{"pageNumber":"4457","pageRowStart":"111400","pageSize":"25","recordCount":184812,"records":[{"id":25278,"text":"25278 - 1990 - Treatment of chlorophenol-contaminated water and soils using immobilized microorganisms","interactions":[],"lastModifiedDate":"2014-07-08T16:12:39","indexId":"25278","displayToPublicDate":"1990-01-01T16:11:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Treatment of chlorophenol-contaminated water and soils using immobilized microorganisms","docAbstract":"No abstract available.","language":"English","publisher":"BioTrol Inc.","publisherLocation":"Earth City, MO","doi":"10.3133/25278","issn":"0364-7064","usgsCitation":"Crawford, R.L., and Chresand, T.J., 1990, Treatment of chlorophenol-contaminated water and soils using immobilized microorganisms, ii, 26 p., https://doi.org/10.3133/25278.","productDescription":"ii, 26 p.","numberOfPages":"28","costCenters":[],"links":[{"id":289571,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bd12fbe4b00cbf31f72366","contributors":{"authors":[{"text":"Crawford, Ronald L.","contributorId":24279,"corporation":false,"usgs":true,"family":"Crawford","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chresand, Thomas J.","contributorId":33624,"corporation":false,"usgs":true,"family":"Chresand","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":193365,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70241997,"text":"70241997 - 1990 - Chapter 21: Neodymium, strontium, and trace-element evidence of crustal anatexis and magma mixing in the Idaho batholith","interactions":[],"lastModifiedDate":"2023-04-03T21:11:23.853533","indexId":"70241997","displayToPublicDate":"1990-01-01T15:57:54","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter 21: Neodymium, strontium, and trace-element evidence of crustal anatexis and magma mixing in the Idaho batholith","docAbstract":"<p>Variations in initial<span>&nbsp;</span><sup>143</sup>Nd/<sup>144</sup><span>&nbsp;</span>Nd in Late Cretaceous plutonic rocks along the South Fork of the Clearwater River (SFCR) supplement results of Sr and O studies, which demonstrate large-scale mixing in magmas forming the western margin of the Idaho batholith. These marginal or border phases of the batholith span the terrane boundary between Proterozoic crust of North America and late Paleozoic-Mesozoic intraoceanic arc terranes (WSD terranes), delineated by the Western Idaho suture zone (or WISZ).<span>&nbsp;</span><sup>ɛ</sup>Nd<sup>(t)</sup><span>&nbsp;</span>values in Early Cretaceous and older, pre-accretionary plutons of the WSD range from +3 to +7.6, and average +5.7. Proterozoic orthogneisses and metasedimentary rocks range from -7.4 to -13.7 and -10.45 to -15.7, respectively.<span>&nbsp;</span><sup>ɛ</sup>Nd<sup>(t)</sup><span>&nbsp;</span>in Late Cretaceous plutons of the SFCR decreases abruptly from west to east near the WISZ, varying inversely with ɛSr<sup>(t)</sup>. Although Sr isotopic evidence (Fleck and Criss, 1985) is consistent with a binary mixing model, Sm-Nd results modify those conclusions, suggesting that SFCR plutons may be divided into three groups. Group 1 plutons occur in a narrow zone (&lt;4 km width) along the suture zone (WISZ). These bodies probably represent at least three-component mixtures of very high-Sr, arc-type magmas, one or more Proterozoic crustal components that may include lower crust, and a high-Nb, high-Zr component. Group 2 plutons are characterized by high ɛSr<sup>(t)</sup>.and nearly constant, low ɛNd<sup>(t)</sup>. These bodies are thought to represent mixtures of deep-seated partial melts of two different Proterozoic lithospheric types, possibly representing upper and lower crust. Plutons belonging to Group 3 have ɛNd<sup>(t)</sup>.values &lt;-14 and probably incorporated substantial amounts of Proterozoic metasedimentary rocks, but mixing components are poorly defined.</p><p>Trace-element variations in SFCR rocks also reflect the arc terrane-continental crustal boundary as Nb, Zr, and Nd increase dramatically, whereas Sr, Rb/Nb, and Sm/Nd exhibit coincident decreases east of the WISZ. Modeling of these variations with the isotopic variations in Nd and Sr supports mixing, but precludes contamination-bulk-assimilation models. Correlated ɛNd, ɛSr, and δ<sup>18</sup>O within the SFCR favors mixing of crustal and subcrustal magmas rather than derivation of the melts entirely from subcontinental lithosphere.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The nature and origin of Cordilleran magmatism","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM174-p359","usgsCitation":"Fleck, R.J., 1990, Chapter 21: Neodymium, strontium, and trace-element evidence of crustal anatexis and magma mixing in the Idaho batholith, chap. <i>of</i> The nature and origin of Cordilleran magmatism, v. 174, p. 359-374, https://doi.org/10.1130/MEM174-p359.","productDescription":"16 p.","startPage":"359","endPage":"374","costCenters":[],"links":[{"id":415125,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.72255873206723,\n              47.96477348100723\n            ],\n            [\n              -118.72255873206723,\n              43.0950493093458\n            ],\n            [\n              -111.05361477858645,\n              43.0950493093458\n            ],\n            [\n              -111.05361477858645,\n              47.96477348100723\n            ],\n            [\n              -118.72255873206723,\n              47.96477348100723\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"174","noUsgsAuthors":false,"publicationDate":"1990-01-01","publicationStatus":"PW","contributors":{"editors":[{"text":"Anderson, J. Lawford","contributorId":7275,"corporation":false,"usgs":true,"family":"Anderson","given":"J.","email":"","middleInitial":"Lawford","affiliations":[],"preferred":false,"id":868479,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Fleck, Robert J. 0000-0002-3149-8249 fleck@usgs.gov","orcid":"https://orcid.org/0000-0002-3149-8249","contributorId":1048,"corporation":false,"usgs":true,"family":"Fleck","given":"Robert","email":"fleck@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":868478,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70241996,"text":"70241996 - 1990 - Chapter 15: Two different lithosphere types in the Sierra Nevada, California","interactions":[],"lastModifiedDate":"2023-04-03T20:57:23.991707","indexId":"70241996","displayToPublicDate":"1990-01-01T15:50:01","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter 15: Two different lithosphere types in the Sierra Nevada, California","docAbstract":"<p>Chemical and isotopic characteristics of plutons in the western United States reflect compositions and protoliths of subjacent source materials. A discontinuously exposed shear zone that extends along the length of the Sierra Nevada in California marks a boundary between two areas manifested geologically by wall-rock and roof-pendant lithologies of different ages, depositional environments, and structural histories. In addition, plutons on either side of the boundary have different chemical and isotopic compositions, which indicate that their source regions are of two fundamentally different lithosphere types. The western lithosphere type is called Panthalassan, whereas the eastern type is called North American.</p><p>Isotopic investigations of plutons have defined an initial<span>&nbsp;</span><sup>87</sup>Sr/<sup>86</sup>Sr (Sr<sub>i</sub>) = 0.706 line in each lithosphere type. However, δ<sup>18</sup>O more than +9 per mil in plutons with Sr<sub>i</sub><span>&nbsp;</span>greater than 0.706 in the Panthalassan lithosphere indicates a significantly greater sedimentary component in the source materials for these plutons than for those plutons with similar Sr<sub>i</sub><span>&nbsp;</span>but δ<sup>18</sup>O less than +9 per mil intruded into North American lithosphere. In contrast to the North American lithosphere, there is no evidence that a Proterozoic crystalline sialic basement exists where plutons have Sr<sub>i</sub><span>&nbsp;</span>greater than 0.706 in the Panthalassan lithosphere. Instead, the plutons with Sr<sub>i</sub><span>&nbsp;</span>greater than 0.706 intruded into Panthalassan lithosphere probably acquired that characteristic by assimilation of sediments derived from a Proterozoic sialic crust.</p><p>Plutons with Sr<sub>i</sub><span>&nbsp;</span>less than 0.706 have chemical and Nd isotopic characteristics that indicate time-integrated depletion in large ion lithophile elements in their source regions in the Panthalassan lithosphere relative to their sources in the North American lithosphere.