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,{"id":15767,"text":"ofr72322 - 1972 - Reconnaissance geologic map of the Nome C-3 quadrangle, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr72322","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-322","title":"Reconnaissance geologic map of the Nome C-3 quadrangle, Seward Peninsula, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72322","usgsCitation":"Sainsbury, C., Hudson, T., Ewing, R., and Marsch, W., 1972, Reconnaissance geologic map of the Nome C-3 quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 72-322, 9 leaves :ill., 2 folded maps ;27 cm.; 1 sheet, scale 1:63,360, https://doi.org/10.3133/ofr72322.","productDescription":"9 leaves :ill., 2 folded maps ;27 cm.; 1 sheet, scale 1:63,360","costCenters":[],"links":[{"id":106533,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8705.htm","linkFileType":{"id":5,"text":"html"},"description":"8705"},{"id":148964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0322/report-thumb.jpg"},{"id":44779,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0322/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44780,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0322/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"63360","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db6413c1","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":171670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":171669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ewing, Rodney","contributorId":106914,"corporation":false,"usgs":true,"family":"Ewing","given":"Rodney","affiliations":[],"preferred":false,"id":171671,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marsch, W.R.","contributorId":25033,"corporation":false,"usgs":true,"family":"Marsch","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":171668,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":64840,"text":"i785B - 1972 - Map showing ground-water potential in the Aspen Quadrangle, Pitkin County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:53","indexId":"i785B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"785","subseriesTitle":"NONE","chapter":"B","title":"Map showing ground-water potential in the Aspen Quadrangle, Pitkin County, Colorado","language":"ENGLISH","doi":"10.3133/i785B","usgsCitation":"Bryant, B., 1972, Map showing ground-water potential in the Aspen Quadrangle, Pitkin County, Colorado: U.S. Geological Survey IMAP 785, 1 map :col. ;58 x 44 cm. folded to 26 x 22 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i785B.","productDescription":"1 map :col. ;58 x 44 cm. folded to 26 x 22 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":255220,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0785b/plate-1.pdf","size":"7923","linkFileType":{"id":1,"text":"pdf"}},{"id":255221,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0785b/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":255222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0785b/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.86749999999999,39.1175 ], [ -106.86749999999999,39.25 ], [ -106.75,39.25 ], [ -106.75,39.1175 ], [ -106.86749999999999,39.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ce0","contributors":{"authors":[{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":272245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64692,"text":"i673 - 1972 - Geologic map and cross sections of the Gallinas Creek area, Sangre de Cristo Mountains, San Miguel County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"i673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"673","subseriesTitle":"NONE","title":"Geologic map and cross sections of the Gallinas Creek area, Sangre de Cristo Mountains, San Miguel County, New Mexico","language":"ENGLISH","doi":"10.3133/i673","usgsCitation":"Baltz, E., 1972, Geologic map and cross sections of the Gallinas Creek area, Sangre de Cristo Mountains, San Miguel County, New Mexico: U.S. Geological Survey IMAP 673, 1 map :col. ;85 x 94 cm. on sheet 100 x 117 cm., https://doi.org/10.3133/i673.","productDescription":"1 map :col. ;85 x 94 cm. on sheet 100 x 117 cm.","costCenters":[],"links":[{"id":106909,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9450.htm","linkFileType":{"id":5,"text":"html"},"description":"9450"},{"id":187166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.5,35.6175 ], [ -105.5,35.784166666666664 ], [ -105.25,35.784166666666664 ], [ -105.25,35.6175 ], [ -105.5,35.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4a2f","contributors":{"authors":[{"text":"Baltz, E.H.","contributorId":67146,"corporation":false,"usgs":true,"family":"Baltz","given":"E.H.","affiliations":[],"preferred":false,"id":271990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64839,"text":"i718 - 1972 - Geologic map of the Isla de Mona Quadrangle, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:53","indexId":"i718","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"718","subseriesTitle":"NONE","title":"Geologic map of the Isla de Mona Quadrangle, Puerto Rico","language":"ENGLISH","doi":"10.3133/i718","usgsCitation":"Seiders, V., 1972, Geologic map of the Isla de Mona Quadrangle, Puerto Rico: U.S. Geological Survey IMAP 718, 1 map :col. ;69 x 66 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i718.","productDescription":"1 map :col. ;69 x 66 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106930,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9480.htm","linkFileType":{"id":5,"text":"html"},"description":"9480"},{"id":187430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91449,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0718/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -67.95083333333334,18.034166666666668 ], [ -67.95083333333334,18.166666666666668 ], [ -67.83333333333333,18.166666666666668 ], [ -67.83333333333333,18.034166666666668 ], [ -67.95083333333334,18.034166666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e6b","contributors":{"authors":[{"text":"Seiders, V.M.","contributorId":26716,"corporation":false,"usgs":true,"family":"Seiders","given":"V.M.","email":"","affiliations":[],"preferred":false,"id":272244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64686,"text":"i784I - 1972 - Natural land slopes, Hartford North Quadrangle, Connecticut","interactions":[],"lastModifiedDate":"2012-02-10T00:10:53","indexId":"i784I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"784","subseriesTitle":"NONE","chapter":"I","title":"Natural land slopes, Hartford North Quadrangle, Connecticut","language":"ENGLISH","doi":"10.3133/i784I","usgsCitation":"Barker, R., and Stone, C., 1972, Natural land slopes, Hartford North Quadrangle, Connecticut: U.S. Geological Survey IMAP 784, 1 map :col. ;58 x 44 cm., on sheet 73 x 106 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i784I.