hydrology, to evolve a global perspective on water, and to provide global information on water. Until the last decade or so, hydrology was a laggard science. The science was also fragmented among surface‐water hydrology, agricultural hydrology, groundwater hydrology, oceanology, hydrometeorology, and hydrogeochemistry. All these disciplines were bona fide members of the hydrological family, but there was little interchange, so there was no central focus for the science as a whole. ©1980. American Geophysical Union. All Rights Reserved.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/EO061i053p01241","issn":"00963941","usgsCitation":"Nace, R.L., 1980, Hydrology comes of age: Impact of the International Hydrological Decade: Eos, Transactions, American Geophysical Union, v. 61, no. 53, p. 1241-1241, https://doi.org/10.1029/EO061i053p01241.","productDescription":"1 p. ","startPage":"1241","endPage":"1241","costCenters":[],"links":[{"id":370199,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"53","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","contributors":{"authors":[{"text":"Nace, R. L.","contributorId":11332,"corporation":false,"usgs":true,"family":"Nace","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":777272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207569,"text":"70207569 - 1980 - Uranium in secondary silica: A possible exploration guide","interactions":[],"lastModifiedDate":"2020-06-04T14:38:44.259661","indexId":"70207569","displayToPublicDate":"1980-12-24T12:45:18","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Uranium in secondary silica: A possible exploration guide","docAbstract":"<p><span>Study of uraniferous silica precipitates in the Shirley Basin, Wyoming, identified areas where ancient uraniferous ground water once ponded. Chalcedony collected from and directly beneath thick accumulations of rhyolite ash contain as much as 250 ppm uranium in a pre-ash topographic low and lesser concentrations (10 to 160 ppm) elsewhere. Differences in the U concentration of chalcedony collected from approximately the same stratigraphic horizon reflect the enrichment of uranium in ground water as it percolated downward and basinward through the overlying rhyolite ash. Uranium is homogeneously distributed as a uranyl species within the chalcedony and reflects coprecipitation of dissolved uranium and colloidal silica in a uraniferous silica-gel. Laboratory measurements of the partitioning of uranium between various solutions and silica-gel precipitates indicate that, for ranges of pH and dissolved carbonate typical of ground water, dried silica-gel contains about 400 to 1,000 times the uranium concentration of the solution from which it forms. Uranium is postulated to be incorporated as an adsorbed uranyl-silica-hydroxyl complex. A 20-m.y.-minimum apparent age for uraniferous chalcedony was obtained by U-Pb isotope dating. Reported minimum ages for nearby sedimentary uranium deposits generally lie between this age and the age of rhyolite which hosts the silica (32.4 + or - 2.6 m.y.). Leaching of uranium from ash during the period 20 to 32 m.y. is therefore compatible with a volcanic source-rock hypothesis.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.75.4.592","usgsCitation":"Zielinski, R.A., 1980, Uranium in secondary silica: A possible exploration guide: Economic Geology, v. 75, no. 4, p. 592-602, https://doi.org/10.2113/gsecongeo.75.4.592.","productDescription":"11 p.","startPage":"592","endPage":"602","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":370679,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Shirley Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.30,\n              42.30\n            ],\n            [\n              -106.00,\n              42.30\n            ],\n            [\n              -106.00,\n              42.15\n            ],\n            [\n              -106.30,\n              42.15\n            ],\n            [\n              -106.30,\n              42.30\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"75","issue":"4","noUsgsAuthors":false,"publicationDate":"1980-07-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":778522,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207259,"text":"70207259 - 1980 - Research on interactive genetic-geological models to evaluate favourability for undiscovered uranium resources","interactions":[],"lastModifiedDate":"2020-06-01T19:52:46.74834","indexId":"70207259","displayToPublicDate":"1980-12-13T14:24:19","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Research on interactive genetic-geological models to evaluate favourability for undiscovered uranium resources","docAbstract":"<p>Current methods of evaluating favourability for undiscovered uranium resources are unduly subjective, quite possibly inconsistent and, as a consequence, of questionable reliability. This research is aimed at reducing the subjectivity and increasing the reliability by designing an improved method that depends largely on geological data and their statistical frequency of occurrence. This progress report outlines a genetic approach to modelling the geological factors that controlled uranium mineralization in order to evaluate the favourability for the occurrence of undiscovered uranium deposits of the type modeled. A genetic model is constructed