</p><p>The tectonic contact between the two lithosphere types may be the extension of the Sonora-Mojave megashear into northern California.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The nature and origin of Cordilleran magmatism","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM174-p271","usgsCitation":"Kistler, R., 1990, Chapter 15: Two different lithosphere types in the Sierra Nevada, California, chap. <i>of</i> The nature and origin of Cordilleran magmatism, v. 174, p. 271-282, https://doi.org/10.1130/MEM174-p271.","productDescription":"12 p.","startPage":"271","endPage":"282","costCenters":[],"links":[{"id":415109,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.80311909334307,\n              35.67967867440433\n            ],\n            [\n              -118.27941246479301,\n              37.217050651643916\n            ],\n            [\n              -118.5391015788071,\n              37.594563769042765\n            ],\n            [\n              -118.8844118660345,\n              37.75225053631934\n            ],\n            [\n              -119.14711639816923,\n              38.4413482207849\n            ],\n            [\n              -120.00639907494747,\n              39.04033081724296\n            ],\n            [\n              -120.01808171128948,\n              40.065561099062705\n            ],\n            [\n              -121.03109061401318,\n              41.13365961302503\n            ],\n            [\n              -121.8333522558508,\n              41.04287144268798\n            ],\n            [\n              -122.20670849473268,\n              40.65226720719656\n            ],\n            [\n              -121.97952921615854,\n              39.722454345523715\n            ],\n            [\n              -121.11054971843856,\n              38.726852715308155\n            ],\n            [\n              -120.18051771158133,\n              37.63479941611946\n            ],\n            [\n              -119.57756240555739,\n              36.965563780650285\n            ],\n            [\n              -119.34933173045462,\n              36.60899874198313\n            ],\n            [\n              -118.96420772126595,\n              36.25100169979511\n            ],\n            [\n              -118.86871605842819,\n              35.18450304517211\n            ],\n            [\n              -118.21809028354033,\n              35.08551984107308\n            ],\n            [\n              -117.6036883313721,\n              35.45393852346898\n            ],\n            [\n              -117.80311909334307,\n              35.67967867440433\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"174","noUsgsAuthors":false,"publicationDate":"1990-01-01","publicationStatus":"PW","contributors":{"editors":[{"text":"Anderson, J. Lawford","contributorId":7275,"corporation":false,"usgs":true,"family":"Anderson","given":"J.","email":"","middleInitial":"Lawford","affiliations":[],"preferred":false,"id":868477,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Kistler, Ronald W.","contributorId":56969,"corporation":false,"usgs":true,"family":"Kistler","given":"Ronald W.","affiliations":[],"preferred":false,"id":868476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33504,"text":"b1748 - 1990 - Mineral resources of wilderness study areas: the Cockscomb Region, Utah","interactions":[{"subject":{"id":47486,"text":"b1748A - 1990 - Mineral resources of the Cockscomb and Wahweap Wilderness Study Areas, Kane County, Utah","indexId":"b1748A","publicationYear":"1990","noYear":false,"chapter":"A","title":"Mineral resources of the Cockscomb and Wahweap Wilderness Study Areas, Kane County, Utah"},"predicate":"IS_PART_OF","object":{"id":33504,"text":"b1748 - 1990 - Mineral resources of wilderness study areas: the Cockscomb Region, Utah","indexId":"b1748","publicationYear":"1990","noYear":false,"title":"Mineral resources of wilderness study areas: the Cockscomb Region, Utah"},"id":1},{"subject":{"id":52691,"text":"b1748B - 1991 - Mineral resources of the Paria-Hackberry Wilderness Study Area, Kane County, Utah","indexId":"b1748B","publicationYear":"1991","noYear":false,"chapter":"B","title":"Mineral resources of the Paria-Hackberry Wilderness Study Area, Kane County, Utah"},"predicate":"IS_PART_OF","object":{"id":33504,"text":"b1748 - 1990 - Mineral resources of wilderness study areas: the Cockscomb Region, Utah","indexId":"b1748","publicationYear":"1990","noYear":false,"title":"Mineral resources of wilderness study areas: the Cockscomb Region, Utah"},"id":2}],"lastModifiedDate":"2014-07-07T15:51:56","indexId":"b1748","displayToPublicDate":"1990-01-01T15:48:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1748","title":"Mineral resources of wilderness study areas: the Cockscomb Region, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1748","usgsCitation":"U.S. Government Printing Office, 1990, Mineral resources of wilderness study areas: the Cockscomb Region, Utah: U.S. Geological Survey Bulletin 1748, 2 v., https://doi.org/10.3133/b1748.","productDescription":"2 v.","costCenters":[],"links":[{"id":289495,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Cockscomb","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.0669,37.3604 ], [ -112.0669,37.6437 ], [ -111.5546,37.6437 ], [ -111.5546,37.3604 ], [ -112.0669,37.3604 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bbc17de4b084059e8bfeeb"}
,{"id":70241995,"text":"70241995 - 1990 - Chapter 7: Jurassic granitoids and related rocks of the southern Bristol Mountains, southern Providence Mountains, and Colton Hills, Mojave Desert, California","interactions":[],"lastModifiedDate":"2023-04-03T20:45:46.192064","indexId":"70241995","displayToPublicDate":"1990-01-01T15:35:23","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter 7: Jurassic granitoids and related rocks of the southern Bristol Mountains, southern Providence Mountains, and Colton Hills, Mojave Desert, California","docAbstract":"<p><span>Jurassic plutons in the east-central Mojave Desert region are markedly different from older and younger Mesozoic plutons in the region. They form a chemically and texturally heterogeneous group that ranges in composition from diorite to syenogranite; some phases are alkalic. Igneous rocks in the southern Bristol Mountains, southern Providence Mountains, and Colton Hills are subdivided into five broadly defined groups on the basis of field relations and geochemistry: mafic intrusive rocks; mixed intrusive rocks, consisting of subequigranular and porphyritic subgroups; felsic intrusive rocks; metavolcanic and hypabyssal rocks; and dikes. There is a general trend from older, more mafic and heterogeneous rocks to younger, more felsic and homogeneous plutonic phases. Extreme spatial variations in composition and texture and other field relations indicate that the plutons were intruded during a relatively short time span. Field relations also indicate that the plutons were intruded at upper crustal levels. The plutons were affected by extensive late- or early post-magmatic sodium metasomatism (albitization), which resulted from the introduction and circulation of predominantly meteoric fluids. We propose that the plutons in this region were derived from compositionally heterogeneous but genetically related magmas generated from an upper mantle/lower crustal amphibolitic source. Similar Jurassic rocks are found elsewhere in the southern Cordillera, indicating that the genesis of these unusual rocks is a regional phenomenon.