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,{"id":96530,"text":"96530 - 1978 - Use of Landsat data to assess waterfowl habitat quality","interactions":[],"lastModifiedDate":"2012-02-02T00:03:56","indexId":"96530","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Use of Landsat data to assess waterfowl habitat quality","docAbstract":"No abstract available at this time","language":"English","collaboration":"Final Rept. NASA Goddard Space Flight Center, Greenbelt, MD.","usgsCitation":"Colwell, J., Gilmer, D., Work, E., Rebel, D., and Roller, N., 1978, Use of Landsat data to assess waterfowl habitat quality, 83 p.","productDescription":"83 p.","startPage":"83","numberOfPages":"83","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0e9e","contributors":{"authors":[{"text":"Colwell, J.","contributorId":61773,"corporation":false,"usgs":true,"family":"Colwell","given":"J.","email":"","affiliations":[],"preferred":false,"id":299768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilmer, D.S.","contributorId":22270,"corporation":false,"usgs":true,"family":"Gilmer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":299767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Work, E.A.","contributorId":7650,"corporation":false,"usgs":true,"family":"Work","given":"E.A.","affiliations":[],"preferred":false,"id":299766,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rebel, D.L.","contributorId":74700,"corporation":false,"usgs":true,"family":"Rebel","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":299769,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Roller, N.E.G.","contributorId":74703,"corporation":false,"usgs":true,"family":"Roller","given":"N.E.G.","email":"","affiliations":[],"preferred":false,"id":299770,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1014437,"text":"1014437 - 1978 - Recent advances in nutrition of salmonids","interactions":[],"lastModifiedDate":"2012-02-02T00:04:10","indexId":"1014437","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3330,"text":"Salmonid","active":true,"publicationSubtype":{"id":10}},"title":"Recent advances in nutrition of salmonids","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Salmonid","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TL","usgsCitation":"Rumsey, G.L., 1978, Recent advances in nutrition of salmonids: Salmonid, v. 2, no. 4, p. 14-17, 21, 26.","productDescription":"p. 14-17, 21, 26","startPage":"14","endPage":"17, 21, 26","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643a95","contributors":{"authors":[{"text":"Rumsey, G. L.","contributorId":80604,"corporation":false,"usgs":true,"family":"Rumsey","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169257,"text":"70169257 - 1978 - Amplitude of foreshocks as a possible seismic precursor to earthquakes","interactions":[],"lastModifiedDate":"2016-04-05T15:40:30","indexId":"70169257","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Amplitude of foreshocks as a possible seismic precursor to earthquakes","docAbstract":"<p>In recent years, we have made significant progress in being able to recognize the long-range pattern of events that precede large earthquakes. For example, in a recent issue of the&nbsp;<i>Earthquake Information Bulletin,</i> we saw how the pioneering work of S.A. Fedotov of the U.S.S.R in the Kamchatka-Kurile Islands region has been applied worldwide to forecast where large, shallow earthquakes might occur in the next decades. Indeed, such a \"seismic gap\" off the coast of Alaska was filled by the 1972 Sitka earthquake. Promising results are slowly accumulating from other techniques that suggest that intermediate-term precursors might also be seen: among these are tilt and geomagnetic anomalies and anomalous land uplift. But the crucial point remains that short-term precursors (days to hours) will be needed in many cases if there is to be a significant saving of lives.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Lindh, A., 1978, Amplitude of foreshocks as a possible seismic precursor to earthquakes: Earthquake Information Bulletin (USGS), v. 10, no. 5, p. 162-164.","productDescription":"3 p.","startPage":"162","endPage":"164","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be2be4b0f59b85e02d97","contributors":{"authors":[{"text":"Lindh, A.G.","contributorId":24784,"corporation":false,"usgs":true,"family":"Lindh","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":623400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":96541,"text":"96541 - 1978 - Proceedings of a workshop on techniques of rehabilitation and erosion control in recently roaded and logged watersheds, with emphasis to north coastal California. March 13-14, 1978","interactions":[],"lastModifiedDate":"2018-03-21T14:54:07","indexId":"96541","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Proceedings of a workshop on techniques of rehabilitation and erosion control in recently roaded and logged watersheds, with emphasis to north coastal California. March 13-14, 1978","docAbstract":"No abstract available at this time","language":"English","publisher":"National Park Service, Redwood National Park, Resources Management Div.","publisherLocation":"Arcata, CA","usgsCitation":"Madej, M.A., and Kelsey, H., 1978, Proceedings of a workshop on techniques of rehabilitation and erosion control in recently roaded and logged watersheds, with emphasis to north coastal California. March 13-14, 1978, 89 p.","productDescription":"89 p.","startPage":"89","numberOfPages":"89","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":127742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66061c","contributors":{"authors":[{"text":"Madej, Mary Ann 0000-0003-2831-3773 mary_ann_madej@usgs.gov","orcid":"https://orcid.org/0000-0003-2831-3773","contributorId":40304,"corporation":false,"usgs":true,"family":"Madej","given":"Mary","email":"mary_ann_madej@usgs.gov","middleInitial":"Ann","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":299785,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelsey, H.M.","contributorId":84300,"corporation":false,"usgs":true,"family":"Kelsey","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":299786,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":93991,"text":"93991 - 1978 - Alternative sources of vitamin C for channel catfish","interactions":[],"lastModifiedDate":"2012-02-02T00:03:53","indexId":"93991","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Alternative sources of vitamin C for channel catfish","docAbstract":"No abstract available at this time","language":"English","publisher":"Department of Grain, Science and Industry, Kansas Agricultural Experiment Station","publisherLocation":"Manhattan, KS","collaboration":"None/FF","usgsCitation":"Brandt, T., Deyoe, C., and Seib, P., 1978, Alternative sources of vitamin C for channel catfish.