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Reconnaissance mapping on St. Lawrence Island, Alaska has revealed seven epizonal granitic plutons of mid-Cretaceous age with a combined outcrop area of about 350 square miles. The plutonic rocks are dominantly quartz monzonite, but include minor amounts of granodiorite, monzonite, syenite, syenodiorite, and alaskite.

The plutons are structurally and petrologically similar to and about the same age as plutons on the Chukotsky Peninsula, U.S.S.R. and in western Alaska. They suggest tectonic continuity between Siberia and Alaska since at least Cretaceous time.

Several mineralized areas containing molybdenum, copper, lead, and zinc sulfides are associated with the plutonic bodies in the western part of the island.

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1971 - Water resources of Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:58","indexId":"ofr71105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-105","title":"Water resources of Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division, Alaska District,","doi":"10.3133/ofr71105","issn":"0094-9140","usgsCitation":"Feulner, A., Childers, J., and Norman, V., 1971, Water resources of Alaska: U.S. Geological Survey Open-File Report 71-105, 130 p. :ill., maps ;22 x 28 cm., https://doi.org/10.3133/ofr71105.","productDescription":"130 p. :ill., maps ;22 x 28 cm.","costCenters":[],"links":[{"id":155318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0105/report-thumb.jpg"},{"id":52406,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08d2","contributors":{"authors":[{"text":"Feulner, A.J.","contributorId":70796,"corporation":false,"usgs":true,"family":"Feulner","given":"A.J.","affiliations":[],"preferred":false,"id":189301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Childers, J.M.","contributorId":41455,"corporation":false,"usgs":true,"family":"Childers","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":189300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norman, V.W.","contributorId":85988,"corporation":false,"usgs":true,"family":"Norman","given":"V.W.","email":"","affiliations":[],"preferred":false,"id":189302,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13019,"text":"ofr7168 - 1971 - Analyses of stream-sediment samples from the Taylor Mountains D-8 quadrangle, Alaska","interactions":[],"lastModifiedDate":"2022-09-29T17:46:25.959128","indexId":"ofr7168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-68","title":"Analyses of stream-sediment samples from the Taylor Mountains D-8 quadrangle, Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7168","usgsCitation":"Clark, A.L., Condon, W.H., Hoare, J., and Sorg, D.H., 1971, Analyses of stream-sediment samples from the Taylor Mountains D-8 quadrangle, Alaska: U.S. Geological Survey Open-File Report 71-68, Report: 60 p.; 1 Plate: 17.61 × 21.21 inches, https://doi.org/10.3133/ofr7168.","productDescription":"Report: 60 p.; 1 Plate: 17.61 × 21.21 inches","costCenters":[],"links":[{"id":407621,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8661.htm","linkFileType":{"id":5,"text":"html"}},{"id":41486,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0068/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0068/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Taylor Mountains D-8 quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -159,\n 60.75\n ],\n [\n -158.625,\n 60.75\n ],\n [\n -158.625,\n 61\n ],\n [\n -159,\n 61\n ],\n [\n -159,\n 60.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680d66","contributors":{"authors":[{"text":"Clark, Allen L.","contributorId":96258,"corporation":false,"usgs":true,"family":"Clark","given":"Allen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Condon, W. H.","contributorId":28611,"corporation":false,"usgs":true,"family":"Condon","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":167146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoare, J. M.","contributorId":52143,"corporation":false,"usgs":true,"family":"Hoare","given":"J. M.","affiliations":[],"preferred":false,"id":167147,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sorg, D. H.","contributorId":63380,"corporation":false,"usgs":true,"family":"Sorg","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":167148,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20895,"text":"ofr71257 - 1971 - A heavy mineral study of Pleistocene and Holocene sediments near Nome, Alaska","interactions":[],"lastModifiedDate":"2024-02-02T21:00:58.594447","indexId":"ofr71257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-257","title":"A heavy mineral study of Pleistocene and Holocene sediments near Nome, Alaska","docAbstract":"

A heavy mineral study was carried out for sand-size fractions of onshore Holocene sediments (modern beach and river sediments), nearshore Holocene and Pleistocene relict sediments, and Pleistocene and Pliocene sediments from several nearshore drill-holes. Heavy mineral assemblages of these sediments are dominated by garnet, chlorite, epidote, chloritoid, sphene, and staurolite.

