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,{"id":14297,"text":"ofr72190 - 1972 - Geology of the Karamadazi iron mine, Kayseri Province, Turkey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:37","indexId":"ofr72190","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":"72-190","title":"Geology of the Karamadazi iron mine, Kayseri Province, Turkey","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72190","usgsCitation":"Jacobson, H.S., Yazgan, D., Arda, T., and Filibeli, H., 1972, Geology of the Karamadazi iron mine, Kayseri Province, Turkey: U.S. Geological Survey Open-File Report 72-190, i, 8 leaves :maps ;27 cm.; 2 sheets, https://doi.org/10.3133/ofr72190.","productDescription":"i, 8 leaves :maps ;27 cm.; 2 sheets","costCenters":[],"links":[{"id":144488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fcc3","contributors":{"authors":[{"text":"Jacobson, Herbert Samuel","contributorId":87552,"corporation":false,"usgs":true,"family":"Jacobson","given":"Herbert","email":"","middleInitial":"Samuel","affiliations":[],"preferred":false,"id":169218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yazgan, Durmaz","contributorId":16417,"corporation":false,"usgs":true,"family":"Yazgan","given":"Durmaz","email":"","affiliations":[],"preferred":false,"id":169215,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arda, Turan","contributorId":44547,"corporation":false,"usgs":true,"family":"Arda","given":"Turan","email":"","affiliations":[],"preferred":false,"id":169216,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Filibeli, Huseyin","contributorId":84771,"corporation":false,"usgs":true,"family":"Filibeli","given":"Huseyin","email":"","affiliations":[],"preferred":false,"id":169217,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":35272,"text":"b1371A - 1972 - Mineral resources of the High Sierra Primitive Area, California","interactions":[],"lastModifiedDate":"2022-12-30T22:39:55.041427","indexId":"b1371A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1371","chapter":"A","title":"Mineral resources of the High Sierra Primitive Area, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1371A","usgsCitation":"Moore, J., Marks, L.Y., and Oliver, H.W., 1972, Mineral resources of the High Sierra Primitive Area, California: U.S. Geological Survey Bulletin 1371, Report: vi, 40 p.; 1 Plate: 32.00 x 30.00 inches, https://doi.org/10.3133/b1371A.","productDescription":"Report: vi, 40 p.; 1 Plate: 32.00 x 30.00 inches","costCenters":[],"links":[{"id":411264,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21472.htm","linkFileType":{"id":5,"text":"html"}},{"id":63130,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1371a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63129,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1371a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166235,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1371a/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"High Sierra Primitive Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.896,\n              36.928\n            ],\n            [\n              -118.896,\n              36.783\n            ],\n            [\n              -118.669,\n              36.783\n            ],\n            [\n              -118.669,\n              36.928\n            ],\n            [\n              -118.896,\n              36.928\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2b6","contributors":{"authors":[{"text":"Moore, James Gregory","contributorId":73622,"corporation":false,"usgs":true,"family":"Moore","given":"James Gregory","affiliations":[],"preferred":false,"id":214357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marks, Lawrence Y.","contributorId":49370,"corporation":false,"usgs":true,"family":"Marks","given":"Lawrence","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":214356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oliver, H. W.","contributorId":85570,"corporation":false,"usgs":true,"family":"Oliver","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":214358,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":16082,"text":"ofr72358 - 1972 - Availability of low-sulphur coal in Mingo County, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr72358","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":"72-358","title":"Availability of low-sulphur coal in Mingo County, West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr72358","usgsCitation":"Spencer, F., 1972, Availability of low-sulphur coal in Mingo County, West Virginia: U.S. Geological Survey Open-File Report 72-358, iii, 24 leaves :ill., folded map :, https://doi.org/10.3133/ofr72358.","productDescription":"iii, 24 leaves :ill., folded map :","costCenters":[],"links":[{"id":150333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d841","contributors":{"authors":[{"text":"Spencer, Frank D.","contributorId":58658,"corporation":false,"usgs":true,"family":"Spencer","given":"Frank D.","affiliations":[],"preferred":false,"id":172207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14396,"text":"ofr72204 - 1972 - Reconnaissance geology of the Jabal Bitran quadrangle, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr72204","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":"72-204","title":"Reconnaissance geology of the Jabal Bitran quadrangle, Kingdom of Saudi Arabia","docAbstract":"The Jabal Bitten quadrangle covers an area of 2833 sq km in the \r\neastern part of the Precambrian Shield in Saudi Arabia. The rocks in \r\nthe quadrangle are divided geographically alone arcuate north-trending \r\nlines into an eastern area of granite intruded by a swarm of dikes of \r\nrhyolite and andesite, and a western area of dominantly pelitic \r\nchlorite-sericite schist, separated by the narrow central complex of \r\nthe Idsas Range. This complex is composed of pyroclastic rocks, lava, \r\nconglomerate, marble, and plutonic mafic rocks that have been intricately modified by episodes of metamorphism, igneous intrusion, and \r\nfaulting. The Idsas Range contains ancient gold and copper mines, \r\nand deposits of magnetite, copper, asbestos, and chromite. \r\n\r\nThe rocks in the Jabal Bitten quadrangle are here interpreted to \r\nconsist of three major sedimentary and volcanic groups, the lowermost \r\nof which was deposited unconformably on hornblende-biotite granite \r\ngneiss, and all of which are intruded by granite dikes and plutons. \r\nFrom oldest to youngest the layered rocks are called Halaban Group, \r\nBi'r Khountina Group, and Murdama Group, A biotite-hornblende granite \r\nis older than uppermost Bi'r Khountina, and peralkalic granite is \r\nyounger than Murdama. \r\n\r\nThe layered rocks of these groups are generally metamorphosed to \r\nthe greenschist facies. The metamorphic grade rises abruptly at the \r\nIdsas Range to the albite-epidote-amphibolite facies and lower subfacies of the amphibolite facies in parts of the Halaban Group; some \r\nskarn east of the range may be in the upper part of the amphibolite \r\nfacies. Characteristically, the Halaban Group has the highest grade \r\nand the greatest range in metamorphic grade, and the Murdama Group \r\nhas the lowest but most uniformly developed metamorphic grade. The \r\nmetamorphism of the rocks was caused by three successive pulses of \r\nregional dynamothermal metamorphism plus contact metamorphism around \r\nthe younger bodies of plutonic igneous rocks. \r\n\r\nFour major structural elements of the quadrangle are reflected \r\nin the geography and geologic units. These are a mantled gneiss dome \r\non the east separated from a north-plunging synclinorium in rocks of the Murdama and Bi?r Khountina Groups on the west by a narrow dejective zone of the Halaban and lower Bi?r Khountina. The dejective zone is much modified by impricate overthrusts and accompanying tear faults. These major faults have pushed elements of the Halaban and Bi?r Khountina westward over Bi?r Khountina and Murdama, with the result that very complex fault patterns have evolved.\r\n\r\nOpen geochemical reconnaissance of the area disclosed one positive anomaly for nickel and 40 threshold indications of several elements, principally nickel, chromium, copper, and tungsten. Heavy-mineral and radiometric reconnaissance showed 18 areas containing scheelite and/or powellite and four areas of anomalous radioactivity. Most of these features are in the dejective zone, as are five of the nine ancient workings, the massive and disseminated magnetite, most of the secondary copper minerals, and the traces of asbestos, magnesite, and chromite known in the quadrangle. The mantled gneiss dome and a complex of gabbro and amphibolite on its southwestern flank are the next most mineralized areas. Scant evidence of mineralization is present in the Murdama Group west of the dejective zone.\r\n\r\nMagnetite deposits at Jabal Idsas have the greatest potential of the mineral deposits in the Jabal Bitran quadrangle. Further study of gold at Fawara and Selib mines is recommended, as is investigation of a positive nickel anomaly that shows threshold cobalt and above background radioactivity. The garnetiferous skarn in the east-central part of the quadrangle should be examined for composition and abrasive character of the garnet and for the remote possibility of tungsten in scheelite and beryllium in helvite.