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The nature and origin of Cordilleran magmatism","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM174-p111","usgsCitation":"Fox, L., and Miller, D., 1990, Chapter 7: Jurassic granitoids and related rocks of the southern Bristol Mountains, southern Providence Mountains, and Colton Hills, Mojave Desert, California, chap. <i>of</i> The nature and origin of Cordilleran magmatism, v. 174, p. 111-132, https://doi.org/10.1130/MEM174-p111.","productDescription":"22 p.","startPage":"111","endPage":"132","costCenters":[],"links":[{"id":415107,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Bristol Mountains, Colton Hills, Mojave Desert, Providence Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.17584352801589,\n              35.61009137164501\n            ],\n            [\n              -116.17584352801589,\n              34.26752643651733\n            ],\n            [\n              -115.06232606106683,\n              34.26752643651733\n            ],\n            [\n              -115.06232606106683,\n              35.61009137164501\n            ],\n            [\n              -116.17584352801589,\n              35.61009137164501\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"174","noUsgsAuthors":false,"publicationDate":"1990-01-01","publicationStatus":"PW","contributors":{"editors":[{"text":"Anderson, J. Lawford","contributorId":7275,"corporation":false,"usgs":true,"family":"Anderson","given":"J.","email":"","middleInitial":"Lawford","affiliations":[],"preferred":false,"id":868475,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Fox, Lydia","contributorId":192666,"corporation":false,"usgs":false,"family":"Fox","given":"Lydia","email":"","affiliations":[],"preferred":false,"id":868473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, David M. 0000-0003-3711-0441 dmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":140769,"corporation":false,"usgs":true,"family":"Miller","given":"David M.","email":"dmiller@usgs.gov","affiliations":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":868474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006920,"text":"70006920 - 1990 - Evaluation of condition indices for estimation of growth of largemouth bass and white crappie","interactions":[],"lastModifiedDate":"2012-10-15T17:16:41","indexId":"70006920","displayToPublicDate":"1990-01-01T15:29:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of condition indices for estimation of growth of largemouth bass and white crappie","docAbstract":"We evaluated the ability of three condition indices-condition factor (<i>K</i>), relative condition (<i>K<sub>n</sub></i>), and relative weight (<i>W<sub>r</sub></i>)-to estimate annual growth rates of largemouth bass <i>Micropterus salmoides</i> and white crappies <i>Pomoxis annularis</i> collected during standardized autumn electrofishing and trap-net surveys of Texas reservoirs. Multiple-regression models for estimation of length increments from initial length (at the start of the growing season) and condition indices had R<sup>2</sup> values of 0.63-0.76 for largemouth bass and 0.46-0.83 for white crappie. However, these models are not useful for indirect estimation ofgrowth rates because growth must be known (initial length equals length at capture minus estimated annual growth). Models based on length at capture and condition indices had R<sup>2</sup> values of 0.22-0.68 for largemouth bass and less than 0.45 for white crappie. The low precision of models based on length at capture indicates that condition provides a weak basis for indirect estimation of growth rates from Texas reservoirs sampled during autumn and, therefore, is unreliable for detection of size-related growth phenomena such as \"stockpiling\" (size specific, density-dependent growth depression). Direct estimates of growth rates based on back-calculations or tagging data seem necessary for reliable detection of size-related growth patterns for largemouth bass and white crappies from Texas reservoirs.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8675(1990)010<0434:EOCIFE>2.3.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Gutreuter, S., and Childress, W.M., 1990, Evaluation of condition indices for estimation of growth of largemouth bass and white crappie: North American Journal of Fisheries Management, v. 10, no. 4, p. 434-441, https://doi.org/10.1577/1548-8675(1990)010<0434:EOCIFE>2.3.CO;2.","productDescription":"8 p.","startPage":"434","endPage":"441","numberOfPages":"8","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":262595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":262593,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8675(1990)010<0434:EOCIFE>2.3.CO;2"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50dc9fd4e4b0d55926e3e6b5","contributors":{"authors":[{"text":"Gutreuter, Steve","contributorId":91437,"corporation":false,"usgs":true,"family":"Gutreuter","given":"Steve","affiliations":[],"preferred":false,"id":355468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Childress, W. Michael","contributorId":6733,"corporation":false,"usgs":true,"family":"Childress","given":"W.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":355467,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":49452,"text":"ofr90244 - 1990 - Proceedings of conference XLIX: a meeting of the U.S. ad hoc working group on \"Earthquake related casualties\"; July 13, 1989, Baltimore, Maryland","interactions":[],"lastModifiedDate":"2018-07-24T15:55:06","indexId":"ofr90244","displayToPublicDate":"1990-01-01T15:21:00","publicationYear":"1990","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":"90-244","title":"Proceedings of conference XLIX: a meeting of the U.S. ad hoc working group on \"Earthquake related casualties\"; July 13, 1989, Baltimore, Maryland","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90244","usgsCitation":"1990, Proceedings of conference XLIX: a meeting of the U.S. ad hoc working group on \"Earthquake related casualties\"; July 13, 1989, Baltimore, Maryland: U.S. Geological Survey Open-File Report 90-244, vi, 147 p., https://doi.org/10.3133/ofr90244.","productDescription":"vi, 147 p.","costCenters":[],"links":[{"id":355960,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0244/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":355959,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0244/report-thumb.jpg","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c112801e4b034bf6a8200c4","contributors":{"compilers":[{"text":"Huey, Linda","contributorId":206500,"corporation":false,"usgs":true,"family":"Huey","given":"Linda","email":"","affiliations":[],"preferred":true,"id":740834,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Hays, Walter W.","contributorId":66669,"corporation":false,"usgs":true,"family":"Hays","given":"Walter W.","affiliations":[],"preferred":false,"id":740833,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":33490,"text":"b1753 - 1990 - Mineral resources of wilderness study areas: Central Green River Region, Utah","interactions":[{"subject":{"id":33346,"text":"b1753A - 1990 - Mineral resources of the Coal Canyon, Spruce Canyon, and Flume Canyon Wilderness Study Areas, Grand County, Utah","indexId":"b1753A","publicationYear":"1990","noYear":false,"chapter":"A","title":"Mineral resources of the Coal Canyon, Spruce Canyon, and Flume Canyon Wilderness Study Areas, Grand County, Utah"},"predicate":"IS_PART_OF","object":{"id":33490,"text":"b1753 - 1990 - Mineral resources of wilderness study areas: Central Green River Region, Utah","indexId":"b1753","publicationYear":"1990","noYear":false,"title":"Mineral resources of wilderness study areas: Central Green River Region, Utah"},"id":1},{"subject":{"id":47487,"text":"b1753B - 1990 - Mineral resources of the Desolation Canyon, Turtle Canyon, and Floy Canyon Wilderness Study Areas, Carbon, Emery, and Grand counties, Utah","indexId":"b1753B","publicationYear":"1990","noYear":false,"chapter":"B","title":"Mineral resources of the Desolation Canyon, Turtle Canyon, and Floy Canyon Wilderness Study Areas, Carbon, Emery, and Grand counties, Utah"},"predicate":"IS_PART_OF","object":{"id":33490,"text":"b1753 - 1990 - Mineral resources of wilderness study areas: Central Green River Region, Utah","indexId":"b1753","publicationYear":"1990","noYear":false,"title":"Mineral resources of wilderness study areas: Central Green River Region, Utah"},"id":2}],"lastModifiedDate":"2014-07-07T15:23:02","indexId":"b1753","displayToPublicDate":"1990-01-01T15:18:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1753","title":"Mineral resources of wilderness study areas: Central Green River Region, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1753","usgsCitation":"Dickerson, R.P., 1990, Mineral resources of wilderness study areas: Central Green River Region, Utah: U.S. Geological Survey Bulletin 1753, https://doi.org/10.3133/b1753.","costCenters":[],"links":[{"id":289491,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Green River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.053,36.9979 ], [ -114.053,42.0016 ], [ -109.0411,42.0016 ], [ -109.0411,36.9979 ], [ -114.053,36.9979 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bbc17ae4b084059e8bfee1","contributors":{"authors":[{"text":"Dickerson, Robert