The nearshore region of Nome is mainly underlain by various types of Pleistocene sediments such as relict gravel that Mantles glacial drift, relict gravel over Nome River outwash fan, relict gravelly sand of submerged beaches, and relict gravel that mantles bedrock. In places these relict sediments are covered by Holocene sandy and muddy sediments. The high concentration of heavy minerals is expected for various relict sediments, because the latter were winnowed by several transgressions and regressions of the sea during Pleistocene time. Concentration of heavy minerals, however, is greater for Holocene sand than relict gravel, which mantles glacial drift and relict gravelly sand of submerged beaches. The high concentration of heavy minerals in Holocene sand suggests the winnowing of sand by strong bottom currents. The low concentration of heavy minerals in the relict gravel on glacial drift and relict gravelly sand of submerged beaches is probably due to the heterogenous nature of relict sediments. Sand fractions of the relict sediments probably have been introduced during the Holocene time. Also, contamination of samples of relict gravel from underlying glacial drift is suspected.

A greater concentration of coarse gold particles (1 iiuii. or larger) is found in nearshore relict gravel that mantles glacial drift than in any other sediment type. Relict gravel on glacial drift, which carries high gold values, does not show a high concentration of heavy minerals or a high concentration of garnet. Two factors account for the lack of correlation between concentration of gold and the other heavy minerals: (1) contrast between hydraulic properties of the gold particles and other heavy minerals, and (2) the heterogeneous nature of relict sediments. Because of their extremely high specific gravity, coarse gold particles are not moved by longshore currents or bottom currents from relict gravel which mantles glacial drift, whereas the heavy minerals which are mostly medium to fine sand in size, are transported by longshore currents and strong bottom currents. The Holocene sand winnowed by strong bottom currents shows a high concentration of heavy minerals.

Heavy mineral assemblages are more or less similar for the various sediments. Minor compositional variations mainly reflect the effect of sorting of mineral grains according to size and specific gravity. The frequencies of garnet and staurolite are slightly higher than average for modern beach and river sediments. In nearshore sediments, garnet is most abundant in Holocene sand winnowed by strong bottom currents. Holocene silty sediment which occurs in small patches is characterized by high concentration of micaceous minerals and low concentration of garnet, because the weak currents which deposit fine sediments usually carry light micaceous minerals in great abundance and minerals of high specific gravity like garnet in small amounts. Samples of Pleistocene glacial till and Pliocene marine silt from several nearshore drill-hole locations show high concentrations of micaceous minerals and low concentration of garnet.