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 73 x 106 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":255114,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0784i/plate-1.pdf","size":"6888","linkFileType":{"id":1,"text":"pdf"}},{"id":255115,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0784i/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":255116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0784i/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.75,41.75 ], [ -72.75,41.8675 ], [ -72.61749999999999,41.8675 ], [ -72.61749999999999,41.75 ], [ -72.75,41.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6981cd","contributors":{"authors":[{"text":"Barker, R.M.","contributorId":59101,"corporation":false,"usgs":true,"family":"Barker","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":271983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, C.S.","contributorId":74078,"corporation":false,"usgs":true,"family":"Stone","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":271984,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12570,"text":"ofr7223 - 1972 - Geology of Area A, Catak iron deposit, Egrigoz Mountains Kutahya Province, Turkey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr7223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-23","title":"Geology of Area A, Catak iron deposit, Egrigoz Mountains Kutahya Province, Turkey","docAbstract":"The Catak iron deposit consist of magnetite-bearing lenses distributed along the northeast-trending contact of the north end of. the Egrigoz granitic massif in Kutahya Province. Area A is near the northeast end of the deposit and contains three main irregular magnetite lenses. A body of talc-silicate hornfels, almost surrounded by quartzite and schist , lies a short distance from the contact with quartz monzonite and contains the magnetite-bearing lenses west-northwest to northwest-trending structural grain is expressed by schistosity, joints, shears, lithologic contacts and outcrop patterns, although the mineralized rock and general intrusive contact trend northeast. \r\n\r\nThe ranges of the average content of Fe, Si, and S, determined from drill data are 33.54-53.95 percent; 5.86-12.25 percent; and. 8.33-9.49 percent, respectively.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr7223","usgsCitation":"Barosh, P.J., 1972, Geology of Area A, Catak iron deposit, Egrigoz Mountains Kutahya Province, Turkey: U.S. Geological Survey Open-File Report 72-23, 22 leaves :maps ;27 cm., https://doi.org/10.3133/ofr7223.","productDescription":"22 leaves :maps ;27 cm.","costCenters":[],"links":[{"id":146244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0023/report-thumb.jpg"},{"id":40947,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40948,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0023/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40949,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0023/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40950,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0023/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683ff6","contributors":{"authors":[{"text":"Barosh, Patrick James","contributorId":42184,"corporation":false,"usgs":true,"family":"Barosh","given":"Patrick","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":166357,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14242,"text":"ofr72176 - 1972 - Geology and mineral deposits of the Wadi an Nuqumi quadrangle, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr72176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-176","title":"Geology and mineral deposits of the Wadi an Nuqumi quadrangle, Kingdom of Saudi Arabia","docAbstract":"The rocks, structures, and mineral deposits of the Wadi an Nuqumi quadrangle were formed during three periods of deformation, two of Precambrian age and one of Tertiary and Recent age. The older Precambrian Halaban cycle produced the thick eugeosynclinal suite of interlayered metasedimentary and metavolcanic rocks comprising the Halaban Formation, the numerous synorogenic granitic masses which intrude the layered rocks, and the northward-trending tectonic, plutonic, and metamorphic features of all these rocks which constitute the basic grain of the area. The older Halaban features are everywhere strongly transected, but only slightly deformed and offset, by many eastward-northeastward-, and northwestward-striking fractures and strike-slip faults. Silicic dikes are emplaced in these fractures, and several kinds of barren and metalliferous veins are closely associated with them. All these features are here thought to have formed during a period of deformation of late Precambrian age which produced the Najd Wrench Fault Zone; therefore, these features are named for it. Sporadic remnants of once far more extensive basaltic lava fields and the north-northwestward-striking vertical fractures which occur in them and contain volcanic vents from which they were extruded are the youngest rocks and structures in the Wadi an Nuqumi area. They are thought to have formed during the period of tectonic and volcanic activity which also produced the Red Sea graben. \r\n\r\nThe principal mineral deposits of the Wadi an Nuqumi area are silicified-carbonate breccia veins which occur in structures of the Najd Wrench Fault deformation and metalliferous quartz veins which are closely associated with them. Only the latter possesses any economic potential, the most promising being the gold and silver-bearing quartz-base metal veins of the Al Numrahniyah and Muthaheel ancient mines.