{"pageNumber":"4206","pageRowStart":"105125","pageSize":"25","recordCount":184904,"records":[{"id":38390,"text":"pp1505A - 1992 - Geologic framework of pre-Cretaceous rocks in the Southern Ute Indian Reservation and adjacent areas, southwestern Colorado and northwestern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:39","indexId":"pp1505A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1505","chapter":"A","title":"Geologic framework of pre-Cretaceous rocks in the Southern Ute Indian Reservation and adjacent areas, southwestern Colorado and northwestern New Mexico","docAbstract":"This report is a discussion and summary of Jurassic and older rocks in the Southern Ute Indian Reservation and adjacent areas, southwestern Colorado and northwestern New Mexico, and is based on analysis of geophysical logs and observations of outcrops. The Reservation, which is located in the northern San Juan Basin, has been the site of deposition of sediments for much of the Phanerozoic. Geologic times represented on the Reservation are the Precambrian, Cambrian, Devonian, Mississippian, Pennsylvanian, Permian, Triassic, Jurassic, Cretaceous, Tertiary, and Quaternary. Rocks of Ordovician and Silurian age have not been reported in this region. \r\n\r\nThicknesses of pre-Cretaceous sedimentary rocks range from about 750 feet (229 meters) on the Archuleta arch, east of the Reservation, to more than 8,300 feet (2,530 meters) just northwest of the Reservation. About 5,500 feet (1,676 meters) of pre-Cretaceous sedimentary rocks occur in the central part of the Reservation, near Ignacio. At Ignacio the top of the Jurassic lies at a depth of 7,600 feet (2,316 meters) below the surface, which is composed of Tertiary rocks. As much as 2,500 feet (762 meters) of Tertiary rocks occur in the area. More than 10,000 feet (3,048 meters) of Cretaceous and younger rocks, and 15,600 feet (4,755 meters) of all Phanerozoic sedimentary rocks occur in the vicinity of the Reservation. \r\n\r\nIn the early Paleozoic the area that includes the Southern Ute Reservation was on the stable western shelf of the craton. During this time sediments that compose the following shallow-marine clastic and carbonate rocks were deposited: the Upper Cambrian Ignacio Quartzite (0-150 feet; 0-46 meters), Upper Devonian Elbert Formation (50-200 feet; 15-61 meters), Upper Devonian Ouray Limestone (10-75 feet; 3-23 meters), and Mississippian Leadville Limestone (0-250 feet; 0-76 meters). \r\n\r\nMixed carbonate and clastic deposition, which was punctuated by a unique episode of deposition of evaporite sediments, continued through the Pennsylvanian after a significant episode of erosion at the end of the Mississippian. Pennsylvanian rocks on the Reservation are the Molas Formation (20-100 feet; 6-30 meters) and Hermosa Group (400-2,800 feet; 122-853 meters), which consists of the Pinkerton Trail Formation (40-120 feet; 12-36 meters), Paradox Formation and equivalent rocks (200-1,800 feet; 61-549 meters), and Honaker Trail Formation (200-1,300 feet; 61-396 meters). A unit that is transitional between the Pennsylvanian and Permian is the Rico Formation, which is about 200 feet (61 meters) thick across most of the Reservation area. \r\n\r\nThe close of the Paleozoic Era was marked by a great influx of arkosic clastic sediments from uplifted highlands to the north of the Reservation area during the Permian. Near the paleomountain front the Cutler Formation (presently as thick as 8,000 feet; 2,438 meters) formed as a result of deposition of arkosic sediments; however, the original thickness of the Cutler is unknown due to an unconformity at its top. In the area of the Reservation the Cutler has group status and has been divided into several formations: the Halgaito Formation (350-800 feet; 107-244 meters), Cedar Mesa Sandstone and equivalent rocks (150-350 feet; 46-107 meters), Organ Rock Formation (500-900 feet; 152-274 meters), and De Chelly Sandstone (0-100 feet; 0-30 meters). The sediments of these formations were deposited in a variety of environments, including eolian, mud-flat, and fluvial systems. \r\n\r\nFollowing an episode of erosion in the Early and Middle(?) Triassic, deposition in the area of the Southern Ute Reservation continued during the Mesozoic. Sediments of the Upper Triassic Dolores and correlative Chinle Formations were deposited in fluvial, lacustrine, and minor eolian environments. On the Reservation the Dolores is 500-1,200 feet (152-366 meters) thick. Lower Jurassic eolian and fluvial deposits may have been present in much of the Reservation area but have been removed ","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and mineral resources of the Southern Ute Indian Reservation","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp1505A","usgsCitation":"Condon, S.M., 1992, Geologic framework of pre-Cretaceous rocks in the Southern Ute Indian Reservation and adjacent areas, southwestern Colorado and northwestern New Mexico: U.S. Geological Survey Professional Paper 1505, p. A1-A56, 1 plate in pocket, https://doi.org/10.3133/pp1505A.","productDescription":"p. A1-A56, 1 plate in