Test well data that may be used to determine the hydrogeology of the zone of high permeability in Palm Beach County, Florida are presented. Lithologic logs from 46 test wells and geophysical logs from 40 test wells are contained in this report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8168","collaboration":"Prepared in cooperation with Palm Beach County and the South Florida Water Management District","usgsCitation":"Swayze, L.J., McGovern, M.C., and Fischer, J.N., 1980, Lithologic logs and geophysical logs from test drilling in Palm Beach County, Florida, since 1974: U.S. Geological Survey Open-File Report 81-68, iii, 93 p., https://doi.org/10.3133/ofr8168.","productDescription":"iii, 93 p.","costCenters":[],"links":[{"id":143067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0068/report-thumb.jpg"},{"id":350355,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Palm Beach County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bb78","contributors":{"authors":[{"text":"Swayze, Leo J.","contributorId":55437,"corporation":false,"usgs":true,"family":"Swayze","given":"Leo","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":163054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGovern, Michael C.","contributorId":88738,"corporation":false,"usgs":true,"family":"McGovern","given":"Michael","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":163055,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fischer, John N.","contributorId":19939,"corporation":false,"usgs":true,"family":"Fischer","given":"John","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":163053,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11393,"text":"ofr81293 - 1980 - Dry tilt and nearfield geodetic investigations of crustal movements, Southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr81293","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-293","title":"Dry tilt and nearfield geodetic investigations of crustal movements, Southern California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81293","usgsCitation":"Sylvester, A.G., 1980, Dry tilt and nearfield geodetic investigations of crustal movements, Southern California: U.S. Geological Survey Open-File Report 81-293, 17 leaves :ill., maps ;28 cm.; (95 p. - PGS), https://doi.org/10.3133/ofr81293.","productDescription":"17 leaves :ill., maps ;28 cm.; (95 p. - PGS)","costCenters":[],"links":[{"id":142567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0293/report-thumb.jpg"},{"id":39217,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0293/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633cc1","contributors":{"authors":[{"text":"Sylvester, Arthur G.","contributorId":23953,"corporation":false,"usgs":true,"family":"Sylvester","given":"Arthur","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":163061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6230,"text":"pp1145 - 1980 - Paleozoic and Mesozoic deformations in the central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1145","title":"Paleozoic and Mesozoic deformations in the central Sierra Nevada, California","docAbstract":"Analysis of structural and stratigraphic data indicates that several periods of regional deformation, consisting of combined folding, faulting, cataclasis, and regional metamorphism, occurred throughout the central Sierra Nevada during Paleozoic and Mesozoic time. The oldest regional deformation occurred alono northward trends during the Devonian and Mississippian periods in most roof pendants containing lower Paleozoic metasedimentary rocks at the center and along the crest of the range. This deformation is expressed in some roof pendants by an angular unconformity separating older thrice-deformed from younger twice-deformed Paleozoic metasedimentary rocks. \r\n\r\nThe first Mesozoic deformation, which consisted of uplift and erosion and was accompanied by the onset of Andean-type volcanism during the Permian and Triassic, is expressed by an angular unconformity in several roof pendants from the Saddlebag Lake to the Mount Morrison areas. This unconformity is defined by Permian and Triassic andesitic to rhyolitic metavolcanic rocks unconformably overlying more intensely deformed Pennsylvanian, Permian(?), and older metasedimentary rocks. A later regional deformation occurred during the Triassic along N. 20?_30? W. trends in Permian and Triassic metavolcanic rocks of the Saddlebag Lake and Mount Dana roof pendants, in upper Paleozoic rocks of the Pine Creek roof pendant, and in the Calaveras Formation of the western metamorphic belt; the roof pendants are crosscut by Upper Triassic granitic rocks of the Lee Vining intrusive epoch. A still later period of Early and Middle Jurassic regional deformation occurred along N. 30?-60? E. trends in upper Paleozoic rocks of the Calaveras Formation of the western metamorphic belt. A further period of deformation was the Late Jurassic Nevadan orogeny, which occurred along N. 20?_40? W. trends in Upper Jurassic rocks of the western metamorphic belt that are crosscut by Upper Jurassic granitic rocks of the Yosemite intrusive epoch. Structures of similar age occur in intensely deformed oceanic-lithospheric and syntectonic plutonic rocks of the lower Kings River area, in Jurassic metavolcanic rocks of the Ritter Range roof pendant, and in Triassic metasedimentary rocks of the Mineral King roof pendant. The final Mesozoic deformation occurred along N. 50?-80? W. trends in both high-country roof pendants and the lower Kings River area; structures of this generation are crosscut by relatively undeformed Upper Cretaceous granitic rocks of the Cathedral Range intrusive epoch.