from all the factors that describe the processes, in chronological sequence, that formed uranium deposits thought to have a common origin. The field and laboratory evidence for the processes constitute a geologic occurrence base that parallels the chronological sequence of events. The genetic model and the geologic-occurrence base are portrayed as two columns of an interactive matrix called the \"genetic-geologic model\". For each column, eight chronological stages are used to describe the overall formation of the uranium deposits. These stages consist of (1) precursor processes; (2) host-rock formation; (3) preparation of host-rock; (4) uranium-source development; (5) transport of uranium; (6) primary uranium deposition; (7) post-deposition modification; and (8) preservation. To apply the genetic-geological model to evaluate favourability, a question is posed that determines the presence or absence of each attribute listed under the geologic-occurrence base. By building a logic circuit of the attributes according to either their essential or non-essential nature, the resultant match between a well-documented control area and the test area may be determined. The degree of match is a measure of favourability for uranium occurrence as hypothesized in the genetic model. This process of geological decision analysis results in a series of favourability maps that can be combined into a final composite favourability map. </p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Uranium Evaluation and Mining Techniques: Proceedings of a Symposium Held in Buenos Aires, Argentina, 1–4 October 1979","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Uranium Evaluation and Mining Techniques","conferenceDate":"October, 1-4, 1979","conferenceLocation":"Buenos Aires, Argentina","language":"English","publisher":"IAEA","isbn":"9200402801","usgsCitation":"Finch, W., Granger, H., Lupe, R., and McCammon, R., 1980, Research on interactive genetic-geological models to evaluate favourability for undiscovered uranium resources, <i>in</i> Uranium Evaluation and Mining Techniques: Proceedings of a Symposium Held in Buenos Aires, Argentina, 1–4 October 1979, Buenos Aires, Argentina, October, 1-4, 1979, p. 447-462.","productDescription":"16 p.","startPage":"447","endPage":"462","costCenters":[],"links":[{"id":370266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Finch, W.I.","contributorId":75919,"corporation":false,"usgs":true,"family":"Finch","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":777481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Granger, H.C.","contributorId":15203,"corporation":false,"usgs":true,"family":"Granger","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":777482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lupe, R.D.","contributorId":107696,"corporation":false,"usgs":true,"family":"Lupe","given":"R.D.","affiliations":[],"preferred":false,"id":777483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCammon, R.B.","contributorId":17218,"corporation":false,"usgs":true,"family":"McCammon","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":777484,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70120130,"text":"70120130 - 1980 - The effect of band loss on estimates of annual survival","interactions":[],"lastModifiedDate":"2014-08-12T13:44:06","indexId":"70120130","displayToPublicDate":"1980-12-01T13:37:13","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2284,"text":"Journal of Field Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"The effect of band loss on estimates of annual survival","docAbstract":"<p>Banding has proven to be a useful technique in the study of population dynamics of avian species.  However, band loss has long been recognized as a potential problem, (Hickey, 1952; Ludwig, 1967).  Recently, Brownie et al. (1978) presented 14 models based on an array of explicit assumptions for the analysis of band recovery data.  Various estimation models (assumption sets) allowed survival and/or recovery rates to be (a) constant, (b) time-specific, or (c) time- and age-specific.  Optimal inference methods were employed and statistical tests of critical assumptions were developed and emphasized.</p>\n<br/>\n<p>The methods of Brownie et al. (1978), as with all previously published methods of which we are aware, assume no loss of bands during the study.  However, some band loss is certain to occur and this potentially biases the estimates of annual survival rates whatever the analysis method.  A few empirical studies have estimated band loss rates (a notable exception is Ludwig, 1967); consequently, for almost all band recovery data, the exact rate of band loss is unknown.  In this paper we investigate the bias in estimates of annual survival rates due to varying degrees of hypothesized band loss.  Our main results are based on perhaps the most useful model, originally developed by Seber (1970), for estimation of annual survival rate.  Inferences are made concerning the bias of estimated survival rates in other models because the structure of these estimators is similar.