pocket","costCenters":[],"links":[{"id":119812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1505a/report-thumb.jpg"},{"id":64740,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1505a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64741,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1505a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a56a9","contributors":{"authors":[{"text":"Condon, Steven M.","contributorId":95464,"corporation":false,"usgs":true,"family":"Condon","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":219734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":77047,"text":"pp1551 - 1992 - The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","interactions":[{"subject":{"id":38252,"text":"pp1551B - 1998 - The Loma Prieta, California, earthquake of October 17, 1989: Liquefaction","indexId":"pp1551B","publicationYear":"1998","noYear":false,"chapter":"B","title":"The Loma Prieta, California, earthquake of October 17, 1989: Liquefaction"},"predicate":"IS_PART_OF","object":{"id":77047,"text":"pp1551 - 1992 - The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","indexId":"pp1551","publicationYear":"1992","noYear":false,"title":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure"},"id":1},{"subject":{"id":38342,"text":"pp1551A - 1994 - The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion","indexId":"pp1551A","publicationYear":"1994","noYear":false,"chapter":"A","title":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion"},"predicate":"IS_PART_OF","object":{"id":77047,"text":"pp1551 - 1992 - The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","indexId":"pp1551","publicationYear":"1992","noYear":false,"title":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure"},"id":2},{"subject":{"id":38343,"text":"pp1551E - 1994 - The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances","indexId":"pp1551E","publicationYear":"1994","noYear":false,"chapter":"E","title":"The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances"},"predicate":"IS_PART_OF","object":{"id":77047,"text":"pp1551 - 1992 - The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","indexId":"pp1551","publicationYear":"1992","noYear":false,"title":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure"},"id":3}],"lastModifiedDate":"2019-07-18T13:37:59","indexId":"pp1551","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1551","title":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","docAbstract":"Professional Paper 1551 describes the effects at the land surface caused by the Loma Prieta earthquake. These effects: include the pattern and characteristics of strong ground shaking, liquefaction of both floodplain deposits along the Pajaro and Salinas Rivers in the Monterey Bay region and sandy artificial fills along the margins of San Francisco Bay, landslides in the epicentral region, and increased stream flow. Some significant findings and their impacts were: \r\n\r\n* Strong shaking that was amplified by a factor of about two by soft soils caused damage at up to 100 kilometers (60 miles) from the epicenter. \r\n\r\n* Instrumental recordings of the ground shaking have been used to improve how building codes consider site amplification effects from soft soils. \r\n\r\n* Liquefaction at 134 locations caused $99.2 million of the total earthquake loss of $5.9 billion. Liquefaction of floodplain deposits and sandy artificial fills was similar in nature to that which occurred in the 1906 San Francisco earthquake and indicated that many areas remain susceptible to liquefaction damage in the San Francisco and Monterey Bay regions. \r\n\r\n* Landslides caused $30 million in earthquake losses, damaging at least 200 residences. Many landslides showed evidence of movement in previous earthquakes. \r\n\r\n* Recognition of the similarities between liquefaction and landslides in 1906 and 1989 and research in intervening years that established methodologies to map liquefaction and landslide hazards prompted the California legislature to pass in 1990 the Seismic Hazards Mapping Act that required the California Geological Survey to delineate regulatory zones of areas potentially susceptible to these hazards. \r\n\r\n* The earthquake caused the flow of many streams in the epicentral region to increase. Effects were noted up to 88 km from the epicenter. \r\n\r\n* Post-earthquake studies of the Marina District of San Francisco provide perhaps the most comprehensive case history of earthquake effects at a specific site developed for any earthquake. Soft soils beneath the Marina amplified ground shaking to damaging levels and caused liquefaction of sandy artificial fills. Liquefaction required 123 repairs of pipelines in the Municipal Water Supply System, more than three times the number of repairs elsewhere in the system. Approximately 13.6 km of gas-distribution lines were replaced, and more than 20% of the wastewater collection lines were repaired or replaced. \r\n","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1551","collaboration":"Chapter D will not be published\r\nPrepared in cooperation with the National Science Foundation","usgsCitation":"Coordinated by Holzer, T.L., 