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1145","usgsCitation":"Nokleberg, W.J., and Kistler, R.W., 1980, Paleozoic and Mesozoic deformations in the central Sierra Nevada, California: U.S. Geological Survey Professional Paper 1145, 24 p., https://doi.org/10.3133/pp1145.","productDescription":"24 p.","costCenters":[],"links":[{"id":124949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1145/report-thumb.jpg"},{"id":33435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688604","contributors":{"authors":[{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":152346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kistler, Ronald Wayne","contributorId":27857,"corporation":false,"usgs":true,"family":"Kistler","given":"Ronald","email":"","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":152347,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66919,"text":"i1174 - 1980 - Geologic map of the Talkeetna Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"i1174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1174","subseriesTitle":"NONE","title":"Geologic map of the Talkeetna Quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/i1174","usgsCitation":"Reed, B., and Nelson, S., 1980, Geologic map of the Talkeetna Quadrangle, Alaska: U.S. Geological Survey IMAP 1174, 1 map : col. ;45 x 63 cm. on sheet 106 x 73 cm., https://doi.org/10.3133/i1174.","productDescription":"1 map : col. ;45 x 63 cm. on sheet 106 x 73 cm.","costCenters":[],"links":[{"id":108192,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12246.htm","linkFileType":{"id":5,"text":"html"},"description":"12246"},{"id":189192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -153,62 ], [ -153,63 ], [ -150,63 ], [ -150,62 ], [ -153,62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a614","contributors":{"authors":[{"text":"Reed, B.L.","contributorId":29434,"corporation":false,"usgs":true,"family":"Reed","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":275287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, S.W.","contributorId":67869,"corporation":false,"usgs":true,"family":"Nelson","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":275288,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6496,"text":"pp1070 - 1980 - Foraminifera from the Kara and Greenland seas, and review of Arctic studies","interactions":[],"lastModifiedDate":"2019-12-03T07:35:13","indexId":"pp1070","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1070","title":"Foraminifera from the Kara and Greenland seas, and review of Arctic studies","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Government Print Office","doi":"10.3133/pp1070","usgsCitation":"Todd, R., and Low, D., 1980, Foraminifera from the Kara and Greenland seas, and review of Arctic studies: U.S. Geological Survey Professional Paper 1070, v. 1070, 30 p., https://doi.org/10.3133/pp1070.","productDescription":"30 p.","costCenters":[],"links":[{"id":33953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1070/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1070/report-thumb.jpg"}],"country":"Greenland, Russia","otherGeospatial":"Greenland Sea, Kara Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 91.318359375,\n 79.981890541616\n ],\n [\n 68.73046875,\n 76.434603583513\n ],\n [\n 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Ruth","contributorId":81091,"corporation":false,"usgs":true,"family":"Todd","given":"Ruth","email":"","affiliations":[],"preferred":false,"id":152824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Low, Doris","contributorId":108102,"corporation":false,"usgs":true,"family":"Low","given":"Doris","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":152825,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3645,"text":"cir826 - 1980 - A review and evaluation of alternatives for updating U.S. Geological Survey land use and land cover maps","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir826","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"826","title":"A review and evaluation of alternatives for updating U.S. Geological Survey land use and land cover maps","docAbstract":"Since 1974, the U.S. Geological Survey has been engaged in a nationwide program of baseline mapping of land use and land cover and associated data at a scale of 1:250,000. As l:100,000-scale bases have become available, they have been used for mapping certain areas and for special applications. These two scales are appropriate for mapping land use and land cover data on a nationwide basis within a practical time frame, and with an acceptable degree of standardization, accuracy, and level of detail. An essential requisite to better use of the land is current information on land use and land cover conditions and on the rates and trends of changes with time. Thus, plans are underway to update these maps and data. The major considerations in planning a nationwide program for updating U.S. Geological Survey land use and land cover maps are as follows: (1) How often should maps be updated? (2) What remotely sensed source materials should be used for detecting and compiling changes in land use and land cover? (3) What base maps should be used for presenting data on land use and land cover changes? (4) What maps or portions of a map should be updated? (5) What methods should be used for identifying and mapping changes? (6) What procedures should be followed for updating maps and what formats should be used? These factors must be considered in developing a map update program that portrays an appropriate level of information, relates to and builds upon the existing U.S. Geological Survey land use and land cover digital and statistical data base, is timely, cost-effective and standardized, and meets the varying needs of land use and land cover data users.