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Field Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Northeastern Bird-Banding Association","publisherLocation":"Ipswich, NH","usgsCitation":"Nelson, L.J., Anderson, D.R., and Burnham, K.P., 1980, The effect of band loss on estimates of annual survival: Journal of Field Ornithology, v. 51, no. 1, p. 30-38.","productDescription":"9 p.","startPage":"30","endPage":"38","numberOfPages":"9","costCenters":[],"links":[{"id":292037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a90e4b0461e44764ad7","contributors":{"authors":[{"text":"Nelson, Louis J.","contributorId":106028,"corporation":false,"usgs":true,"family":"Nelson","given":"Louis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":497945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":497943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":497944,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011744,"text":"70011744 - 1980 - Rates of volcanic activity along the southwest rift zone of Mauna Loa volcano, Hawaii","interactions":[],"lastModifiedDate":"2023-08-31T15:04:57.263717","indexId":"70011744","displayToPublicDate":"1980-12-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Rates of volcanic activity along the southwest rift zone of Mauna Loa volcano, Hawaii","docAbstract":"Flow-by-flow mapping of the 65 km long subaerial part of the southwest rift zone and adjacent flanks of Mauna Loa Volcano, Hawaii, and about 50 new 14C dates on charcoal from beneath these flows permit estimates of rates of lava accumulation and volcanic growth over the past 10 000 years. The sequence of historic eruptions along the southwest rift zone, beginning in 1868, shows a general pattern of uprift migration and increasing eruptive volume, culminating in the great 1950 eruption. No event comparable to 1950, in terms of volume or vent length, is evident for at least the previous 1000 years. Rates of lava accumulation along the zone have been subequal to those of Kilauea Volcano during the historic period but they were much lower in late prehistoric time (unpubl. Kilauea data by R. T. Holcomb). Rates of surface covering and volcanic growth have been markedly asymmetric along Mauna Loa's southwest rift zone. Accumulation rates have been about half again as great on the northwest side of the rift zone in comparison with the southeast side. The difference apparently reflects a westward lateral shift of the rift zone of Mauna Loa away from Kilauea Volcano, which may have acted as a barrier to symmetrical growth of the rift zone. -Author","language":"English","publisher":"Springer","doi":"10.1007/BF02600366","usgsCitation":"Lipman, P.W., 1980, Rates of volcanic activity along the southwest rift zone of Mauna Loa volcano, Hawaii: Bulletin Volcanologique, v. 43, no. 4, p. 703-725, https://doi.org/10.1007/BF02600366.","productDescription":"23 p.","startPage":"703","endPage":"725","numberOfPages":"23","costCenters":[],"links":[{"id":220928,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Mauna Loa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -156,\n              19.625\n            ],\n            [\n              -156,\n              18.75\n            ],\n            [\n              -155,\n              18.75\n            ],\n            [\n              -155,\n              19.625\n            ],\n            [\n              -156,\n              19.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"43","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9549e4b0c8380cd8190d","contributors":{"authors":[{"text":"Lipman, P. W.","contributorId":93470,"corporation":false,"usgs":true,"family":"Lipman","given":"P.","middleInitial":"W.","affiliations":[],"preferred":false,"id":361859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012241,"text":"70012241 - 1980 - Calcite-impregnated defluidization structures in littoral sands of Mono Lake, California","interactions":[],"lastModifiedDate":"2026-01-12T16:36:45.11377","indexId":"70012241","displayToPublicDate":"1980-11-28T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Calcite-impregnated defluidization structures in littoral sands of Mono Lake, California","docAbstract":"Associated locally with well-known tufa mounds and towers of Mono Lake, California, are subvertical, concretionary sand structures through which fresh calcium-containing artesian waters moved up to sites of calcium carbonate precipitation beneath and adjacent to the lake. The structures include closely spaced calcite-impregnated columns, tubes, and other configurations with subcylindrical to bizarre cross sections and predominantly vertical orientation in coarse, barely coherent pumice sands along the south shore of the lake. Many structures terminate upward in extensive calcareous layers of caliche and tufa. Locally they enter the bases of tufa mounds and towers. A common form superficially resembles root casts and animal burrows except that branching is mostly up instead of down. Similar defluidization structures in ancient sedimentary rocks have been mistakenly interpreted as fossil burrows.