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":127185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687387","contributors":{"authors":[{"text":"Brandt, T.M.","contributorId":91432,"corporation":false,"usgs":true,"family":"Brandt","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":298338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deyoe, C.W.","contributorId":28189,"corporation":false,"usgs":true,"family":"Deyoe","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":298336,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seib, P.A.","contributorId":43294,"corporation":false,"usgs":true,"family":"Seib","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":298337,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70169263,"text":"70169263 - 1978 - Water-level monitoring in the area of the Palmdale Uplift, Southern California","interactions":[],"lastModifiedDate":"2016-04-05T16:15:39","indexId":"70169263","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Water-level monitoring in the area of the Palmdale Uplift, Southern California","docAbstract":"<p>Abnormal behavior of water levels in wells has been observed prior to a number of earthquakes. For instance, water-level minima have been noted in the Cienega Winery well before earthquakes on the San Andreas fault. Abnormal water-level fluctuations were used in conjunctions with other precursors to predict the February 4, 1975, Haicheng earthquake in northeastern China. That such changes should occur prior to earthquakes is not surprising. Ground water that occupies the void spaces in porous rocks or alluvium can be expected to rise in wells when an aquifer is squeezed and fall when it is distended. COnfined aquifers, in particualr, have been found to be highly sensitive to Earth strain changes.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Lamar, D., and Merifield, P., 1978, Water-level monitoring in the area of the Palmdale Uplift, Southern California: Earthquake Information Bulletin (USGS), v. 10, no. 4, p. 144-147.","productDescription":"4 p.","startPage":"144","endPage":"147","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319256,"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              -117.09228515624999,\n              32.52828936482526\n            ],\n            [\n              -115.1806640625,\n              32.713355353177555\n            ],\n            [\n              -115.631103515625,\n              35.51434313431818\n            ],\n            [\n              -119.53125,\n              34.95799531086792\n            ],\n            [\n              -118.39965820312499,\n              32.46342595776104\n            ],\n            [\n              -117.09228515624999,\n              32.52828936482526\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be57e4b0f59b85e02f66","contributors":{"authors":[{"text":"Lamar, D.L.","contributorId":53801,"corporation":false,"usgs":true,"family":"Lamar","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":623410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merifield, P.M.","contributorId":69557,"corporation":false,"usgs":true,"family":"Merifield","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":623411,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70169267,"text":"70169267 - 1978 - Radon emanation on the San Andreas Fault","interactions":[],"lastModifiedDate":"2016-04-05T16:49:47","indexId":"70169267","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Radon emanation on the San Andreas Fault","docAbstract":"<p>Radon is a radioactive gas with a half-life of 3.8 days. (Half-life is the time required for the substance to lose half of its radioactivity by decay.) It is itself produced by the decay of uranium. Radon is constantly emanated from the Earth into the atmosphere. Many cases are known where anomalously large amounts of radon have been given off along active faults. THe radon emanation has shown variations with time that are related to changing atmospheric conidtions and possibly to nearby seismic activity.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"King, C.Y., 1978, Radon emanation on the San Andreas Fault: Earthquake Information Bulletin (USGS), v. 10, no. 4, p. 136-138.","productDescription":"3 p.","startPage":"136","endPage":"138","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319251,"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              -121.36322021484374,\n              36.93013456125331\n            ],\n            [\n              -121.49368286132812,\n              36.85435108768685\n            ],\n            [\n              -121.09954833984374,\n              36.41465185677695\n            ],\n            [\n              -120.9814453125,\n              36.477619571094515\n            ],\n            [\n              -121.36322021484374,\n              36.93013456125331\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be49e4b0f59b85e02ed1","contributors":{"authors":[{"text":"King, C. Y.","contributorId":167759,"corporation":false,"usgs":false,"family":"King","given":"C.