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir826","usgsCitation":"Milazzo, V.A., 1980, A review and evaluation of alternatives for updating U.S. Geological Survey land use and land cover maps: U.S. Geological Survey Circular 826, 19 p. : ill., maps ; 26 cm., https://doi.org/10.3133/cir826.","productDescription":"19 p. : ill., maps ; 26 cm.","costCenters":[],"links":[{"id":124600,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0826/report-thumb.jpg"},{"id":30687,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0826/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a813f","contributors":{"authors":[{"text":"Milazzo, Valerie A.","contributorId":88717,"corporation":false,"usgs":true,"family":"Milazzo","given":"Valerie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8113,"text":"ofr801290 - 1980 - Selected administrative, land, and resource data for Known Geothermal Resources Areas in Arizona, California, Idaho, Nevada, Oregon, and Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr801290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1290","title":"Selected administrative, land, and resource data for Known Geothermal Resources Areas in Arizona, California, Idaho, Nevada, Oregon, and Washington","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801290","usgsCitation":"Burkhardt, H., Brook, C., and Smith, F., 1980, Selected administrative, land, and resource data for Known Geothermal Resources Areas in Arizona, California, Idaho, Nevada, Oregon, and Washington: U.S. Geological Survey Open-File Report 80-1290, i, 29 p. ;28 cm., https://doi.org/10.3133/ofr801290.","productDescription":"i, 29 p. ;28 cm.","costCenters":[],"links":[{"id":140629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1290/report-thumb.jpg"},{"id":35718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1290/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa787","contributors":{"authors":[{"text":"Burkhardt, H.E.","contributorId":69974,"corporation":false,"usgs":true,"family":"Burkhardt","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":157170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brook, C.A.","contributorId":82699,"corporation":false,"usgs":true,"family":"Brook","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":157171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, F.W.","contributorId":27445,"corporation":false,"usgs":true,"family":"Smith","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":157169,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7371,"text":"ofr802010 - 1980 - Overconsolidated surficial sediment on the Beaufort Sea shelf","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr802010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-2010","title":"Overconsolidated surficial sediment on the Beaufort Sea shelf","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr802010","usgsCitation":"Reimnitz, E., Kempema, E., Ross, R., and Minkler, P., 1980, Overconsolidated surficial sediment on the Beaufort Sea shelf: U.S. Geological Survey Open-File Report 80-2010, 37 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr802010.","productDescription":"37 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2010/report-thumb.jpg"},{"id":34770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a30b","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":155442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kempema, Edward","contributorId":49353,"corporation":false,"usgs":true,"family":"Kempema","given":"Edward","email":"","affiliations":[],"preferred":false,"id":155444,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, Robin","contributorId":36547,"corporation":false,"usgs":true,"family":"Ross","given":"Robin","email":"","affiliations":[],"preferred":false,"id":155443,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minkler, Peter","contributorId":8846,"corporation":false,"usgs":true,"family":"Minkler","given":"Peter","email":"","affiliations":[],"preferred":false,"id":155441,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7370,"text":"ofr801226 - 1980 - Overburden geochemistry of the U.S. Bureau of Land Management experimental coal mining reclamation site at Ojo Encino, Northeast McKinley County, San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr801226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1226","title":"Overburden geochemistry of the U.S. Bureau of Land Management experimental coal mining reclamation site at Ojo Encino, Northeast McKinley County, San Juan Basin, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801226","usgsCitation":"Hinkley, T.K., Herring, J., Smith, K., and Boerngen, J., 1980, Overburden geochemistry of the U.S. Bureau of Land Management experimental coal mining reclamation site at Ojo Encino, Northeast McKinley County, San Juan Basin, New Mexico: U.S. Geological Survey Open-File Report 80-1226, 21 p. ;28 cm., https://doi.org/10.3133/ofr801226.","productDescription":"21 p. ;28 cm.","costCenters":[],"links":[{"id":140387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1226/report-thumb.jpg"},{"id":112896,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1226/report.pdf","size":"701","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a3f0","contributors":{"authors":[{"text":"Hinkley, Todd K. 0000-0001-8507-6271 thinkley@usgs.gov","orcid":"https://orcid.org/0000-0001-8507-6271","contributorId":1497,"corporation":false,"usgs":true,"family":"Hinkley","given":"Todd","email":"thinkley@usgs.gov","middleInitial":"K.