1992, The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure: U.S. Geological Survey Professional Paper 1551, https://doi.org/10.3133/pp1551.","additionalOnlineFiles":"Y","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":194795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8210,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/pp1551/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881d5","contributors":{"authors":[{"text":"Coordinated by Holzer, Thomas L.","contributorId":16517,"corporation":false,"usgs":true,"family":"Coordinated by Holzer","given":"Thomas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":288405,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47567,"text":"b1787GG - 1992 - Stratigraphic correlations between the Eagle Valley Evaporite and Minturn Formation, Eagle Basin, Northwest Colorado","interactions":[{"subject":{"id":47567,"text":"b1787GG - 1992 - Stratigraphic correlations between the Eagle Valley Evaporite and Minturn Formation, Eagle Basin, Northwest Colorado","indexId":"b1787GG","publicationYear":"1992","noYear":false,"chapter":"GG","title":"Stratigraphic correlations between the Eagle Valley Evaporite and Minturn Formation, Eagle Basin, Northwest Colorado"},"predicate":"IS_PART_OF","object":{"id":33224,"text":"b1787 - 1987 - Evolution of sedimentary basins: Uinta and Piceance Basins","indexId":"b1787","publicationYear":"1987","noYear":false,"title":"Evolution of sedimentary basins: Uinta and Piceance Basins"},"id":1}],"isPartOf":{"id":33224,"text":"b1787 - 1987 - Evolution of sedimentary basins: Uinta and Piceance Basins","indexId":"b1787","publicationYear":"1987","noYear":false,"title":"Evolution of sedimentary basins: Uinta and Piceance Basins"},"lastModifiedDate":"2017-08-09T09:32:32","indexId":"b1787GG","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"1787","chapter":"GG","title":"Stratigraphic correlations between the Eagle Valley Evaporite and Minturn Formation, Eagle Basin, Northwest Colorado","language":"ENGLISH","doi":"10.3133/b1787GG","usgsCitation":"Schenk, C.J., 1992, Stratigraphic correlations between the Eagle Valley Evaporite and Minturn Formation, Eagle Basin, Northwest Colorado: U.S. Geological Survey Bulletin 1787, p. GG1-GG8, sect., strat. cols., geol. sketch map, https://doi.org/10.3133/b1787GG.","productDescription":"p. GG1-GG8, sect., strat. cols., geol. sketch map","costCenters":[],"links":[{"id":169401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1787gg/report-thumb.jpg"},{"id":84502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1787gg/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b09de","contributors":{"authors":[{"text":"Schenk, Christopher J. 0000-0002-0248-7305 schenk@usgs.gov","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":826,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"schenk@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":235742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28126,"text":"wri914028 - 1992 - Development and routing of mudflow resulting from hypothetical failure of Spirit Lake debris dam, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri914028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4028","title":"Development and routing of mudflow resulting from hypothetical failure of Spirit Lake debris dam, Washington","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914028","usgsCitation":"Kresch, D., 1992, Development and routing of mudflow resulting from hypothetical failure of Spirit Lake debris dam, Washington: U.S. Geological Survey Water-Resources Investigations Report 91-4028, v, 30 p. :ill., maps ;28 cm. [PGS - 29 p.], https://doi.org/10.3133/wri914028.","productDescription":"v, 30 p. :ill., maps ;28 cm. [PGS - 29 p.]","costCenters":[],"links":[{"id":121579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4028/report-thumb.jpg"},{"id":56959,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66724b","contributors":{"authors":[{"text":"Kresch, D. L.","contributorId":52559,"corporation":false,"usgs":true,"family":"Kresch","given":"D. L.","affiliations":[],"preferred":false,"id":199263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20876,"text":"ofr92162 - 1992 - Integrating quality assurance in project work plans of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr92162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-162","title":"Integrating quality assurance in project work plans of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey's objectives for including quality assurance procedures in a project work plan are to ensure that the quality of the data collected is defined and is appropriate for the objectives of the investigation. The data- quality information can be used in the interpre- tation of the data. A project work plan that includes quality assessment provides definable benefits such as clarity of expectations, a method for obtaining a set of data that is expected and has been proven valid, a documentation trail, products that are produced on time and that meet project objectives, and a decrease in work that is lost or redone. Project chiefs must prepare and can publish the work plan for scientific investigations. An expanded outline of a framework that can be used to prepare a project work plan that includes quality assurance is described in this report and contains the following topics: data-quality objectives; project organization and responsibilities; data collection; data processing; project reviews; data analysis; remedial actions; project progress reports and quality assurance reports to management.