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.210.4473.1009","issn":"00368075","usgsCitation":"Cloud, P., and Lajoie, K.R., 1980, Calcite-impregnated defluidization structures in littoral sands of Mono Lake, California: Science, v. 210, no. 4473, p. 1009-1012, https://doi.org/10.1126/science.210.4473.1009.","productDescription":"4 p.","startPage":"1009","endPage":"1012","costCenters":[],"links":[{"id":221874,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mono Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.2110407898813,\n              38.08685583176151\n            ],\n            [\n              -119.2110407898813,\n              37.92409113914387\n            ],\n            [\n              -118.87991470946412,\n              37.92409113914387\n            ],\n            [\n              -118.87991470946412,\n              38.08685583176151\n            ],\n            [\n              -119.2110407898813,\n              38.08685583176151\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"210","issue":"4473","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2f6e4b0c8380cd4b4f5","contributors":{"authors":[{"text":"Cloud, P.","contributorId":65973,"corporation":false,"usgs":true,"family":"Cloud","given":"P.","affiliations":[],"preferred":false,"id":363068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lajoie, K. R.","contributorId":6828,"corporation":false,"usgs":true,"family":"Lajoie","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363067,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70157384,"text":"70157384 - 1980 - Annual report of the USGS Mission, Kingdom of Saudi Arabia, for the second year of the fifth extension of the USGS-MPMR work agreement : fiscal year 1399/1400 : 1 Rajab 1399-29 Jumad Thani 1400 (27 May 1979-14 May 1980)","interactions":[],"lastModifiedDate":"2015-09-22T12:26:05","indexId":"70157384","displayToPublicDate":"1980-11-27T18:30:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"Interagency report, 293","title":"Annual report of the USGS Mission, Kingdom of Saudi Arabia, for the second year of the fifth extension of the USGS-MPMR work agreement : fiscal year 1399/1400 : 1 Rajab 1399-29 Jumad Thani 1400 (27 May 1979-14 May 1980)","docAbstract":"<p><span>Prepared for Directorate General of Mineral Resources, Ministry of Petroleum and Mineral Resources, Jiddah, Saudi Arabia.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Jiddah, Saudi Arabia","usgsCitation":"U.S. Geological Survey Saudi Arabia Mission, 1980, Annual report of the USGS Mission, Kingdom of Saudi Arabia, for the second year of the fifth extension of the USGS-MPMR work agreement : fiscal year 1399/1400 : 1 Rajab 1399-29 Jumad Thani 1400 (27 May 1979-14 May 1980), v, 41 p.","productDescription":"v, 41 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308368,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Saudi Arabia","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56027bb4e4b03bc34f5447fe","contributors":{"authors":[{"text":"U.S. Geological Survey Saudi Arabia Mission","contributorId":147326,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey Saudi Arabia Mission","id":572941,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70199709,"text":"70199709 - 1980 - Geochemical evidence for water‐rock interaction along the San Andreas and Garlock Faults of California","interactions":[],"lastModifiedDate":"2018-09-26T09:56:42","indexId":"70199709","displayToPublicDate":"1980-11-10T09:56:07","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical evidence for water‐rock interaction along the San Andreas and Garlock Faults of California","docAbstract":"<p><span>Mesozoic granitoid rocks adjacent to the San Andreas fault in central California have retained their radiogenic Ar for the last 70 m.y. but have, generally, the highest&nbsp;</span><sup>18</sup><span>O and H</span><sub>2</sub><span>O</span><sup>+</sup><span>&nbsp;contents and the lowest D contents of all the granitoid rocks in California. The geographical coincidence of the D,&nbsp;</span><sup>18</sup><span>O, and H</span><sub>2</sub><span>O</span><sup>+</sup><span>&nbsp;patterns with the present trace of the San Andreas fault leave little doubt that some kind of groundwater circulation system has operated in the vicinity of the fault in central California. Similar isotopic patterns exist in rocks along the Garlock fault. These water‐rock interactions probably took place at temperatures &lt;200°C, although depth, extent, and timing are not resolved. Stable isotope compositions of rocks from many localities of the earth have provided unambiguous proof that meteoric waters have descended to depths at least as great as 8 to 10 km when a heat source such as a cooling pluton was present. Massive circulation of groundwater is common in the upper crust of tectonically active areas and may affect the frictional stress state along major faults. The geochemical evidence for extensive deep circulation of groundwater and the relatively high permeabilities for most rocks of the upper crust recently compiled by Brace (1980) argues against nearly lithostatic fluid pressures as an ambient condition of the upper crust. Groundwater circulation along the San Andreas provides an efficient mechanism for diffusing the heat flow anomaly that arises in heat transport calculations that are based on thermal conduction alone.