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":155437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herring, J. R.","contributorId":43348,"corporation":false,"usgs":true,"family":"Herring","given":"J. R.","affiliations":[],"preferred":false,"id":155439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, K. S. 0000-0001-8547-9804","orcid":"https://orcid.org/0000-0001-8547-9804","contributorId":47779,"corporation":false,"usgs":true,"family":"Smith","given":"K. S.","affiliations":[],"preferred":false,"id":155440,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boerngen, J.G.","contributorId":28974,"corporation":false,"usgs":true,"family":"Boerngen","given":"J.G.","affiliations":[],"preferred":false,"id":155438,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":4831,"text":"pp1138AC - 1980 - Petroleum-resource appraisal and discovery rate forecasting in partially explored regions","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"pp1138AC","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1138","chapter":"A-C","title":"Petroleum-resource appraisal and discovery rate forecasting in partially explored regions","docAbstract":"PART A: A model of the discovery process can be used to predict the size distribution of future petroleum discoveries in partially explored basins. The parameters of the model are estimated directly from the historical drilling record, rather than being determined by assumptions or analogies. The model is based on the concept of the area of influence of a drill hole, which states that the area of a basin exhausted by a drill hole varies with the size and shape of targets in the basin and with the density of previously drilled wells. It also uses the concept of discovery efficiency, which measures the rate of discovery within several classes of deposit size. The model was tested using 25 years of historical exploration data (1949-74) from the Denver basin. From the trend in the discovery rate (the number of discoveries per unit area exhausted), the discovery efficiencies in each class of deposit size were estimated. Using pre-1956 discovery and drilling data, the model accurately predicted the size distribution of discoveries for the 1956-74 period. \r\n\r\nPART B: A stochastic model of the discovery process has been developed to predict, using past drilling and discovery data, the distribution of future petroleum deposits in partially explored basins, and the basic mathematical properties of the model have been established. The model has two exogenous parameters, the efficiency of exploration and the effective basin size. The first parameter is the ratio of the probability that an actual exploratory well will make a discovery to the probability that a randomly sited well will make a discovery. The second parameter, the effective basin size, is the area of that part of the basin in which drillers are willing to site wells. Methods for estimating these parameters from locations of past wells and from the sizes and locations of past discoveries were derived, and the properties of estimators of the parameters were studied by simulation. \r\n\r\nPART C: This study examines the temporal properties and determinants of petroleum exploration for firms operating in the Denver basin. Expectations associated with the favorability of a specific area are modeled by using distributed lag proxy variables (of previous discoveries) and predictions from a discovery process model. In the second part of the study, a discovery process model is linked with a behavioral well-drilling model in order to predict the supply of new reserves. \r\n\r\nResults of the study indicate that the positive effects of new discoveries on drilling increase for several periods and then diminish to zero within 2? years after the deposit discovery date. Tests of alternative specifications of the argument of the distributed lag function using alternative minimum size classes of deposits produced little change in the model's explanatory power. This result suggests that, once an exploration play is underway, favorable operator expectations are sustained by the quantity of oil found per time period rather than by the discovery of specific size deposits. When predictions of the value of undiscovered deposits (generated from a discovery process model) were substituted for the expectations variable in models used to explain exploration effort, operator behavior was found to be consistent with these predictions. This result suggests that operators, on the average, were efficiently using information contained in the discovery history of the basin in carrying out their exploration plans. Comparison of the two approaches to modeling unobservable operator expectations indicates that the two models produced very similar results. The integration of the behavioral well-drilling model and discovery process model to predict the additions to reserves per unit time was successful only when the quarterly predictions were aggregated to annual values. The accuracy of the aggregated predictions was also found to be reasonably robust to errors in predictions from the behavioral well-drilling equation.