P.","contributorId":6461,"corporation":false,"usgs":true,"family":"Dickerson","given":"Robert","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":211362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047459,"text":"70047459 - 1990 - Digital line graphs from 1:24,000-scale maps","interactions":[],"lastModifiedDate":"2013-09-19T13:13:11","indexId":"70047459","displayToPublicDate":"1990-01-01T15:16:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":357,"text":"Data Users Guide","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"1","title":"Digital line graphs from 1:24,000-scale maps","docAbstract":"The Earth Science Information Centers (ESIC) distribute digital cartographic/geographic data files produced by the U.S. Geological Survey (USGS) as part of the National Mapping Program. Digital cartographic data flles are grouped into four basic types. The first of these, called a Digital Line . Graph (DLG), is line map information in digital form. These data files include information on planimetric base categories, such as transportation, hydrography, and boundaries. The second type, called a Digital Elevation Model (DEM), consists of a sampled array of elevations for a number of ground positions that are usually at regularly spaced intervals. The third type is Land Use and Land Cover digital data, which provides information on nine major classes of land use such as urban, agricultural, or forest as wen as associated map data such as political units and Federal land ownership. The fourth type, the Geographic Names Information System, provides primary information for all known places, features, and areas in the United States identified by a proper name.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70047459","usgsCitation":"U.S. Geological Survey National Mapping Division, 1990, Digital line graphs from 1:24,000-scale maps (Second printing (revised)): Data Users Guide 1, iv, 107 p., https://doi.org/10.3133/70047459.","productDescription":"iv, 107 p.","numberOfPages":"113","costCenters":[],"links":[{"id":277875,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047459/report.pdf"},{"id":276132,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047459/report-thumb.jpg"}],"edition":"Second printing (revised)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae2e4b0e21cafa49c38","contributors":{"authors":[{"text":"U.S. Geological Survey National Mapping Division","contributorId":128185,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey National Mapping Division","id":535573,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70216795,"text":"70216795 - 1990 - Transmissivity and well yields of the Upper Floridan aquifer in Florida","interactions":[],"lastModifiedDate":"2020-12-08T13:14:24.908555","indexId":"70216795","displayToPublicDate":"1990-01-01T15:13:33","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":7451,"text":"Florida Geological Survey Map Series","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"132","title":"Transmissivity and well yields of the Upper Floridan aquifer in Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Florida Geological Survey","usgsCitation":"Andrews, W.J., 1990, Transmissivity and well yields of the Upper Floridan aquifer in Florida: Florida Geological Survey Map Series 132, 1 Plate: 15.748 x 19.685 inches.","productDescription":"1 Plate: 15.748 x 19.685 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,{"id":70069025,"text":"70069025 - 1990 - Geology and mineral resources map of the South Mountain quadrangle, Malheur County, Oregon","interactions":[],"lastModifiedDate":"2014-01-13T14:59:49","indexId":"70069025","displayToPublicDate":"1990-01-01T14:52:11","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":254,"text":"Geologic Map Series","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"67","title":"Geology and mineral resources map of the South Mountain quadrangle, Malheur County, Oregon","language":"English","publisher":"Oregon Department of Geology and Mineral Industries","usgsCitation":"Evans, J.G., 1990, Geology and mineral resources map of the South Mountain quadrangle, Malheur County, Oregon: Geologic Map Series 67, 39.4 x 27.17 inches.","productDescription":"39.4 x 27.17 inches","costCenters":[],"links":[{"id":280915,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"scale":"24000","projection":"Lambert Conformal Conic","datum":"1927 North American Datum","country":"United States","state":"Oregon","county":"Malheur County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.875,43.75 ], [ -117.875,43.875 ], [ -117.75,43.875 ], [ -117.75,43.75 ], [ -117.875,43.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5de6e4b0b290850fb598","contributors":{"authors":[{"text":"Evans, James G. jevans@usgs.gov","contributorId":2396,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"jevans@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":488200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70241921,"text":"70241921 - 1990 - Development of slope valleys in the glacimarine environment of a complex subduction zone, Northern Gulf of Alaska","interactions":[],"lastModifiedDate":"2023-03-30T19:53:15.946894","indexId":"70241921","displayToPublicDate":"1990-01-01T14:39:01","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesTitle":{"id":11125,"text":"Special Papers of the Geological Society of London","active":true,"publicationSubtype":{"id":24}},"title":"Development of slope valleys in the glacimarine environment of a complex subduction zone, Northern Gulf of Alaska","docAbstract":"<p><span>Morphological, seismic-reflection, and sedimentological evidence indicates that glacial ice tongues cut large sea valleys into the Gulf of Alaska continental shelf during the Pleistocene. During the Holocene, glacially-derived sediments from the Copper River and other meltwater streams have been prograding seaward across the shelf, covering the glacial and glacimarine upper Yakataga diamicts that blanketed the shelf and accumulated on the upper slope seaward of the sea valleys during the Pleistocene. GLORIA imagery near Middleton Island provides a new perspective on the glacimarine depositional environment on the continental slope in a collision zone between the Pacific and North American plates. Southwest of Middleton Island, along the subduction margin, sinuous valleys funnel sediment around shelf-edge-parallel, subduction-created, anticlinal ridges that have deflected and locally trapped glacimarine sediment. The slope south and southeast of Middleton Island where oblique convergence occurs, is incised by dendritic, erosional gulley systems, contains no compressional ridges, and thus, the apparently active sediment pathways to the trench are unrestricted. However, below the sea valley mouths, apparently both glacial and glacimarine sediments blanket the upper slope, covering any dendritic gulley systems that may have formed during or since the Pleistocene low stands of sea level.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Glacimarine environments: Processes and sediments","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of London","doi":"10.1144/GSL.SP.1990.053.01.08","usgsCitation":"Carlson, P.R., Bruns, T.R., and Fisher, M.A., 1990, Development of slope valleys in the glacimarine environment of a complex subduction zone, Northern Gulf of Alaska, chap. <i>of</i> Glacimarine environments: Processes and sediments: Special Papers of the Geological Society of London, v. 53, p. 139-153, https://doi.org/10.1144/GSL.SP.1990.053.01.08.","productDescription":"15 p.","startPage":"139","endPage":"153","costCenters":[],"links":[{"id":414986,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska, Middleton Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -146.51063585535928,\n              59.53369695538194\n            ],\n            [\n              -146.51063585535928,\n              59.33022597265119\n            ],\n            [\n              -146.14027962132684,\n              59.33022597265119\n            ],\n            [\n              -146.14027962132684,\n              59.53369695538194\n            ],\n            [\n              -146.51063585535928,\n              59.53369695538194\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"53","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":868229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bruns, Terry R.","contributorId":29420,"corporation":false,"usgs":true,"family":"Bruns","given":"Terry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":868230,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, Michael