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB11p06286","usgsCitation":"O’Neil, J.R., and Hanks, T.C., 1980, Geochemical evidence for water‐rock interaction along the San Andreas and Garlock Faults of California: Journal of Geophysical Research, v. 85, no. B11, p. 6286-6292, https://doi.org/10.1029/JB085iB11p06286.","productDescription":"7 p.","startPage":"6286","endPage":"6292","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":357740,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault, Garlock Fault","volume":"85","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"O’Neil, James R.","contributorId":70762,"corporation":false,"usgs":true,"family":"O’Neil","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":746289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanks, Thomas C. 0000-0003-0928-0056 thanks@usgs.gov","orcid":"https://orcid.org/0000-0003-0928-0056","contributorId":3065,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","email":"thanks@usgs.gov","middleInitial":"C.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":746290,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70200769,"text":"70200769 - 1980 - Grooved terrain on Ganymede","interactions":[],"lastModifiedDate":"2019-06-11T14:43:16","indexId":"70200769","displayToPublicDate":"1980-11-01T09:33:12","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Grooved terrain on Ganymede","docAbstract":"<p><span>The icy crust of Ganymede comprises bright and dark areas. Investigation of Voyager 1 and 2 images has shown that bright terrain is grooved and separates dark polygons of cratered terrain. The grooved terrain contains alternating ridges and grooves in straight and curvilinear sets, which are locally interrupted by smooth patches and swaths. Cratered terrain, where 'it occurs in small wedges and slivers, has a pervasive grain of narrowly spaced furrows, and thus is transitional to grooved terrain. An analysis of the morphology of terrain types, and of superposition and cross-cutting relations, suggests that grooved terrain grew at the expense of cratered terrain, that tracts of cratered terrain were converted into grooved terrain&nbsp;</span><i>in situ</i><span>, and that vertical tectonism and shear movements dominated in the restructuring of Ganymede's surface. It is postulated that during a period in the planet's history when the lithosphere was thin, upwelling convection currents caused incipient rifting accompanied by intensive normal faulting; where rifting went to completion, crustal segments separated, locally spread apart, and sheared past one another. In places subduction and compression may have occurred, but the evidence is inconclusive. Thus, the grooved terrain on Ganymede may record an early phase of ice-plate tectonics that caused rifting and drifting of the icy lithosphere, but, unlike silicate plate tectonics on Earth, may have resulted in only minor vertical turnover.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(80)90039-1","usgsCitation":"Lucchitta, B.K., 1980, Grooved terrain on Ganymede: Icarus, v. 44, no. 2, p. 481-501, https://doi.org/10.1016/0019-1035(80)90039-1.","productDescription":"21 p.","startPage":"481","endPage":"501","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":359011,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lucchitta, Baerbel K. blucchitta@usgs.gov","contributorId":3649,"corporation":false,"usgs":true,"family":"Lucchitta","given":"Baerbel","email":"blucchitta@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":750439,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70181810,"text":"70181810 - 1980 - Surficial deposits, weathering processes, and evolution of an inner Coastal Plain landscape, Augusta, Georgia","interactions":[],"lastModifiedDate":"2017-02-14T13:53:05","indexId":"70181810","displayToPublicDate":"1980-10-31T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Surficial deposits, weathering processes, and evolution of an inner Coastal Plain landscape, Augusta, Georgia","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Excursions in Southeastern geology; Volume II","language":"English","publisher":"American Geological Institute","publisherLocation":"Falls Church, VA","isbn":"0-913312-49-5 ","usgsCitation":"Newell, W.L., Pavich, M.J., Prowell, D.C., Markewich, H.W., Neathery, T.L., and Frey, R.W., 1980, Surficial deposits, weathering processes, and evolution of an inner Coastal Plain landscape, Augusta, Georgia, chap. <i>of</i> Excursions in Southeastern geology; Volume II, v. II, p. 527-544.","productDescription":"18 p.","startPage":"527","endPage":"544","costCenters":[],"links":[{"id":335367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","volume":"II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a4254ae4b0c825128ad4df","contributors":{"authors":[{"text":"Newell, Wayne L. wnewell@usgs.gov","contributorId":2512,"corporation":false,"usgs":true,"family":"Newell","given":"Wayne","email":"wnewell@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":668685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pavich, Milan J. mpavich@usgs.gov","contributorId":2348,"corporation":false,"usgs":true,"family":"Pavich","given":"Milan","email":"mpavich@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":668686,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prowell, David C.","contributorId":46956,"corporation":false,"usgs":true,"family":"Prowell","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":668687,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Markewich, Helaine W. 0000-0001-9656-3243 helainem@usgs.gov","orcid":"https://orcid.org/0000-0001-9656-3243","contributorId":2008,"corporation":false,"usgs":true,"family":"Markewich","given":"Helaine","email":"helainem@usgs.gov","middleInitial":"W.