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72176","usgsCitation":"Hummel, C.L., 1972, Geology and mineral deposits of the Wadi an Nuqumi quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 72-176, 18 leaves :ill. (some folded, some col.), maps (some folded, some col.) ;27 cm.; 1 sheet, https://doi.org/10.3133/ofr72176.","productDescription":"18 leaves :ill. (some folded, some col.), maps (some folded, some col.) ;27 cm.; 1 sheet","costCenters":[],"links":[{"id":144395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0176/report-thumb.jpg"},{"id":42927,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0176/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42928,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0176/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42929,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0176/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42930,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0176/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46da","contributors":{"authors":[{"text":"Hummel, C. L.","contributorId":53798,"corporation":false,"usgs":true,"family":"Hummel","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":169138,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6363,"text":"pp698 - 1972 - Petrographic and chemical reconnaissance study of some granitic and gneissic rocks near the San Andreas fault from Bodega Head to Cajon Pass, California","interactions":[],"lastModifiedDate":"2018-03-07T11:20:43","indexId":"pp698","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"698","title":"Petrographic and chemical reconnaissance study of some granitic and gneissic rocks near the San Andreas fault from Bodega Head to Cajon Pass, California","docAbstract":"<p>This petrographic and chemical study is based on reconnaissance sampling of granitic and related gneissic rock in the California Coast and Transverse Ranges. In the Coast Ranges, granitic rocks are restricted to an elongate belt, the Salinian block, between the San Andreas and Sur-Nacimiento fault zones. These rocks have a considerable compositional range, but are dominantly quartz monzonite and granodiorite. Moist of the Salinian block seems to be a structurally coherent basement block of chemically related granitic rocks. However, on both the east and the west sides of the block, gneiss crops out in abundance; these rocks may be structurally separate from the main part of the Salinian block. In the Transverse Ranges, the granitic and related rocks are dominantly of granodiorite composition, and in many areas granitic and gneissic rocks are intimately intermixed.</p><p>Chemically the rocks of the California Coast and Transverse Ranges are somewhat intermediate in character between those of the east-central part of the Sierra Nevada batholith and those of the western part of the Sierra Nevada batholith and the southern California batholith. Probably the closest similarity is to the east-central Sierra Nevada rocks, but the rocks of the Coast and Transverse Ranges are somewhat higher in Al<sub>2</sub>O<sub>3</sub> and lower in K<sub>2</sub>O than Sierran rocks of the comparable SiO<sub>2</sub> content.</p><p>Granitic basement rocks of the Salinian block are now anomalously sandwiched between Franciscan terranes. The petrographic and chemical data are compatible with the concept that the Salinian rocks were originally part of the great batholithic belt along the west coast, which is exemplified by the Sierra Nevada hatholith. It also seems most likely that the Salinian block was transported from somewhere south of the Sierra Nevada batholith by large-scale right-lateral movement along the San Andreas fault zone.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp698","usgsCitation":"Ross, D.C., 1972, Petrographic and chemical reconnaissance study of some granitic and gneissic rocks near the San Andreas fault from Bodega Head to Cajon Pass, California: U.S. Geological Survey Professional Paper 698, Report: v, 92 p.; 2 Plates: 48.04 x 36.66 inches and 48.51 x 19.37 inches, https://doi.org/10.3133/pp698.","productDescription":"Report: v, 92 p.; 2 Plates: 48.04 x 36.66 inches and 48.51 x 19.37 inches","costCenters":[],"links":[{"id":121634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0698/report-thumb.jpg"},{"id":33731,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0698/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33732,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0698/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33733,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0698/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124,\n              32\n            ],\n            [\n              -116,\n              32\n            ],\n            [\n              -116,\n              40\n            ],\n            [\n              -124,\n              40\n            ],\n            [\n              -124,\n              32\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688138","contributors":{"authors":[{"text":"Ross, Donald C.","contributorId":146987,"corporation":false,"usgs":true,"family":"Ross","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":152580,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56309,"text":"wdrME711 - 1972 - Water resources data for Maine, water year 1971","interactions":[],"lastModifiedDate":"2025-08-19T13:54:39.325036","indexId":"wdrME711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ME-71-1","title":"Water resources data for Maine, water year 1971","docAbstract":"<p>Water resources data for the 1971 water year for Maine including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, records of water-quality data on the chemical and physical characteristics of surface- and ground-water, and records of ground-water levels in index wells are given in this report. Records for a few pertinent gaging stations in bordering States and Provinces are also included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of G. S. Hayes, District Chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Maine.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Maine, water year 1971: U.S. Geological Survey Water Data Report ME-71-1, vi, 112 p., https://doi.org/10.3133/wdrME711.","productDescription":"vi, 112 p.","costCenters":[],"links":[{"id":181429,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/me-71-1/report-thumb.jpg"},{"id":494297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/me-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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