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr92162","usgsCitation":"Shampine, W., Pope, L.M., and Koterba, M., 1992, Integrating quality assurance in project work plans of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 92-162, iii, 12 p. :ill. ;28 cm., https://doi.org/10.3133/ofr92162.","productDescription":"iii, 12 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0162/report-thumb.jpg"},{"id":50471,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0162/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0eb1","contributors":{"authors":[{"text":"Shampine, W. J.","contributorId":16023,"corporation":false,"usgs":true,"family":"Shampine","given":"W. J.","affiliations":[],"preferred":false,"id":183420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pope, L. M.","contributorId":71939,"corporation":false,"usgs":true,"family":"Pope","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":183422,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koterba, M.T.","contributorId":62570,"corporation":false,"usgs":true,"family":"Koterba","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":183421,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20814,"text":"ofr92136 - 1992 - Guidelines for preparing a quality assurance plan for district offices of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:36","indexId":"ofr92136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-136","title":"Guidelines for preparing a quality assurance plan for district offices of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey has a policy that requires each District office to prepare a Quality Assurance Plan. This plan is a combination of a District's management principles and quality assurance processes. The guidelines presented in this report provide a framework or expanded outline that a District can use to prepare a plan. Parti- cular emphasis is given to a District's: (1) quality assurance policies; (2) organization and staff responsibilities; and (3) program and project planning. The guidelines address the 'how', 'what', and 'who' questions that need to be answered when a District Quality Assurance Plan is prepared.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr92136","usgsCitation":"Schroder, L., and Shampine, W., 1992, Guidelines for preparing a quality assurance plan for district offices of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 92-136, iii, 14 p. :ill. ;28 cm., https://doi.org/10.3133/ofr92136.","productDescription":"iii, 14 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0136/report-thumb.jpg"},{"id":50365,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0136/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a2e0","contributors":{"authors":[{"text":"Schroder, L.J.","contributorId":31767,"corporation":false,"usgs":true,"family":"Schroder","given":"L.J.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":183298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shampine, W. J.","contributorId":16023,"corporation":false,"usgs":true,"family":"Shampine","given":"W. J.","affiliations":[],"preferred":false,"id":183297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":20691,"text":"ofr92364A - 1992 - XDETECT version 2.01 technical reference","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr92364A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-364","chapter":"A","title":"XDETECT version 2.01 technical reference","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr92364A","usgsCitation":"Rogers, J.A., and Kohler, W., 1992, XDETECT version 2.01 technical reference (Version 2.01 [June 1991].): U.S. Geological Survey Open-File Report 92-364, 2 computer disks ;5 1/4 in. +1 text (12 p., 13 p. of plates : ill. ; 28 cm.), https://doi.org/10.3133/ofr92364A.","productDescription":"2 computer disks ;5 1/4 in. +1 text (12 p., 13 p. of plates : ill. ; 28 cm.)","costCenters":[],"links":[{"id":154054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0364a/report-thumb.jpg"},{"id":50252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0364a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 2.01 [June 1991].","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de5c3","contributors":{"authors":[{"text":"Rogers, John A.","contributorId":82704,"corporation":false,"usgs":true,"family":"Rogers","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":183076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kohler, W.M.","contributorId":62999,"corporation":false,"usgs":true,"family":"Kohler","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":183075,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":20671,"text":"ofr92448 - 1992 - Inventory of metal mines and occurrence associated with the early Mesozoic basins of the Eastern United States; II, occurrence descriptions and summary tables","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr92448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-448","title":"Inventory of metal mines and occurrence associated with the early Mesozoic basins of the Eastern United States; II, occurrence descriptions and summary tables","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr92448","usgsCitation":"Robinson, and Sears, C., 1992, Inventory of metal mines and occurrence associated with the early Mesozoic basins of the Eastern United States; II, occurrence descriptions and summary tables: U.S. Geological Survey Open-File Report 92-448, 190 p.  ;28 cm., https://doi.org/10.3133/ofr92448.","productDescription":"190 p.  ;28 cm.","costCenters":[],"links":[{"id":153129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0448/report-thumb.jpg"},{"id":50195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c6e4b07f02db540002","contributors":{"authors":[{"text":"Robinson, Jr. 0000-0002-9676-9564","orcid":"https://orcid.org/0000-0002-9676-9564","contributorId":8479,"corporation":false,"usgs":true,"family":"Robinson","suffix":"Jr.","email":"","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":5068,"text":"Midwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":183040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sears, C.M.","contributorId":36944,"corporation":false,"usgs":true,"family":"Sears","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":183041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20930,"text":"ofr92129 - 1992 - Hydro-climatic data network (HCDN); a U.S. Geological Survey streamflow data set for the United States for the study of climate variations, 1874-1988","interactions":[],"lastModifiedDate":"2016-07-27T12:53:30","indexId":"ofr92129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-129","title":"Hydro-climatic data network (HCDN); a U.S. Geological Survey streamflow data set for the United States for the study of climate variations, 1874-1988","docAbstract":"<p>Records of streamflow can provide an account of climatic variation over a hydrologic basin. The ability to do so is conditioned on the absence of confounding factors that diminish the climate signal. A national data set of streamflow records that are relatively free of confounding anthropogenic influences has been developed for the purpose of studying the variation in surface-water conditions throughout the United States. Records in the U.S. Geological Survey (USGS) National Water Storage and Retrieval System (WATSTORE) data base for active and discontinued streamflow gaging stations through water year 1988 (that is, through September 30, 1988) were reviewed jointly with data specialists in each USGS District office. The resulting collection of stations, each with its respective period of record satisfying the qualifying criteria, is called the Hydro-Climatic Data Network, or HCDN. The HCDN consists of 1,659 sites throughout the United States and its territories, totaling 73,231 water years of daily mean discharge values. For each station in the HCDN, information necessary for its identification, along with any qualifying comments about the available record and a set of descriptive watershed characteristics are provided in tabular format in this report, both on paper and on computer disk (enclosed). For each station in the HCDN, the appropriate daily mean discharge values were compiled, and statistical characteristics, including monthly mean discharges and annual mean, minimum and maximum discharges, were derived. The discharge data values are provided in a companion report.</p>","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of this report can be purchased from USGS Books and Open-File Reports Section,","doi":"10.3133/ofr92129","usgsCitation":"Slack, J.R., and Landwehr, J., 1992, Hydro-climatic data network (HCDN); a U.S. Geological Survey streamflow data set for the United States for the study of climate variations, 1874-1988: U.S. Geological Survey Open-File Report 92-129, vii, 193 p. :ill., maps ;28 cm. +1 computer disk (5 1/4 in.), https://doi.org/10.3133/ofr92129.","productDescription":"vii, 193 p. :ill., maps ;28 cm. +1 computer disk (5 1/4 in.)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"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":50522,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1246,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr92-129","linkFileType":{"id":5,"text":"html"}},{"id":154083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0129/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db62966d","contributors":{"authors":[{"text":"Slack, J. R.","contributorId":40205,"corporation":false,"usgs":true,"family":"Slack","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landwehr, Jurate Maciunas","contributorId":106522,"corporation":false,"usgs":true,"family":"Landwehr","given":"Jurate Maciunas","affiliations":[],"preferred":false,"id":183525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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