A. mfisher@usgs.gov","contributorId":1991,"corporation":false,"usgs":true,"family":"Fisher","given":"Michael","email":"mfisher@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":868231,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70242055,"text":"70242055 - 1990 - Chapter 22: Changing patterns of extensional tectonics; Overprinting of the basin of the middle and upper Miocene Esmeralda Formation in western Nevada by younger structural basins","interactions":[],"lastModifiedDate":"2023-04-05T19:47:04.144312","indexId":"70242055","displayToPublicDate":"1990-01-01T14:32:46","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter 22: Changing patterns of extensional tectonics; Overprinting of the basin of the middle and upper Miocene Esmeralda Formation in western Nevada by younger structural basins","docAbstract":"<p><span>The middle and upper Miocene Esmeralda Formation of western Nevada was deposited in a continental basin that crops out over an area of about 2,000 km</span><sup>2</sup><span>. The formation consists of thin, westerly derived sedimentary rocks in the western three-quarters of the outcrop area and of thick (3+ km) easterly derived sedimentary rocks in the eastern quarter. Megabreccias along the eastern margin of the basin are interpreted as landslide deposits derived from fault scarps. The basin was probably a half-graben with a major fault or faults on the east side. The position of the basin, its size, and the inferred major syndepositional faults on its east side are all unrelated to present-day topography and the distribution of major faults in the area and indicate a change in paleogeography and structural pattern since the late Miocene. In the eastern part of the basin, this change was accompanied by deformation that includes low-angle-fault detachment of the Esmeralda Formation from underlying amphibolite-grade Late Proterozoic and lower Paleozoic rocks in the Mineral Ridge-Weepah Hills area and uplift, folding, faulting, tilting, and surface exposure of the entire 3+ km thickness of the formation. Middle and upper Miocene basins in the northern part of the Basin and Range province commonly have been attributed to the onset of basin-range tectonism. The tectonic history of the Esmeralda Formation, however, indicates that some of these basins do not occupy the same area, nor are they related to the same syndepositional faults, as present basins. The extensional basin of the Esmeralda Formation can be viewed either as an early structure in an evolving, but kinematically related, extensional terrane in which the distribution of basins and faults changed gradually with time, or as the product of an extensional event kinematically different from that which produced present structures in the same area. The latter hypothesis is favored because of the marked contrasts in the paleogeography and structures associated with the Esmeralda basin compared with modern basins.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Basin and Range extensional tectonics near the latitude of Las Vegas, Nevada","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM176-p447","usgsCitation":"Stewart, J.H., and Diamond, D.S., 1990, Chapter 22: Changing patterns of extensional tectonics; Overprinting of the basin of the middle and upper Miocene Esmeralda Formation in western Nevada by younger structural basins, chap. <i>of</i> Basin and Range extensional tectonics near the latitude of Las Vegas, Nevada, v. 176, p. 447-476, https://doi.org/10.1130/MEM176-p447.","productDescription":"30 p.","startPage":"447","endPage":"476","costCenters":[],"links":[{"id":415289,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Esmerelda County, Mineral County, Mono County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.30725359509913,\n              38.09179976780905\n            ],\n            [\n              -118.30725359509913,\n              37.46076186262489\n            ],\n            [\n              -117.18163912792792,\n              37.46076186262489\n            ],\n            [\n              -117.18163912792792,\n              38.09179976780905\n            ],\n            [\n              -118.30725359509913,\n              38.09179976780905\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"176","noUsgsAuthors":false,"publicationDate":"1990-01-01","publicationStatus":"PW","contributors":{"editors":[{"text":"Wernicke, Brian P.","contributorId":204208,"corporation":false,"usgs":false,"family":"Wernicke","given":"Brian","email":"","middleInitial":"P.","affiliations":[{"id":36877,"text":"Cal Tech","active":true,"usgs":false}],"preferred":false,"id":868711,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Stewart, John H.","contributorId":83086,"corporation":false,"usgs":true,"family":"Stewart","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":868709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Diamond, David S.","contributorId":303953,"corporation":false,"usgs":false,"family":"Diamond","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":868710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70242781,"text":"70242781 - 1990 - Lithology and evolution of the crust-mantle boundary region in the southwestern Basin and Range Province","interactions":[],"lastModifiedDate":"2023-04-17T19:38:32.599148","indexId":"70242781","displayToPublicDate":"1990-01-01T14:29:11","publicationYear":"1990","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":"Lithology and evolution of the crust-mantle boundary region in the southwestern Basin and Range Province","docAbstract":"<p><span>Mantle and crustal xenoliths from volcanic rocks in the southwestern Basin and Range province and Colorado Plateau Transition Zone reveal histories of episodic magmatism and deformation that have profoundly influenced the crustal structure of this region. Seismic transects in this area show a strongly reflective Moho of generally low relief, which, in the area of modern transects, consists of a thin zone (&lt;2 km thick) of short reflectors. The upper mantle is transparent and has a&nbsp;</span><i>P<sub>n</sub></i><span>&nbsp;of 7.8–8.0 km/s similar to much of the western United States. A lower crustal zone, 2–13 km thick, has variable internal reflectivity and a relatively low velocity of 6.6–6.8 km/s. Upper mantle peridotite xenoliths show both ductile and brittle deformational features and have structures and compositions affected by magmatic intrusion; intrusions form complex dike systems and extensive zones of grain boundary infiltration in peridotite xenoliths. Whereas melt infiltration preceded and followed ductile deformation, brittle deformation, represented by closely spaced joint systems and faults, followed ductile deformation and is related to the youngest magmatic episodes. These structural characteristics and high uppermost mantle temperature (∼1000°C) may combine to explain the relatively low&nbsp;</span><i>P<sub>n</sub></i><span>. Alternating layers of ductily deformed and undeformed peridotites, with or without igneous intrusions, may contribute to the reflectivity of the Moho. Lower crustal xenoliths are dominantly igneous-textured pyroxenites and mafic to intermediate gabbros identical to the dikes in peridotite xenoliths. The crustal xenoliths also commonly are jointed, and in addition many show partial melting and have abundant cavities that probably were filled with CO</span><sub>2</sub><span>-rich fluids. These rocks are interpreted as products of underplated magmas that were fed through the mantle dike systems and may represent the lowest crustal unit identified in the seismic records. The mafic compositions and high densities of the crustal xenoliths indicate that the low velocity of the lower crust may be caused in part by fracture systems, partial melts, and high temperatures. Garnet granulite xenoliths from a locality with no mantle peridotite xenoliths probably represent crust of the region before late Miocene extension. Felsic granulite xenoliths from two localities have velocities like those of the two lower crustal units identified seismically and could be present in the modern crust as unequilibrated remnants of old crust. The preferred model for the evolution of the lower lithosphere is one in which extension affects the upper mantle as well as the crust and is overlapped in time by multiple magmatic episodes. The earliest magmatic events preceded extension, and later events accompanied and followed extension.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB095iB01p00649","usgsCitation":"American Geophysical Union, 1990, Lithology and evolution of the crust-mantle boundary region in the southwestern Basin and Range Province: Journal of Geophysical Research B: Solid Earth, v. 95, no. B1, p. 649-665, https://doi.org/10.1029/JB095iB01p00649.","productDescription":"17 p.","startPage":"649","endPage":"665","costCenters":[],"links":[{"id":415875,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Nevada","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.2296009342291,\n              36.246520391919546\n            ],\n            [\n              -116.2296009342291,\n              33.5198044600661\n            ],\n            [\n              -112.71087969886685,\n              33.5198044600661\n            ],\n            [\n              -112.71087969886685,\n              36.246520391919546\n            ],\n            [\n              -116.2296009342291,\n              36.246520391919546\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"95","issue":"B1","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW"}