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":623417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012492,"text":"70012492 - 1978 - Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary","interactions":[],"lastModifiedDate":"2023-02-01T17:40:47.965072","indexId":"70012492","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":664,"text":"Advances in Water Resources","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Empirical model of <i>Skeletonema costatum</i> photosynthetic rate, with applications in the San Francisco Bay estuary","title":"Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary","docAbstract":"<p>An empirical model of<span>&nbsp;</span><i>Skeletonema costatum</i><span>&nbsp;</span>photosynthetic rate is developed and fit to measurements of photosynthesis selected from the literature. Because the model acknowledges existence of: 1) a light-temperature interaction (by allowing optimum irradiance to vary with temperature), 2) light inhibition, 3) temperature inhibition, and 4) a salinity effect, it accurately estimates photosynthetic rates measured over a wide range of temperature, light intensity, and salinity. Integration of predicted instantaneous rate of photosynthesis with time and depth yields daily net carbon assimilation (pg C cell<sup>−1</sup><span>&nbsp;</span>day<sup>−1</sup>) in a mixed layer of specified depth, when salinity, temperature, daily irradiance and extinction coefficient are known. The assumption of constant carbon quota (pg C cell<sup>−1</sup>) allows for prediction of mean specific growth rate (day<sup>−1</sup>), which can be used in numerical models of<span>&nbsp;</span><i>Skeletonema costatum</i><span>&nbsp;</span>population dynamics.</p><p>Application of the model to northern San Francisco Bay clearly demonstrates the limitation of growth by low light availability, and suggests that large population densities of<span>&nbsp;</span><i>S. costatum</i><span>&nbsp;</span>observed during summer months are not the result of active growth in the central deep channels (where growth rates are consistently predicted to be negative). But predicted growth rates in the lateral shallows are positive during summer and fall, thus offering a testable hypothesis that shoals are the only sites of active population growth by<span>&nbsp;</span><i>S. costatum</i><span>&nbsp;</span>(and perhaps other neritic diatoms) in the northern reach of San Francisco Bay.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0309-1708(78)90040-4","usgsCitation":"Cloern, J.E., 1978, Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary: Advances in Water Resources, v. 1, no. 5, p. 267-274, https://doi.org/10.1016/0309-1708(78)90040-4.","productDescription":"8 p.","startPage":"267","endPage":"274","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":222256,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.22039965621613,\n              38.24440703031118\n            ],\n            [\n              -122.57745968735097,\n              38.24440703031118\n            ],\n            [\n              -122.57745968735097,\n              37.3957605043622\n            ],\n            [\n              -121.22039965621613,\n              37.3957605043622\n            ],\n            [\n              -121.22039965621613,\n              38.24440703031118\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"1","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a090ce4b0c8380cd51d98","contributors":{"authors":[{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":363746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197177,"text":"70197177 - 1978 - Paleomagnetic evidence for a Late Cretaceous deformation of the Great Valley Sequence, Sacramento Valley, California","interactions":[],"lastModifiedDate":"2018-05-18T15:40:22","indexId":"70197177","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"Paleomagnetic evidence for a Late Cretaceous deformation of the Great Valley Sequence, Sacramento Valley, California","docAbstract":"<p>Paleomagnetic samples from five localities within the Great Valley sequence range in age from Late Jurassic to Late Cretaceous. All samples possess normal polarity, and alternating-field demagnetization experiments show that the remanence was acquired after the sequence was folded. A mean paleomagnetic pole position determined from 17 demagnetized samples is located at 72° N., 181° E., with the radius of the 95-percent circle of confidence equal to 5.4°. This pole position agrees very well with known Cretaceous poles from North America, a fact indicating that the deformation and remagnetization of the sequence must have occurred during the Late Cretaceous.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Mankinen, E.A., 1978, Paleomagnetic evidence for a Late Cretaceous deformation of the Great Valley Sequence, Sacramento Valley, California: Journal of Research of the U.S. Geological Survey, v. 6, no. 3, p. 383-390.","productDescription":"8 p.","startPage":"383","endPage":"390","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354345,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":354344,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue3/report.pdf#page=103"}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley","volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff4d95e4b0da30c1bfdc37","contributors":{"authors":[{"text":"Mankinen, Edward A. 0000-0001-7496-2681 emank@usgs.gov","orcid":"https://orcid.org/0000-0001-7496-2681","contributorId":1054,"corporation":false,"usgs":true,"family":"Mankinen","given":"Edward","email":"emank@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":735916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169277,"text":"70169277 - 1978 - Tiltmeter studies in earthquake prediction","interactions":[],"lastModifiedDate":"2016-04-07T16:21:07","indexId":"70169277","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Tiltmeter studies in earthquake prediction","docAbstract":"<p>Our knowledge is still very limited as to the way in which the Earth's surface deforms around active faults and why it does so. By far the easiest method of providing clues to the mechanisms involved is to record the associated pattern of tilt of the Earth's surface.