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72204","usgsCitation":"Kahr, V.P., Overstreet, W., Whitlow, J.W., and Ankary, A., 1972, Reconnaissance geology of the Jabal Bitran quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 72-204, iii, 70 leaves :ill. (some col.), folded map ;28 cm.; 1 sheet, https://doi.org/10.3133/ofr72204.","productDescription":"iii, 70 leaves :ill. (some col.), folded map ;28 cm.; 1 sheet","costCenters":[],"links":[{"id":148300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0204/report-thumb.jpg"},{"id":43074,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0204/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0204/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640a14","contributors":{"authors":[{"text":"Kahr, Viktor P.","contributorId":99569,"corporation":false,"usgs":true,"family":"Kahr","given":"Viktor","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":169385,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Overstreet, W.C.","contributorId":105294,"corporation":false,"usgs":true,"family":"Overstreet","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":169386,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whitlow, J. W.","contributorId":63810,"corporation":false,"usgs":true,"family":"Whitlow","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169383,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ankary, A.O.","contributorId":74016,"corporation":false,"usgs":true,"family":"Ankary","given":"A.O.","affiliations":[],"preferred":false,"id":169384,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14348,"text":"ofr72195 - 1972 - Mineral deposits of the northwestern Hijaz quadrangle, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2024-04-02T21:09:30.652159","indexId":"ofr72195","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":"72-195","title":"Mineral deposits of the northwestern Hijaz quadrangle, Kingdom of Saudi Arabia","docAbstract":"<p>A reconnaissance of portions of the Northwestern Hijaz quadrangle in the Kingdom of Saudi Arabia was made during 1964 and 1965 as part of a mineral survey of the Precambrian crystalline rocks of the country. The survey is being made under the terms of an agreement between the Saudi Arabia Ministry of Petroleum and Mineral Resources and the United States Geological Survey. Ancient gold and copper mines occur in the area, and deposits of iron minerals, chromite, copper minerals, asbestos, magnesite, gypsum, and glass sand have been discovered in recent years.</p><p>The land surface of the quadrangle consists of a narrow coastal plain, a mountainous belt, and a plateau. The mountainous bolt is made up of Precambrian rocks that include three major stratigraphic units separated by unconformities. The two older units are slightly metamorphosed and are intruded by plutonic rocks of many kinds. Granitic rocks predominate but intrusions of syenite, diorite, gabbro, and peridotite are known. Dikes are abundant throughout the mountainous area. The Precambrian rocks have been folded on north- to northwest-trending axes. A major northwest-striking wrench fault zone crosses the central portion of the quadrangle. North-, northeast-, and east-trending faults are locally prominent.</p><p>The plateau lies in the northeastern part of the quadrangle. It is made up of unmetamorphosed gently dipping sandstone of Paleozoic age overlain in part by flood basalts of Tertiary to Quaternary age. Sedimentary rocks of Miocene(?) age crop out in the coastal area.</p><p>Gold was mined in the area during the eighth and ninth centuries A. D. The ancient gold mines were reexamined in the 1930s but wore found to be too small and too low grade for mining. Exploration for minerals other than gold began in 1950.</p><p>The present work consisted of the examination of geological features that are potentially favorable for the presence of mineral deposits such as intrusive contacts, fault zones, quartz veins, and hydrothermally altered areas. Samples of wadi sediment were collected in areas that appeared most favorable. The samples were analyzed spectrographically for trace amounts of 27 elements to confirm the presence or absence of mineralization.</p><p>Massive magnetite bodies that range in size from a few hundred to a few thousand tons wore discovered in the course of the work as well as widely scattered traces of secondary copper minerals. The wadi samples disclosed several areas that contain from 5 to 10 times the average trace amounts of base metals and molybdenum; these areas should be prospected in more detail.