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":668688,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Neathery, Thorton L.","contributorId":58189,"corporation":false,"usgs":true,"family":"Neathery","given":"Thorton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":668689,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Frey, Robert W.","contributorId":181575,"corporation":false,"usgs":false,"family":"Frey","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":668690,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":5221599,"text":"5221599 - 1980 - An improved web-tagging technique for waterfowl","interactions":[],"lastModifiedDate":"2024-10-28T15:54:17.727542","indexId":"5221599","displayToPublicDate":"1980-10-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"An improved web-tagging technique for waterfowl","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808320","usgsCitation":"Haramis, G., and Nice, A.D., 1980, An improved web-tagging technique for waterfowl: Journal of Wildlife Management, v. 44, no. 4, p. 898-899, https://doi.org/10.2307/3808320.","productDescription":"2 p.","startPage":"898","endPage":"899","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198992,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Montezuma National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.82041643301584,\n              43.03969461549909\n            ],\n            [\n              -76.82041643301584,\n              42.94072495607546\n            ],\n            [\n              -76.72774197584917,\n              42.94072495607546\n            ],\n            [\n              -76.72774197584917,\n              43.03969461549909\n            ],\n            [\n              -76.82041643301584,\n              43.03969461549909\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684755","contributors":{"authors":[{"text":"Haramis, G.Michael","contributorId":112286,"corporation":false,"usgs":true,"family":"Haramis","given":"G.Michael","email":"","affiliations":[],"preferred":false,"id":334237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nice, Allen D.","contributorId":93159,"corporation":false,"usgs":true,"family":"Nice","given":"Allen","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":334236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5222056,"text":"5222056 - 1980 - Dosing free-living nestling starlings with an organophosphate pesticide, famphur","interactions":[],"lastModifiedDate":"2024-10-28T17:15:58.948323","indexId":"5222056","displayToPublicDate":"1980-10-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Dosing free-living nestling starlings with an organophosphate pesticide, famphur","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808325","usgsCitation":"Powell, G., and Gray, D., 1980, Dosing free-living nestling starlings with an organophosphate pesticide, famphur: Journal of Wildlife Management, v. 44, no. 4, p. 918-921, https://doi.org/10.2307/3808325.","productDescription":"4 p.","startPage":"918","endPage":"921","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198997,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","city":"Laurel","otherGeospatial":"Patuxent Wildlife Research Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.82280310319254,\n              39.07579891097075\n            ],\n            [\n              -76.82280310319254,\n              39.03142847712391\n            ],\n            [\n              -76.7495720992876,\n              39.03142847712391\n            ],\n            [\n              -76.7495720992876,\n              39.07579891097075\n            ],\n            [\n              -76.82280310319254,\n              39.07579891097075\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db636067","contributors":{"authors":[{"text":"Powell, G.V.N.","contributorId":23894,"corporation":false,"usgs":true,"family":"Powell","given":"G.V.N.","email":"","affiliations":[],"preferred":false,"id":335380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, D.C.","contributorId":30719,"corporation":false,"usgs":true,"family":"Gray","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":335381,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":11088,"text":"ofr81380 - 1980 - Geological studies in an area of induced seismicity at Monticello Reservoir, South Carolina","interactions":[],"lastModifiedDate":"2023-09-01T13:31:01.37412","indexId":"ofr81380","displayToPublicDate":"1980-09-30T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-380","title":"Geological studies in an area of induced seismicity at Monticello Reservoir, South Carolina","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81380","usgsCitation":"Secor, D.T., 1980, Geological studies in an area of induced seismicity at Monticello Reservoir, South Carolina: U.S. Geological Survey Open-File Report 81-380, Report: v, 42 p.; 9 Plates: 21.49 x 32.23 inches or smaller, https://doi.org/10.3133/ofr81380.","productDescription":"Report: v, 42 p.; 9 Plates: 21.49 x 32.23 inches or smaller","costCenters":[],"links":[{"id":38852,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38851,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38850,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38846,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38847,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38848,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38849,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38853,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38854,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0380/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38855,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0380/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143285,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0380/report-thumb.jpg"},{"id":420385,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12025.