,{"id":33170,"text":"b1904 - 1990 - Contributions to Precambrian geology of Lake Superior region","interactions":[{"subject":{"id":33112,"text":"b1904T - 1995 - Archean and early Proterozoic tectonic framework of north-central United States and adjacent Canada","indexId":"b1904T","publicationYear":"1995","noYear":false,"chapter":"T","title":"Archean and early Proterozoic tectonic framework of north-central United States and adjacent Canada"},"predicate":"IS_PART_OF","object":{"id":33170,"text":"b1904 - 1990 - Contributions to Precambrian geology of Lake Superior region","indexId":"b1904","publicationYear":"1990","noYear":false,"title":"Contributions to Precambrian geology of Lake Superior region"},"id":1},{"subject":{"id":33114,"text":"b1904U - 1995 - Precambrian crustal blocks in Minnesota: Neodymium isotope evidence from basement and metasedimentary rocks","indexId":"b1904U","publicationYear":"1995","noYear":false,"chapter":"U","title":"Precambrian crustal blocks in Minnesota: Neodymium isotope evidence from basement and metasedimentary rocks"},"predicate":"IS_PART_OF","object":{"id":33170,"text":"b1904 - 1990 - Contributions to Precambrian geology of Lake Superior region","indexId":"b1904","publicationYear":"1990","noYear":false,"title":"Contributions to Precambrian geology of Lake Superior region"},"id":2},{"subject":{"id":47530,"text":"b1904CD - 1991 - Tectonic imbrication and foredeep development in the Penokean orogen, east-central Minnesota: An interpretation based on regional geophysics and the results of test-drilling.  The Penokean orogeny in Minnesota and upper Michigan; a comparison of structural geology","indexId":"b1904CD","publicationYear":"1991","noYear":false,"chapter":"C,D","title":"Tectonic imbrication and foredeep development in the Penokean orogen, east-central Minnesota: An interpretation based on regional geophysics and the results of test-drilling.  The Penokean orogeny in Minnesota and upper Michigan; a comparison of structural geology"},"predicate":"IS_PART_OF","object":{"id":33170,"text":"b1904 - 1990 - Contributions to Precambrian geology of Lake Superior region","indexId":"b1904","publicationYear":"1990","noYear":false,"title":"Contributions to Precambrian geology of Lake Superior region"},"id":3},{"subject":{"id":47587,"text":"b1904K - 1991 - Nature and style of deformation in the foreland of the early Proterozoic Penokean Orogen, northern Michigan","indexId":"b1904K","publicationYear":"1991","noYear":false,"chapter":"K","title":"Nature and style of deformation in the foreland of the early Proterozoic Penokean Orogen, northern Michigan"},"predicate":"IS_PART_OF","object":{"id":33170,"text":"b1904 - 1990 - Contributions to Precambrian geology of Lake Superior region","indexId":"b1904","publicationYear":"1990","noYear":false,"title":"Contributions to Precambrian geology of Lake Superior region"},"id":4},{"subject":{"id":47588,"text":"b1904L - 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,{"id":70123844,"text":"70123844 - 1990 - Brown trout population and habitat changes associated with increased minimum low flows in Douglas Creek, Wyoming","interactions":[],"lastModifiedDate":"2014-09-09T14:22:23","indexId":"70123844","displayToPublicDate":"1990-01-01T14:21:53","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"Biological Report 90(11)","title":"Brown trout population and habitat changes associated with increased minimum low flows in Douglas Creek, Wyoming","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Wolff, S., Wesche, T.A., Harris, D., and Hubert, W., 1990, Brown trout population and habitat changes associated with increased minimum low flows in Douglas Creek, Wyoming, 20 p.","productDescription":"20 p.","numberOfPages":"20","costCenters":[],"links":[{"id":293550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54101449e4b07ab1cd980894","contributors":{"authors":[{"text":"Wolff, S.W.","contributorId":30550,"corporation":false,"usgs":true,"family":"Wolff","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":500383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wesche, Thomas A.","contributorId":14595,"corporation":false,"usgs":true,"family":"Wesche","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":500382,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harris, D.D.","contributorId":59002,"corporation":false,"usgs":true,"family":"Harris","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":500384,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hubert, W.A.","contributorId":12822,"corporation":false,"usgs":true,"family":"Hubert","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":500381,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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,{"id":70242054,"text":"70242054 - 1990 - Chapter 10: Shallow crustal deformation in the Pahranagat area, southern Nevada","interactions":[],"lastModifiedDate":"2023-04-05T19:27:14.08515","indexId":"70242054","displayToPublicDate":"1990-01-01T14:14:56","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter 10: Shallow crustal deformation in the Pahranagat area, southern Nevada","docAbstract":"<p>The Pahranagat area lies in the Basin and Range Province of southern Nevada. Paleozoic rocks in the study area were folded and faulted during the Sevier orogeny and subsequently extended prior to deposition of Tertiary strata. Middle Oligocene strata overlie the Paleozoic rocks with pronounced angular unconformity and were deposited on rocks of Late Cambrian through Pennsylvanian age in the eastern part of the study area. Middle Oligocene and Miocene strata unconformably overlie lower Paleozoic and Precambrian strata in the western part of the study area.</p><p>In the eastern part of the study area, extension occurred prior to deposition of the middle Oligocene strata; the area was relatively stable between the middle Oligocene and latest Miocene, and there was renewed extension following the latest Miocene to present. There is a significant structural and stratigraphic break in Cenozoic rocks of the western part of the quadrangle where angular unconformities in the Tertiary section indicate extension continued intermittently during the late Oligocene and Miocene.</p><p>Faulting and folding that has formed the present Basin and Range topography of the study area is latest Miocene and/or younger in age. Fault scarps in alluvial deposits, active seismicity, and warm springs indicate the area is still tectonically active. The study area lies in a zone of northeast-southwest-trending structures characterized by structural, geophysical, and igneous trends that are referred to herein as the Escalante disrupted zone.