No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83848","usgsCitation":"Nowlan, G., Howd, F.H., and Nakagawa, H.M., 1983, Analytical results for 2244 stream-sediment samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire: U.S. Geological Survey Open-File Report 83-848, Report: i, 117 p.; 1 Plate: 30.53 × 47.40 inches, https://doi.org/10.3133/ofr83848.","productDescription":"Report: i, 117 p.; 1 Plate: 30.53 × 47.40 inches","costCenters":[],"links":[{"id":152191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0848/report-thumb.jpg"},{"id":49840,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0848/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0848/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390840,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14244.htm"}],"country":"United States","state":"Maine, New Hampshire","otherGeospatial":"Lewiston 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.211,\n 44\n ],\n [\n -70,\n 44\n ],\n [\n -70,\n 45\n ],\n [\n -71.211,\n 45\n ],\n [\n -71.211,\n 44\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca6d","contributors":{"authors":[{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":182426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howd, F. H.","contributorId":52965,"corporation":false,"usgs":true,"family":"Howd","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":182425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nakagawa, H. M.","contributorId":106475,"corporation":false,"usgs":true,"family":"Nakagawa","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8617,"text":"ofr83425 - 1983 - Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83425","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-425","title":"Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards","docAbstract":"An 1800-joule sparker survey of the West Florida continental slope between about 26?N and 29?15?N showed a top bed of Pleistocene age forming an irregular drape over a surface that is probably Pliocene. The contact between the top two layers is unconformable in the south and, in some places, shows karst collapse and solution features. Karst topography grades into a more hummocky erosional surface to the north, which in turn smoothes out; the contact become conformable still further north. A period of folding, which is widespread over the outer portion of the study area and which may be related to large scale mass wasting, occurred at about the same time represented by the unconformity. Significant subsidence has occurred as late as Pleistocene. \r\n\r\nThe surface layer thins to a minimum (0 in the south) at about 525-meters water depth and then thickens again dramatically to the west, downslope. This thinning is interpreted to be due to the Loop Current, which flows from north to south in the area and which acts to block deposition and scour the bottom. \r\n\r\nDespite the fact that the margin is dominated by carbonates, usually associated with low sedimentation rates, there is widespread evidence of mass wasting affecting ancient and surficial deposits on the outer part of the upper slope. \r\n\r\nThree potential groups of geohazards identified are: \r\n\r\n1. Potential bottom failure in areas where a thin top layer overlies the karst surface. \r\n2. Potential for sliding and slumping. \r\n3. Scour due to currents which could also affect drilling and engineering activities.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83425","usgsCitation":"Doyle, L.J., 1983, Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards: U.S. Geological Survey Open-File Report 83-425, 21 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83425.","productDescription":"21 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0425/report-thumb.jpg"},{"id":36208,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0425/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f40a9","contributors":{"authors":[{"text":"Doyle, Larry J.","contributorId":43352,"corporation":false,"usgs":true,"family":"Doyle","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7942,"text":"ofr83431A - 1983 - Idaho; basic data for thermal springs and wells as recorded in Geotherm; Part A","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83431A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-431","chapter":"A","title":"Idaho; basic data for thermal springs and wells as recorded in Geotherm; Part A","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83431A","usgsCitation":"Bliss, J.D., 1983, Idaho; basic data for thermal springs and wells as recorded in Geotherm; Part A: U.S. Geological Survey Open-File Report 83-431, 64 p. ;28 cm., https://doi.org/10.3133/ofr83431A.","productDescription":"64 p. ;28 cm.","costCenters":[],"links":[{"id":140867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0431a/report-thumb.jpg"},{"id":35513,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0431a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faae3","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7946,"text":"ofr83435 - 1983 - Oregon; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83435","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-435","title":"Oregon; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83435","usgsCitation":"Bliss, J.D., 1983, Oregon; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-435, iv, 342 leaves ;28 cm., https://doi.org/10.3133/ofr83435.","productDescription":"iv, 342 leaves ;28 cm.","costCenters":[],"links":[{"id":140871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0435/report-thumb.jpg"},{"id":35517,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0435/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691238","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7939,"text":"ofr83429 - 1983 - Colorado; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83429","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-429","title":"Colorado; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83429","usgsCitation":"Bliss, J.D., 1983, Colorado; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-429, 176 p. ;28 cm., https://doi.org/10.3133/ofr83429.","productDescription":"176 p. ;28 cm.","costCenters":[],"links":[{"id":140808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0429/report-thumb.jpg"},{"id":35510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0429/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae7e8","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43730,"text":"ofr83553 - 1983 - Land use and land cover and associated maps for Enid, Oklahoma; Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:04:52","indexId":"ofr83553","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-553","title":"Land use and land cover and associated maps for Enid, Oklahoma; Kansas","language":"ENGLISH","doi":"10.3133/ofr83553","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Enid, Oklahoma; Kansas: U.S. Geological Survey Open-File Report 83-553, maps :photocopy ;45 x 65 cm., on sheets 77 x 107 cm., https://doi.org/10.3133/ofr83553.","productDescription":"maps :photocopy ;45 x 65 cm., on sheets 77 x 107 cm.","costCenters":[],"links":[{"id":134910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b138d","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":531331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9111,"text":"ofr82726 - 1983 - STEREO; a computer program for projecting and plotting stereograms","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82726","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-726","title":"STEREO; a computer program for projecting and plotting stereograms","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82726","usgsCitation":"German, P., and Johnson, C.E., 1983, STEREO; a computer program for projecting and plotting stereograms: U.S. Geological Survey Open-File Report 82-726, 74 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82726.","productDescription":"74 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":141925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0726/report-thumb.jpg"},{"id":36721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0726/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe0a8","contributors":{"authors":[{"text":"German, Peter","contributorId":54999,"corporation":false,"usgs":true,"family":"German","given":"Peter","email":"","affiliations":[],"preferred":false,"id":159118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Carl E.","contributorId":53796,"corporation":false,"usgs":true,"family":"Johnson","given":"Carl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159117,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10335,"text":"ofr821061 - 1983 - Preliminary geologic map of the Coolin area","interactions":[],"lastModifiedDate":"2021-11-19T22:38:11.434816","indexId":"ofr821061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-1061","title":"Preliminary geologic map of the Coolin area","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821061","usgsCitation":"Miller, F.K., 1983, Preliminary geologic map of the Coolin area: U.S. Geological Survey Open-File Report 82-1061, Report: 20 p.; 1 Plate: 24.18 × 35.29 inches, https://doi.org/10.3133/ofr821061.","productDescription":"Report: 20 p.; 1 Plate: 24.18 × 35.29 inches","costCenters":[],"links":[{"id":391962,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13635.htm"},{"id":38188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1061/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38187,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1061/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1061/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Coolin area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117,\n 48.25\n ],\n [\n -116.75,\n 48.25\n ],\n [\n -116.75,\n 48.5\n ],\n [\n -117,\n 48.5\n ],\n [\n -117,\n 48.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bada","contributors":{"authors":[{"text":"Miller, Fred K.","contributorId":89503,"corporation":false,"usgs":true,"family":"Miller","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":161214,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10917,"text":"ofr83566 - 1983 - Time series analysis of Cenozoic era sea level and paleotemperature data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr83566","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-566","title":"Time series analysis of Cenozoic era sea level and paleotemperature data","docAbstract":"A statistical analysis of Cenozoic era sea level and paleotemperature data was performed to determine the cycles of each data set and the correspondence between them. Accordingly, each of the four time series were first analyzed independently in the univariate mode of a spectral analysis. The two basic data sets were then analyzed in a paired cross-spectral analysis. \r\n\r\nThe prominent periodic cycles remaining in the data sets after linear trend removal, were: sea level surface from seismic stratigraphy--9.6 million years, updated version of sea level surface from seismic stratigraphy--9.5 million years, continental paleotemperatures from paleobotanical interpretations--9.6 million years, and marine paleotemperatures from foraminiferal isotopic data--12.7 million years. The cross-correlation properties between the data sets of continental paleotemperatures from paleobotanical interpretations and sea level surface from seismic stratigraphy at the common prominent period of 9.6 million years were: (1) The squared coherency value which measures cross correlation between the two data sets has the value 0.30, and (2) the amount by which the continental paleotemperatures from paleobotanical interpretations data lags the sea level surface from seismic stratigraphy data is 2.70 million years.