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"South Carolina","otherGeospatial":"Monticello Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.26465819284638,\n              34.379539937343665\n            ],\n            [\n              -81.52169157854195,\n              34.379539937343665\n            ],\n            [\n              -81.52169157854195,\n              34.1180459632578\n            ],\n            [\n              -81.26465819284638,\n              34.1180459632578\n            ],\n            [\n              -81.26465819284638,\n              34.379539937343665\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880f0","contributors":{"authors":[{"text":"Secor, Donald T.","contributorId":23543,"corporation":false,"usgs":true,"family":"Secor","given":"Donald","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":162513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70237066,"text":"70237066 - 1980 - Basin development along the Late Mesozoic and Cainozoic California Margin: A plate tectonic margin of subduction, oblique subduction and transform tectonics","interactions":[],"lastModifiedDate":"2022-09-29T11:58:47.234811","indexId":"70237066","displayToPublicDate":"1980-09-29T06:55:12","publicationYear":"1980","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"4","title":"Basin development along the Late Mesozoic and Cainozoic California Margin: A plate tectonic margin of subduction, oblique subduction and transform tectonics","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Along the Californian margin of the North American plate, the configuration and structural stability of late Mesozoic and Cainozoic basins are related to plate kinematics. Three tectonic regimes are recorded; orthogonal high-angle subduction, oblique low-angle subduction, and transform slip. During the first, regionally extensive forearc basins developed; during the second and third, borderland settings formed as a consequence of wrench faulting. In the forearc basins, sedimentological facies constitute regional belts that persist for hundreds of kilometres, with stratigraphic sequences that are 1–15 km thick. Shorelines are relatively straight, shelf facies are broad and well developed, and basin fill is composed of shallow marine, shelf and coalescing submarine-fan facies. Sediment transport in the deeper water facies commonly is parallel to the basin axis. Borderland basins reflect tectonic instability. A principal effect of wrench tectonics is the vertical reciprocation of crustal blocks. Shorelines are generally irregular, and narrow shelves pass abruptly into deep basins. Lithofacies change dramatically along strike, and stratigraphic thicknesses are variable from basin to basin, from tens of metres up to 6 km. Basin-margin facies are marked by unconformities, slump aprons, lithological pinch-outs and submarine canyon channels. Penecontemporaneous slip along the basin-margin faults complicates these lithofacies patterns. Borderland type palaeogeography is most extensively developed in the transform tectonic regime, and therefore the more seaward offshore basins are relatively depleted of terrigenous debris owing to transport barriers.</p></div></div>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sedimentation in Oblique-Slip Mobile Zones","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Wiley","doi":"10.1002/9781444303735.ch4","usgsCitation":"Howell, D.G., Crouch, J.K., Greene, H.G., McCulloch, D.S., and Vedder, J.G., 1980, Basin development along the Late Mesozoic and Cainozoic California Margin: A plate tectonic margin of subduction, oblique subduction and transform tectonics, chap. 4 <i>of</i> Sedimentation in Oblique-Slip Mobile Zones, v. 4, p. 43-62, https://doi.org/10.1002/9781444303735.ch4.","productDescription":"20 p.","startPage":"43","endPage":"62","costCenters":[],"links":[{"id":407566,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.134765625,\n              32.84267363195431\n            ],\n            [\n              -116.103515625,\n              32.84267363195431\n            ],\n            [\n              -116.103515625,\n              38.13455657705411\n            ],\n            [\n              -123.134765625,\n              38.13455657705411\n            ],\n            [\n              -123.134765625,\n              32.84267363195431\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","noUsgsAuthors":false,"publicationDate":"2009-04-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Howell, David G.","contributorId":12091,"corporation":false,"usgs":true,"family":"Howell","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":true,"id":853232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crouch, James K.","contributorId":56645,"corporation":false,"usgs":true,"family":"Crouch","given":"James","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":853233,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Greene, H. G.","contributorId":116109,"corporation":false,"usgs":true,"family":"Greene","given":"H.