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Basin and Range extensional tectonics near the latitude of Las Vegas, Nevada","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM176-p213","usgsCitation":"Jayko, A.S., 1990, Chapter 10: Shallow crustal deformation in the Pahranagat area, southern Nevada, chap. <i>of</i> Basin and Range extensional tectonics near the latitude of Las Vegas, Nevada, v. 176, p. 213-236, https://doi.org/10.1130/MEM176-p213.","productDescription":"24 p.","startPage":"213","endPage":"236","costCenters":[],"links":[{"id":415285,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Pahranagat area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -115.99398730715728,\n              37.61369299951804\n            ],\n            [\n              -115.99398730715728,\n              37.00252475424658\n            ],\n            [\n              -114.74808446309268,\n              37.00252475424658\n            ],\n            [\n              -114.74808446309268,\n              37.61369299951804\n            ],\n            [\n              -115.99398730715728,\n              37.61369299951804\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"176","noUsgsAuthors":false,"publicationDate":"1990-01-01","publicationStatus":"PW","contributors":{"editors":[{"text":"Wernicke, Brian P.","contributorId":204208,"corporation":false,"usgs":false,"family":"Wernicke","given":"Brian","email":"","middleInitial":"P.","affiliations":[{"id":36877,"text":"Cal Tech","active":true,"usgs":false}],"preferred":false,"id":868708,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Jayko, Angela S. 0000-0002-7378-0330 ajayko@usgs.gov","orcid":"https://orcid.org/0000-0002-7378-0330","contributorId":2531,"corporation":false,"usgs":true,"family":"Jayko","given":"Angela","email":"ajayko@usgs.gov","middleInitial":"S.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":868707,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70241951,"text":"70241951 - 1990 - Chapter 6: Petrogenesis of the composite peraluminous-metaluminous Old Woman-Piute Range batholith, southeastern California; isotopic constraints","interactions":[],"lastModifiedDate":"2023-03-31T19:39:16.48289","indexId":"70241951","displayToPublicDate":"1990-01-01T14:10:18","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Chapter 6: Petrogenesis of the composite peraluminous-metaluminous Old Woman-Piute Range batholith, southeastern California; isotopic constraints","docAbstract":"<p><span>The Late Cretaceous Old Woman–Piute Range batholith includes both metaluminous and strongly peraluminous granitoid series that intruded the reactivated craton of southeastern California shortly after the orogenic peak. Whole-rock Sr, Nd, and O, feldspar Pb, and zircon U-Pb isotopic compositions, in combination with major- and trace-element and petrographic data, indicate that although these series are not comagmatic, they both were generated primarily by anatexis of Proterozoic crust. Differences between the two rock types are functions of source compositions: peraluminous granitoids were apparently generated from an intermediate to felsic source, metaluminous granitoids from more mafic igneous material with a possible modest subcrustal contribution. No sedimentary input is required in production of the peraluminous granites, and in fact, chemically mature sedimentary material is ruled out as an important contributor— that is, these are not S-type granites. Lead-isotope data reveal that the crust that yielded both magma series had undergone an ancient high-grade uranium depletion event, but independent evidence indicates that at the time of anatexis this crust was by no means anhydrous.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The nature and origin of Cordilleran magmatism","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM174-p99","usgsCitation":"Miller, C., Wooden, J., Bennett, V.C., Wright, J.E., Solomon, G.C., and Hurst, R.W., 1990, Chapter 6: Petrogenesis of the composite peraluminous-metaluminous Old Woman-Piute Range batholith, southeastern California; isotopic constraints, chap. <i>of</i> The nature and origin of Cordilleran magmatism, v. 174, p. 99-109, https://doi.org/10.1130/MEM174-p99.","productDescription":"11 p.","startPage":"99","endPage":"109","costCenters":[],"links":[{"id":415031,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Old Woman-Piute Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.84670605744392,\n              34.83154259104336\n            ],\n            [\n              -117.56017104150754,\n              34.253012292806346\n            ],\n            [\n              -116.19981844268885,\n              33.574789543375786\n            ],\n            [\n              -116.02054716997617,\n              32.62958925227802\n            ],\n            [\n              -114.93964684920972,\n              32.69617222554004\n            ],\n            [\n              -114.93437416471762,\n              34.07503768985197\n            ],\n            [\n              -115.18746302031184,\n              34.271341960500024\n            ],\n            [\n              -116.24727260311218,\n              35.50393513284436\n            ],\n            [\n              -117.05399333031863,\n              35.73538800712413\n            ],\n            [\n              -117.93980432489823,\n              36.085570223885995\n            ],\n            [\n              -118.08216680617,\n              35.439523872039075\n            ],\n            [\n              -118.84670605744392,\n              34.83154259104336\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"174","noUsgsAuthors":false,"publicationDate":"1990-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Miller, Calvin F.","contributorId":18437,"corporation":false,"usgs":true,"family":"Miller","given":"Calvin F.","affiliations":[],"preferred":false,"id":868358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wooden, Joseph L.","contributorId":32209,"corporation":false,"usgs":true,"family":"Wooden","given":"Joseph L.","affiliations":[],"preferred":false,"id":868359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, Victoria C.","contributorId":190637,"corporation":false,"usgs":false,"family":"Bennett","given":"Victoria","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":868360,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wright, James E.","contributorId":105648,"corporation":false,"usgs":true,"family":"Wright","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":868361,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Solomon, G. 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,{"id":70242600,"text":"70242600 - 1990 - Consolidation, triaxial shear-strength, and index-property characteristics of organic-rich sediment from the Peru continental margin: Results from Leg 112","interactions":[],"lastModifiedDate":"2023-04-10T19:28:11.406697","indexId":"70242600","displayToPublicDate":"1990-01-01T14:08:32","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":5640,"text":"Proceedings of the Ocean Drilling Program: Scientific Results","onlineIssn":"1096-7451","printIssn":"0884-5891","active":true,"publicationSubtype":{"id":3}},"seriesNumber":"112","chapter":"43","title":"Consolidation, triaxial shear-strength, and index-property characteristics of organic-rich sediment from the Peru continental margin: Results from Leg 112","docAbstract":"<p>Sites 679, 680, and 681 of the Ocean Drilling Program were drilled along an east-west transect across an organic-rich, diatomaceous, coastal upwelling facies that occurs as a shelf/slope lens along the Peru continental margin. Seven 60-cm-long, unsplit core sections from these sites were tested for consolidation, triaxial shear strength, and geotechnical index properties. The testing showed that the sediment has unusually high water content, Atterberg limits, degree of overconsolidation, compressibility, and shear strength. The sediment has unusually low density and grain specific gravity. Atterberg limits, grain specific gravity, compressibility, and apparent excess maximum past stress increase linearly with organic-carbon content, which also correlates positively with diatom content. Overconsolidation measured in these tests is probably not a result of sediment erosion or slumping, but rather the result of diagenesis or interparticle bonding by organic matter. High shear strengths were measured throughout, but particularly high relative shear strengths (as indicated by friction angles and degrees of dilatancy during shear) occur near 20 mbsf. This \"crustlike\" behavior is probably produced by early diagenesis (perhaps including dolotomization) within the upper 20 m, and is complemented by interlocking of diatoms. </p>","language":"English","publisher":"Ocean Drilling Program, Texas A&M University","doi":"10.2973/odp.proc.sr.112.169.1990","usgsCitation":"Lee, H., Kayen, R., and McArthur, W., 1990, Consolidation, triaxial shear-strength, and index-property characteristics of organic-rich sediment from the Peru continental margin: Results from Leg 112: Proceedings of the Ocean Drilling