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1138AC","usgsCitation":"Drew, L.J., Schuenemeyer, J., Root, D.H., and Attanasi, E.D., 1980, Petroleum-resource appraisal and discovery rate forecasting in partially explored regions: U.S. Geological Survey Professional Paper 1138, NA, https://doi.org/10.3133/pp1138AC.","productDescription":"NA","costCenters":[],"links":[{"id":117418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1138a-c/report-thumb.jpg"},{"id":31771,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1138a-c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686c60","contributors":{"authors":[{"text":"Drew, Lawrence J. ldrew@usgs.gov","contributorId":2635,"corporation":false,"usgs":true,"family":"Drew","given":"Lawrence","email":"ldrew@usgs.gov","middleInitial":"J.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":149864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuenemeyer, J.H.","contributorId":106094,"corporation":false,"usgs":true,"family":"Schuenemeyer","given":"J.H.","affiliations":[],"preferred":false,"id":149866,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Root, David H.","contributorId":92232,"corporation":false,"usgs":true,"family":"Root","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":149865,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Attanasi, E. D. 0000-0001-6845-7160","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":107672,"corporation":false,"usgs":true,"family":"Attanasi","given":"E.","middleInitial":"D.","affiliations":[],"preferred":false,"id":149867,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":9362,"text":"ofr801274 - 1980 - RASO; program for renumbering Fortran source programs","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr801274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1274","title":"RASO; program for renumbering Fortran source programs","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801274","usgsCitation":"Harrach, G.H., 1980, RASO; program for renumbering Fortran source programs: U.S. Geological Survey Open-File Report 80-1274, i, 62 p. ;28 cm., https://doi.org/10.3133/ofr801274.","productDescription":"i, 62 p. ;28 cm.","costCenters":[],"links":[{"id":140859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1274/report-thumb.jpg"},{"id":37073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1274/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fc2","contributors":{"authors":[{"text":"Harrach, George H.","contributorId":39371,"corporation":false,"usgs":true,"family":"Harrach","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8942,"text":"ofr80180 - 1980 - Vertical crustal movements in the conterminous United States over the last 10 million years","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr80180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-180","title":"Vertical crustal movements in the conterminous United States over the last 10 million years","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80180","usgsCitation":"Gable, D.J., and Hatton, T., 1980, Vertical crustal movements in the conterminous United States over the last 10 million years: U.S. Geological Survey Open-File Report 80-180, 9 p., 33 over -size sheets, 4 fold. maps (in pocket) ;33 cm., https://doi.org/10.3133/ofr80180.","productDescription":"9 p., 33 over -size sheets, 4 fold. maps (in pocket) ;33 cm.","costCenters":[],"links":[{"id":141118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0180/report-thumb.jpg"},{"id":36554,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0180/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36555,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0180/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36556,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0180/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36557,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0180/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6021e4","contributors":{"authors":[{"text":"Gable, Dolores J.","contributorId":52957,"corporation":false,"usgs":true,"family":"Gable","given":"Dolores","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatton, Tom","contributorId":46521,"corporation":false,"usgs":true,"family":"Hatton","given":"Tom","email":"","affiliations":[],"preferred":false,"id":158598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5881,"text":"pp1101 - 1980 - The Boulder Creek Batholith, Front Range, Colorado","interactions":[{"subject":{"id":14095,"text":"ofr6570 - 1965 - Allanites from the Boulder Creek batholith, Colorado","indexId":"ofr6570","publicationYear":"1965","noYear":false,"title":"Allanites from the Boulder Creek batholith, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5881,"text":"pp1101 - 1980 - The Boulder Creek Batholith, Front Range, Colorado","indexId":"pp1101","publicationYear":"1980","noYear":false,"title":"The Boulder Creek Batholith, Front Range, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"pp1101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1101","title":"The Boulder Creek Batholith, Front Range, Colorado","docAbstract":"The Boulder Creek batholith is the best known of several large Precambrian batholiths of similar rock composition that crop out across central Colorado. The rocks in the batholith belong to the calc-alkaline series and range in composition from granodiorite through quartz diorite (tonalite) to gneissic aplite. Two rock types dominate': the Boulder Creek Granodiorite, the major rock unit, and a more leucocratic and slightly younger unit herein named Twin Spruce Quartz Monzonite. Besides mafic inclusions, which occur mainly in hornblende-bearing phases of the Boulder Creek Granodiorite, there are cogenetic older and younger lenses, dikes, and small plutons of hornblende diorite, hornblendite, gabbro, and pyroxenite. Pyroxenite is not found in the