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72195","usgsCitation":"Johnson, R.F., and Trent, V.A., 1972, Mineral deposits of the northwestern Hijaz quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 72-195, Report: 42 p.; 1 Figure: 40.89 x 40.24 inches; 1 Table: xiii, 11.64 x 7.75 inches, https://doi.org/10.3133/ofr72195.","productDescription":"Report: 42 p.; 1 Figure: 40.89 x 40.24 inches; 1 Table: xiii, 11.64 x 7.75 inches","costCenters":[],"links":[{"id":427322,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0195/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":427321,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0195/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427323,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1972/0195/table-1.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"}},{"id":148340,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0195/report-thumb.jpg"}],"scale":"500000","country":"Saudi Arabia","otherGeospatial":"Hijaz quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              35,\n              28\n            ],\n            [\n              35,\n              24\n            ],\n            [\n              39,\n              24\n            ],\n            [\n              39,\n              28\n            ],\n            [\n              35,\n              28\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","publicComments":"SA(IR) 80","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6359e9","contributors":{"authors":[{"text":"Johnson, Robert Francis","contributorId":8864,"corporation":false,"usgs":true,"family":"Johnson","given":"Robert","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":169301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trent, Virgil A.","contributorId":47381,"corporation":false,"usgs":true,"family":"Trent","given":"Virgil","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":169302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14603,"text":"ofr72219 - 1972 - Surficial geology of the Mount Tom quadrangle, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr72219","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":"72-219","title":"Surficial geology of the Mount Tom quadrangle, Massachusetts","docAbstract":"Movement of the last ice sheet in the Mount Tom quadrangle was due south during time of major advance as indicated by striations, drumlins, and indicator stones. Erratics of the Belchertown Tonalite, derived from the northeast portion of the Easthampton quadrangle, have been carried southward a distance of at least 16 miles. The presence of tonalite boulders on the summit of Mount Tom, elevation 1,205 feet, testifies to uplift of erratics through a vertical distance of 1,000 feet. \r\n\r\nThree tills are recognized on the basis of color, grainsize parameters, and location: (1) a reddish-brown sandy till occurs west of the Holyoke Basalt ridge, (2) a brown silty till lies east of the basalt ridge, and (3) a grayish-brown till-with intermediate grain size occurs in the Easthampton quadrangle and the north-central portion of the Mount Tom quadrangle. The three tills are the same age and are equivalent to the upper till of southern New England. During deglaciation, readvance occurred from the northeast over a minimum distance of 3.5 miles in the southeast portion of the quadrangle. Evidence for readvance consists of (1) till over stratified drift, (2) southwest-oriented till fabrics on south-trending drumlins, (3) west-southwest-trending striations cutting south-trending striations, (4) southwest-oriented glaciotectonic structures, and (5) data from borings. \r\n\r\nWest of the basalt ridge, northward retreat of an active ice margin was punctuated by four stillstands, during which outwash deltas were deposited in proglacial lakes. From oldest to youngest the deposits associated with the four stillstands are named: (1) Paper Mills delta, (2) Barnes delta, (3) Pomeroy Street delta, and (4) White Brook delta. East of the basalt ridge a series of small ice-contact deltas were deposited in high proglacial Lake Hitchcock, which expanded northward with the retreating ice margin. Deposition culminated along the upper east margin of the quadrangle with the formation of a large ice-contact delta named the Holyoke delta. \r\n\r\nContinued northward retreat of the ice margin both east and west of the basalt ridge permitted water of Lake Hitchcock to extend through the Holyoke Narrows and into the valleys of the Manhan River and Broad Brook in the north-central portion of the Mount Tom quadrangle. Drainage of Lake Hitchcock 10,700 years ago (Flint, 1956) initiated rapid downcutting by streams, as shown by numerous stream terraces along the Connecticut, Westfield, and Manhan Rivers, and along lesser tributaries.