&nbsp;</p>\n<p>tilt measurements give us a means of monitoring vertical displacements or local uplift of the crust. The simplest type of tiltmeter is a stationary pendulum (fig. 1). As the Earth's surface distorts locally, the pendulum housing is tilted while, of course, the pendulum continues to hang vertically (that is, in the direction of the gravity vector). The tilt angle is the angle through which the pendulum housing is tilted. The pendulum is the inertial reference (the force of gravity remains unchanged at the site), and tilting of the instrument housing represents the moving reference frame. We note in passing that the tiltmeter could also be used to measure the force of gravity by using the pendulum in the same way as Henry Kater did in his celebrated measurement of <i>g</i> in 1817.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Johnston, M., 1978, Tiltmeter studies in earthquake prediction: Earthquake Information Bulletin (USGS), v. 10, no. 5, p. 182-186.","productDescription":"5 p.","startPage":"182","endPage":"186","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319245,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be55e4b0f59b85e02f4e","contributors":{"authors":[{"text":"Johnston, M.","contributorId":88091,"corporation":false,"usgs":true,"family":"Johnston","given":"M.","email":"","affiliations":[],"preferred":false,"id":623439,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169278,"text":"70169278 - 1978 - Tectonomagnetic effects","interactions":[],"lastModifiedDate":"2016-04-07T16:29:58","indexId":"70169278","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Tectonomagnetic effects","docAbstract":"<p>Measurements of the actual stress within the Earth and its changes with time are very difficult. It is much easier to monitor the direct effects of this stress, such as ground strain, or the indirect effects, such as changes in resistivity, strain, changes in seismic velocity or changes in magnetic field, and so forth. The latter technique is one of the more promising methods for monitoring substantial volumes of the Earth's crust near active faults with only a few instruments. It derives from the piezomagnetic properties of rocks (that is, the change in rock magnetization and, therefore, local magnetic field due to a change in applied stress). AS stress and strain fields along active faults vary, these variations should be reflected in changing local magnetic fields. In particular, rapidly changing fields might be expected to occur just before a large earthquake.</p>\n<p>We know that earthquakes result from the sudden release of elastic strain, the end product, most likely, of a long period of gradual stress accumulation in the crust. At the U.S Geological Survey, our magnetic fields studies have two main directions. First, a determination of the magnetic behavior accompanying shallow earthquakes (seismomagnetic effects). Second, a long-term monitoring of the magnetic field in the vicinity of an active fault to detect magnetic changes due to general tectonic activity, particularly that which ultimately leads to earthquakes. These magnetic changes are generally termed \"tectonomagnetic effects.\"&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Johnston, M., 1978, Tectonomagnetic effects: Earthquake Information Bulletin (USGS), v. 10, no. 3, p. 82-87.","productDescription":"6 p.","startPage":"82","endPage":"87","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319244,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be52e4b0f59b85e02f1b","contributors":{"authors":[{"text":"Johnston, M.","contributorId":88091,"corporation":false,"usgs":true,"family":"Johnston","given":"M.","email":"","affiliations":[],"preferred":false,"id":623440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169279,"text":"70169279 - 1978 - Continuous strain measurements near the San Andreas Fault","interactions":[],"lastModifiedDate":"2016-04-07T16:39:16","indexId":"70169279","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Continuous strain measurements near the San Andreas Fault","docAbstract":"<p>Changes in the state of stress in the Earth's crust produces corresponding changes in the state of strain and may result, as a consequence, in damaging earthquakes. Monitoring ground strain can, therefore, help us in understanding how stress changes occur and when they are likely to lead to this kind of abrupt release of seismic energy.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Johnston, M., 1978, Continuous strain measurements near the San Andreas Fault: Earthquake Information Bulletin (USGS), v. 10, no. 5, p. 187-191.","productDescription":"5 p.","startPage":"187","endPage":"191","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319243,"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              -121.42776489257811,\n              36.994875229523814\n            ],\n            [\n              -121.57882690429688,\n              36.935623193306064\n            ],\n            [\n              -121.58981323242188,\n              36.870832155646326\n            ],\n            [\n              -121.38107299804686,\n              36.712467243386264\n            ],\n            [\n              -121.19018554687499,\n              36.815881441097154\n            ],\n            [\n              -121.42776489257811,\n              36.994875229523814\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be2ee4b0f59b85e02db2","contributors":{"authors":[{"text":"Johnston, M.","contributorId":88091,"corporation":false,"usgs":true,"family":"Johnston","given":"M.","email":"","affiliations":[],"preferred":false,"id":623441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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