batholith. The Boulder Creek Granodiorite in the batholith represents essentially two contemporaneous magmas, a northern body occurring in the Gold Hill and Boulder quadrangles and a larger southern body exposed in the Blackhawk and the greater parts of the Tungsten and Eldorado Springs quadrangles. The two bodies are chemically and mineralogically distinct. The northern body is richer in CaO and poorer in K2O, is more mafic, and has a larger percentage of plagioclase than the southern body. \r\n\r\nA crude sequence of rock types occurs from west to east in the batholith accompanied by a change in plagioclase composition from calcic plagioclase on the west to sodic on the east. Ore minerals tend to decrease, and the ratio potassium feldspar:plagioclase increases inward from the western contact of the batholith, indicating that the Boulder Creek batholith is similar to granodiorite batholiths the world over. Emplacement of the Boulder Creek batholith was contemporaneous with plastic deformation and high-grade regional metamorphism that folded the country rock and the batholith contact along west-northwest and north-northwest axes. Also, smaller satellitic granodiorite bodies tend to conform to the trends of foliation and fold axes in the country rock, suggesting that emplacement was controlled by preexisting structures in the country rock. \r\n\r\nOn a gross scale, chemical equilibrium in the Boulder Creek Granodiorite is expressed by a near 1:1 ratio, or straight-line relationship in the distribution of iron, magnesium, and manganese in biotite and hornblende. General mineralogical trends in the Boulder Creek Granodiorite indicate that modal biotite, hornblende, and plagioclase tend to increase and quartz and microcline tend to decrease as CaO increases. These trends were not found in the Twin Spruce Quartz Monzonite. \r\n\r\nDifferentiation is believed to have played a major role and assimilation a minor role in the development of the Boulder Creek batholith. The Boulder Creek Granodiorite is of probable mantle or lower crust origin, and, based on the scant data available, the Twin Spruce Quartz Monzonite may be of crustal origin, but the magma was extensively altered by contaminants of ambiguous origin. Mafic inclusions, possibly derived from a dioritic magma which was an early differentiate associated temporally with the Boulder Creek Granodiorite and (or) the Twin Spruce Quartz Monzonite, were in jected into the Boulder Creek Granodiorite during the mush stage and before the batholith was completely crystallized. \r\n\r\nBiotite, hornblende, and potassium feldspar were studied extensively. Their chemistry and petrology indicate a homogeneity throughout the batholith not believed possible by a casual observance of the batholithic rocks in the field. The accessory minerals, where investigated, also tend to indicate this same pervasive homogeneity.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1101","usgsCitation":"Gable, D.J., 1980, The Boulder Creek Batholith, Front Range, Colorado: U.S. Geological Survey Professional Paper 1101, 88 p; 2 plates in pocket, https://doi.org/10.3133/pp1101.","productDescription":"88 p; 2 plates in pocket","costCenters":[],"links":[{"id":104551,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4720.htm","linkFileType":{"id":5,"text":"html"},"description":"4720"},{"id":124378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1101/report-thumb.jpg"},{"id":32702,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1101/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32703,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1101/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db68231b","contributors":{"authors":[{"text":"Gable, Dolores J.","contributorId":52957,"corporation":false,"usgs":true,"family":"Gable","given":"Dolores","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":151739,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62891,"text":"gq1534 - 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Regional analyses indicate that harmonic-mean temperature is negatively correlated with altitude. No change in specific conductance since 1951 was noted for the Little Snake River; however, specific conductance in the Yampa River has increaed 14 % since that time and is attributed to increased agricultural and municipal use of water. Site-specific relationships between major inorganic constituents and specific conductance for the Little Snake and Yampa Rivers were similar to regional relationships developed from both historic and recent (1975) data. These relationships provide a means for estimating concentrations of major inorganic constituents from specific conductance, which is easily measured. Trace-element and nutrient data collected from August 1975 through September 1976 at 92 sites in the Yampa River basin indicate that water-quality degradation occurred upstream from 3 sites. The degradation resulted from underground drainage from pyritic materials that probably are associated with coal at one site, discharge from powerplant cooling-tower blowdown water at a second site, and runoff from a small watershed containing a gas field at the third site. Ambient concentrations of dissolved and total iron and manganese frequently exceeded proposed Colorado water-quality standards. The concentrations of many dissolved and total trace elements and nutrients were greatest during March 1976. These were associated with larger suspended-sediment concentrations and smaller pH values than at other times of the year. 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