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72219","usgsCitation":"Larsen, F.D., 1972, Surficial geology of the Mount Tom quadrangle, Massachusetts: U.S. Geological Survey Open-File Report 72-219, xiii, 273 leaves :ill. (some col.), maps (some col.) ;30 cm., https://doi.org/10.3133/ofr72219.","productDescription":"xiii, 273 leaves :ill. (some col.), maps (some col.) ;30 cm.","costCenters":[],"links":[{"id":95276,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0219/plate-1.pdf","size":"7128","linkFileType":{"id":1,"text":"pdf"}},{"id":95277,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0219/plate-2.pdf","size":"5660","linkFileType":{"id":1,"text":"pdf"}},{"id":95278,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0219/plate-3.pdf","size":"3379","linkFileType":{"id":1,"text":"pdf"}},{"id":95279,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0219/plate-4.pdf","size":"7160","linkFileType":{"id":1,"text":"pdf"}},{"id":95280,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0219/plate-5.pdf","size":"3820","linkFileType":{"id":1,"text":"pdf"}},{"id":95281,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0219/plate-6.pdf","size":"9455","linkFileType":{"id":1,"text":"pdf"}},{"id":147852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0219/report-thumb.jpg"},{"id":43266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688915","contributors":{"authors":[{"text":"Larsen, Fredrick D.","contributorId":84386,"corporation":false,"usgs":true,"family":"Larsen","given":"Fredrick","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":169724,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14672,"text":"ofr72231 - 1972 - Iron prospect near Kayalar, Balikesir Province, western Turkey","interactions":[],"lastModifiedDate":"2026-04-23T17:04:37.674423","indexId":"ofr72231","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":"72-231","title":"Iron prospect near Kayalar, Balikesir Province, western Turkey","docAbstract":"<p>In July 1968 a brief reconnaissance was made of an area about 3 km northeast of Kayalar village, Balikesir Province (1:25,000 topographic sheet 119-a3), as part of the cooperative geologic program being undertaken by the Mineral Exploration and Research Institute of Turkey (MTA) and the U. S. Geological Survey (USGS) under the auspices of the Government of Turkey and the Agency for International Development,U. S. Department of State. The coordinates of Kayalar are approximately 39°50130\"N, 27°40'30\"E. This investigation was made to check a verbal report that the area contained significant iron mineralization, possibly in the form of a bedded iron deposit.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72231","usgsCitation":"Leo, G.W., 1972, Iron prospect near Kayalar, Balikesir Province, western Turkey: U.S. Geological Survey Open-File Report 72-231, i, 5 leaves :col. map ;27 cm., https://doi.org/10.3133/ofr72231.","productDescription":"5 p.","costCenters":[],"links":[{"id":503390,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0231/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148845,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0231/report-thumb.jpg"}],"country":"Turkey","otherGeospatial":"Balikesir Province, Kayalar","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672c2","contributors":{"authors":[{"text":"Leo, Gerhard W.","contributorId":26307,"corporation":false,"usgs":true,"family":"Leo","given":"Gerhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56317,"text":"wdrMI711 - 1972 - Water resources data for Michigan, water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2017-07-12T14:35:07","indexId":"wdrMI711","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":"MI-71-1","title":"Water resources data for Michigan, water year 1971; Part 1, Surface water records","docAbstract":"<p>Surface-water records for the 1971 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Michigan are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of T. R. Cummings, 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 Michigan. </p><p>Records of discharge and stage of streams, and contents and stage of lakes or reservoirs are published in a series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Through September 30, 1960, these water-supply papers were in an annual series and since then are in a 5-year series. Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Michigan were contained in Part 4 of that series. </p><p>Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Michigan, water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report MI-71-1, ix, 271 p., https://doi.org/10.3133/wdrMI711.","productDescription":"ix, 271 p.","numberOfPages":"286","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343741,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/mi-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/mi-71-1/report-thumb.jpg"}],"country":"United 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