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":853234,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":853235,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":853236,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70181831,"text":"70181831 - 1980 - Upper Cretaceous and lower Tertiary geology of the Chattahoochee River valley, western Georgia and eastern Alabama","interactions":[],"lastModifiedDate":"2017-02-14T15:03:47","indexId":"70181831","displayToPublicDate":"1980-09-23T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Upper Cretaceous and lower Tertiary geology of the Chattahoochee River valley, western Georgia and eastern Alabama","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Excursions in Southeastern geology","language":"English","publisher":"American Geological Institute ","publisherLocation":"Falls Church, VA","isbn":"0-913312-49-5 ","usgsCitation":"Reinhardt, J., Gibson, T.G., Neathery, T.L., and Frey, R.W., 1980, Upper Cretaceous and lower Tertiary geology of the Chattahoochee River valley, western Georgia and eastern Alabama, chap. <i>of</i> Excursions in Southeastern geology, v. II, p. 385-463.","productDescription":"79 p.","startPage":"385","endPage":"463","costCenters":[],"links":[{"id":335388,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a4254ae4b0c825128ad4e1","contributors":{"authors":[{"text":"Reinhardt, Juergen","contributorId":88714,"corporation":false,"usgs":true,"family":"Reinhardt","given":"Juergen","email":"","affiliations":[],"preferred":false,"id":668756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibson, Thomas G.","contributorId":25180,"corporation":false,"usgs":true,"family":"Gibson","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":668757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neathery, Thorton L.","contributorId":58189,"corporation":false,"usgs":true,"family":"Neathery","given":"Thorton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":668758,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frey, Robert W.","contributorId":181575,"corporation":false,"usgs":false,"family":"Frey","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":668759,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70185555,"text":"70185555 - 1980 - Geology and hydrology for environmental planning in Washtenaw County, Michigan","interactions":[],"lastModifiedDate":"2026-04-17T19:41:47.405329","indexId":"70185555","displayToPublicDate":"1980-09-22T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Geology and hydrology for environmental planning in Washtenaw County, Michigan","docAbstract":"<p>Washteaw County is underlain by glacial deposits that range in thickness from about 50 feet to about 450 feet. Underlying the glacial deposits are sedimentary rocks of Mississippian and Devonian age. The youngest of these rocks are the sandstones of the Marshall Formation in the western part of the county;&nbsp; the oldest are the limestones of the Detroit River Group in the southeast corner.</p><p>Sand and gravel deposits in some places in the county may yield more than 500 gallons per minute of water. Approximately 50 percent of the wells tapping the Marshall Formation, the most reliable bedrock aquifer, can yield as much as 60 gallons per minute.</p><p>Washtenaw County has sand and gravel deposits that are more than 50 feet thick. The deposits are mined in several areas and are of economic importance. In addition, there may be potential for peat production in the western part of the county and for clay production in the eastern part.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/70185555","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Fleck, W.B., 1980, Geology and hydrology for environmental planning in Washtenaw County, Michigan: Open-File Report, iv, 23 p., https://doi.org/10.3133/70185555.","productDescription":"iv, 23 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":503231,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70185555/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":338212,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70185555/report-thumb.jpg"}],"country":"United States","state":"Michigan","county":"Washtenaw County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.553,42.4351],[-83.5492,42.3486],[-83.5417,42.1744],[-83.5399,42.0853],[-83.6563,42.0833],[-83.7763,42.0823],[-83.8927,42.0797],[-84.0164,42.0789],[-84.0165,42.0749],[-84.1353,42.073],[-84.136,42.1611],[-84.1319,42.2483],[-84.132,42.3356],[-84.1333,42.4238],[-84.0196,42.423],[-83.9065,42.4249],[-83.7864,42.4288],[-83.6669,42.4312],[-83.553,42.4351]]]},\"properties\":{\"name\":\"Washtenaw\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d4df18e4b05ec79911d205","contributors":{"authors":[{"text":"Fleck, William B.","contributorId":17587,"corporation":false,"usgs":true,"family":"Fleck","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":685944,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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