Program: Scientific Results 112, v. 112, 13 p., https://doi.org/10.2973/odp.proc.sr.112.169.1990.","productDescription":"13 p.","startPage":"639","endPage":"651","costCenters":[],"links":[{"id":488786,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/odp.proc.sr.112.169.1990","text":"Publisher Index Page"},{"id":415528,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Peru","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.59128156311986,\n              -12.279014981345938\n            ],\n            [\n              -76.59128156311986,\n              -10.599257249269954\n            ],\n            [\n              -79.54660382874512,\n              -10.599257249269954\n            ],\n            [\n              -79.54660382874512,\n              -12.279014981345938\n            ],\n            [\n              -76.59128156311986,\n              -12.279014981345938\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"112","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lee, Homa J. hjlee@usgs.gov","contributorId":1021,"corporation":false,"usgs":true,"family":"Lee","given":"Homa J.","email":"hjlee@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":869075,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kayen, Robert E. 0000-0002-0356-072X","orcid":"https://orcid.org/0000-0002-0356-072X","contributorId":261195,"corporation":false,"usgs":true,"family":"Kayen","given":"Robert E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":869076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McArthur, William","contributorId":47809,"corporation":false,"usgs":true,"family":"McArthur","given":"William","email":"","affiliations":[],"preferred":false,"id":869077,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70124391,"text":"70124391 - 1990 - Overthrust habitat management plan","interactions":[],"lastModifiedDate":"2014-09-11T14:03:30","indexId":"70124391","displayToPublicDate":"1990-01-01T14:02:34","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"WY-045-WHA-T2","title":"Overthrust habitat management plan","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Bureau of Land Management","publisherLocation":"Washington, D.C.","usgsCitation":"Baker, B., and Luce, B., 1990, Overthrust habitat management plan, 65 p.","productDescription":"65 p.","numberOfPages":"65","costCenters":[],"links":[{"id":293764,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5412b9b5e4b0239f1986baca","contributors":{"authors":[{"text":"Baker, B.W.","contributorId":18707,"corporation":false,"usgs":true,"family":"Baker","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":500771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luce, Bob","contributorId":19733,"corporation":false,"usgs":true,"family":"Luce","given":"Bob","email":"","affiliations":[],"preferred":false,"id":500772,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79,"text":"79 - 1990 - Gloria data, Gulf of Mexico","interactions":[],"lastModifiedDate":"2014-08-04T14:03:11","indexId":"79","displayToPublicDate":"1990-01-01T14:02:03","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Gloria data, Gulf of Mexico","docAbstract":"No abstract available.","language":"English","publisherLocation":"Boulder, CO","doi":"10.3133/79","collaboration":"U.S. Geological Survey, National Oceanic and Atmospheric Administration, National Aeronautics and Space Administration.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, Gloria data, Gulf of Mexico, 1 computer laser optical disk, https://doi.org/10.3133/79.","productDescription":"1 computer laser optical disk","costCenters":[],"links":[{"id":291622,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"Mexico;United States","otherGeospatial":"Gulf Of Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.86,18.18 ], [ -97.86,30.4 ], [ -81.04,30.4 ], [ -81.04,18.18 ], [ -97.86,18.18 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e09e58e4b0beb42bdca430","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70123842,"text":"70123842 - 1990 - The effect of developmental activities on water quality functions of bottomland hardwood ecosystems: the report of the water quality workgroup","interactions":[],"lastModifiedDate":"2014-09-09T14:03:49","indexId":"70123842","displayToPublicDate":"1990-01-01T14:01:03","publicationYear":"1990","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The effect of developmental activities on water quality functions of bottomland hardwood ecosystems: the report of the water quality workgroup","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Ecological processes and cumulative impacts: Illustrated by bottomland hardwood wetland ecosystems","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Lewis Publishers","publisherLocation":"Chelsea, MI","usgsCitation":"Scott, M.L., Kleiss, B., Patrick, W., and Segelquist, C., 1990, The effect of developmental activities on water quality functions of bottomland hardwood ecosystems: the report of the water quality workgroup, chap. <i>of</i> Ecological processes and cumulative impacts: Illustrated by bottomland hardwood wetland ecosystems, p. 411-453.","productDescription":"43 p.","startPage":"411","endPage":"453","numberOfPages":"43","costCenters":[],"links":[{"id":293549,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54101480e4b07ab1cd980b54","contributors":{"authors":[{"text":"Scott, M. L.","contributorId":75090,"corporation":false,"usgs":true,"family":"Scott","given":"M.","middleInitial":"L.","affiliations":[],"preferred":false,"id":500377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kleiss, B.A.","contributorId":107320,"corporation":false,"usgs":false,"family":"Kleiss","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":500379,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patrick, W.H.","contributorId":81029,"corporation":false,"usgs":true,"family":"Patrick","given":"W.H.","affiliations":[],"preferred":false,"id":500378,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Segelquist, C.A.","contributorId":108410,"corporation":false,"usgs":true,"family":"Segelquist","given":"C.A.","affiliations":[],"preferred":false,"id":500380,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":80,"text":"80 - 1990 - GLORIA, East Coast","interactions":[],"lastModifiedDate":"2014-08-04T14:00:15","indexId":"80","displayToPublicDate":"1990-01-01T13:59:45","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"GLORIA, East Coast","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/80","collaboration":"National Aeronautics and Space Administration, U.S.A., U.S. Department of the Interior, Geological Survey, U.S. Department of Commerce, National Oceanic and Atmospheric Administration, NOAA.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, GLORIA, East Coast, 14 data files on 2 computer laser optical disks, https://doi.org/10.3133/80.","productDescription":"14 data files on 2 computer laser optical disks","costCenters":[],"links":[{"id":291621,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e09e4fe4b0beb42bdca3e4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70124389,"text":"70124389 - 1990 - Relationships between whitebark pine cone production and fall grizzly bear movements","interactions":[],"lastModifiedDate":"2014-09-11T14:00:04","indexId":"70124389","displayToPublicDate":"1990-01-01T13:58:59","publicationYear":"1990","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Relationships between whitebark pine cone production and fall grizzly bear movements","docAbstract":"No abstract available.","largerWorkTitle":"Proceedings of a symposium on whitebark pine ecosystems: Ecology and management of a high-mountain resource","conferenceTitle":"Ecology and management of a high-mountain resource","conferenceDate":"1989-03-29T00:00:00","conferenceLocation":"Bozeman, MT","language":"English","publisher":"U.S. Dept. of Agriculture, Forest Service, Intermountain Research Station","publisherLocation":"Ogden, UT","usgsCitation":"Blanchard, B., 1990, Relationships between whitebark pine cone production and fall grizzly bear movements, 1 p.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":293762,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5412b9bbe4b0239f1986baea","contributors":{"authors":[{"text":"Blanchard, B.M.","contributorId":40907,"corporation":false,"usgs":true,"family":"Blanchard","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":500769,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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