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr83566","usgsCitation":"Rosenfield, G.H., and Huffman, T.E., 1983, Time series analysis of Cenozoic era sea level and paleotemperature data: U.S. Geological Survey Open-File Report 83-566, iv, 42 p., https://doi.org/10.3133/ofr83566.","productDescription":"iv, 42 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":142435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0566/report-thumb.jpg"},{"id":38684,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0566/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b6ce","contributors":{"authors":[{"text":"Rosenfield, George H.","contributorId":103282,"corporation":false,"usgs":true,"family":"Rosenfield","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huffman, Tod E.","contributorId":14823,"corporation":false,"usgs":true,"family":"Huffman","given":"Tod","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42469,"text":"ofr83362 - 1983 - Section A-A', subsurface correlations of some Upper Cretaceous and Tertiary rocks from the Cherokee Ridge, Wyoming, to the southeast flank of the Sand Wash Basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr83362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-362","title":"Section A-A', subsurface correlations of some Upper Cretaceous and Tertiary rocks from the Cherokee Ridge, Wyoming, to the southeast flank of the Sand Wash Basin, Colorado","language":"ENGLISH","doi":"10.3133/ofr83362","usgsCitation":"Bader, J., 1983, Section A-A', subsurface correlations of some Upper Cretaceous and Tertiary rocks from the Cherokee Ridge, Wyoming, to the southeast flank of the Sand Wash Basin, Colorado: U.S. Geological Survey Open-File Report 83-362, 1 section on 2 sheets :photocopy ;sheets 232 x 109 cm., https://doi.org/10.3133/ofr83362.","productDescription":"1 section on 2 sheets :photocopy ;sheets 232 x 109 cm.","costCenters":[],"links":[{"id":135407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20924,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0362/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20925,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0362/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20926,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0362/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667fbe","contributors":{"authors":[{"text":"Bader, J.W.","contributorId":68281,"corporation":false,"usgs":true,"family":"Bader","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":226553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9421,"text":"ofr83172 - 1983 - Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A","interactions":[],"lastModifiedDate":"2022-10-31T19:54:25.920382","indexId":"ofr83172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-172","title":"Garnet peridotites from Williams kimberlites, north-central Montana, U.S.A","docAbstract":"Two Williams kimberlites, 250x350m and 37x390m, in the eastern part of a swarm of 30 middle Eocene alnoitic diatremes in north-central Montana, USA, contain xenoliths of garnet-bearing lherzolites, harzburgites and dunites, in addition to spinel peridotites and upper and lower crustal amphibolites and granulites. Colluvial purple, red, and pink garnets are dominantly Mg- and Cr-rich, indicating their derivation From peridotites or megacrysts, and have CaO and Cr2O3 contents that fall in the lherzolite trend.
Temperatures were calculated by the Lindsley-Dixon 20 kb method for lherzolites and by the O'Neill-Wood method for harzburgites and dunites, and pressures were calculated by the MacGregor method, or were assumed to be 50 kb for dunites. Most peridotites equilibrated at 1220-1350°C and 50-60 kb, well above a 44mW/m2 shield geotherm and on or at higher P than the graphite-diamond boundary. Four lherzolites are low T-P (830-990°C, 23-42 kb) and are close to the shield geotherm. All four low T-P lherzolites have coarse textures whereas the high T-P cluster has both coarse and porphyroclastic textures, indicating a range of conditions of deformation and recrystallization in a restricted high T-P range. The tiny size (0.01-0.2 mm) of granulated and euhedral olivines in several xenoliths shows that deformation was occurring just prior to incorporation in kimberlite and that ascent was rapid enough (40-70 km/hr) to retard Further coarsening of fine-grained olivine. For other high T-P peridotites, cessation of deformation and beginning of recrystallization before or during inclusion in kimberlite is suggested by larger (up to 3mm) euhedral olivines in a matrix of fine granulated olivine or by optical continuity of large and nearby small olivines.
Two low T-P lherzolites contain distinctive, phlogopite-rimmed, 5-8mm clots of moderate-Cr garnet + Cr-spinel + Cr-diopside + enstatite that are inferred to have formed by reaction of an initial high-Cr garnet brought into the garnet + spinel stability Field. This suggests a reduction in pressure and temperature prior to inclusion in the kimberlite, followed by metasomatic introduction of phlogopite. These textural and compositional variations of peridotites seem most compatible with kimberlite generation and ascent during dynamic diapiric perturbation of the upper mantle.
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