Holocene, Pleistocene, and Pliocene sediments of Nome are mostly derived from the same general metamorphic source rocks of the inland region. The majority of the minerals found in heavy mineral assemblages, such as garnet, chlorite, epidote, chloritoid, sphene, staurolite, hornblende, and tremolite-actinolite, are reported to occur in the metamorphic rocks of Nome and the adjacent region.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71257","usgsCitation":"Sheth, M., 1971, A heavy mineral study of Pleistocene and Holocene sediments near Nome, Alaska: U.S. Geological Survey Open-File Report 71-257, xiii, 83 p., https://doi.org/10.3133/ofr71257.","productDescription":"xiii, 83 p.","costCenters":[],"links":[{"id":425330,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0257/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153557,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0257/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Nome","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -165.46944230357468,\n 64.51990788878058\n ],\n [\n -165.46944230357468,\n 64.48799257721126\n ],\n [\n -165.34584925658916,\n 64.48799257721126\n ],\n [\n -165.34584925658916,\n 64.51990788878058\n ],\n [\n -165.46944230357468,\n 64.51990788878058\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4c5","contributors":{"authors":[{"text":"Sheth, Madhusudan","contributorId":23014,"corporation":false,"usgs":true,"family":"Sheth","given":"Madhusudan","email":"","affiliations":[],"preferred":false,"id":183455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12880,"text":"ofr7161 - 1971 - Geology and coal resources of T. 6 S., R. 51 W., unsurveyed, Umiat principal meridian, in the Cape Beaufort coal field, northwestern Alaska","interactions":[],"lastModifiedDate":"2021-10-12T21:03:16.119186","indexId":"ofr7161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-61","title":"Geology and coal resources of T. 6 S., R. 51 W., unsurveyed, Umiat principal meridian, in the Cape Beaufort coal field, northwestern Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7161","usgsCitation":"Callahan, J.E., 1971, Geology and coal resources of T. 6 S., R. 51 W., unsurveyed, Umiat principal meridian, in the Cape Beaufort coal field, northwestern Alaska: U.S. Geological Survey Open-File Report 71-61, Report: i, 18 p. ; 4 Plates: 46.17 × 32.93 inches or smaller, https://doi.org/10.3133/ofr7161.","productDescription":"Report: i, 18 p. ; 4 Plates: 46.17 × 32.93 inches or smaller","costCenters":[],"links":[{"id":41298,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0061/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390448,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8656.htm"},{"id":41297,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0061/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41296,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0061/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41295,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0061/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41294,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0061/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0061/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Alaska","otherGeospatial":"Cape Beaufort coal field","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -163.9330,\n 68.8640\n ],\n [\n -164.167,\n 68.8640\n ],\n [\n -164.167,\n 68.9630\n ],\n [\n -163.9330,\n 68.9630\n ],\n [\n -163.9330,\n 68.8640\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6863c0","contributors":{"authors":[{"text":"Callahan, James E.","contributorId":7273,"corporation":false,"usgs":true,"family":"Callahan","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":166888,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18492,"text":"ofr7171 - 1971 - Reconnaissance geologic map and geochemical analyses of stream sediment and rock samples of the Anchorage B-7 quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr7171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-71","title":"Reconnaissance geologic map and geochemical analyses of stream sediment and rock samples of the Anchorage B-7 quadrangle, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7171","usgsCitation":"Clark, S.H., and Bartsch, S.R., 1971, Reconnaissance geologic map and geochemical analyses of stream sediment and rock samples of the Anchorage B-7 quadrangle, Alaska: U.S. Geological Survey Open-File Report 71-71, 70 leaves :ill., maps ;30 cm., https://doi.org/10.3133/ofr7171.","productDescription":"70 leaves :ill., maps ;30 cm.","costCenters":[],"links":[{"id":106523,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8663.htm","linkFileType":{"id":5,"text":"html"},"description":"8663"},{"id":151922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0071/report-thumb.jpg"},{"id":47848,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0071/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47849,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643a32","contributors":{"authors":[{"text":"Clark, Sandra H. B.","contributorId":88706,"corporation":false,"usgs":true,"family":"Clark","given":"Sandra","email":"","middleInitial":"H. B.","affiliations":[],"preferred":false,"id":179228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartsch, Susan R.","contributorId":94314,"corporation":false,"usgs":true,"family":"Bartsch","given":"Susan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":179229,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":17786,"text":"ofr71276 - 1971 - Translation of 1964 Russian correlations between Wrangel Island and northern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr71276","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-276","title":"Translation of 1964 Russian correlations between Wrangel Island and northern Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr71276","usgsCitation":"Tailleur, I.L., 1971, Translation of 1964 Russian correlations between Wrangel Island and northern Alaska: U.S. Geological Survey Open-File Report 71-276, ii, 12 leaves :ill. ;28 cm.; 13 p., https://doi.org/10.3133/ofr71276.","productDescription":"ii, 12 leaves :ill. ;28 cm.; 13 p.","costCenters":[],"links":[{"id":111702,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10925","linkFileType":{"id":5,"text":"html"}},{"id":149168,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626d87","contributors":{"authors":[{"text":"Tailleur, Irvin L.","contributorId":105304,"corporation":false,"usgs":true,"family":"Tailleur","given":"Irvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16281,"text":"ofr71284 - 1971 - The Shublik Formation and adjacent strata in northeastern Alaska description, minor elements, depositional environments and diagenesis","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr71284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-284","title":"The Shublik Formation and adjacent strata in northeastern Alaska description, minor elements, depositional environments and diagenesis","docAbstract":"The Shublik Formation (Middle and Late Triassic) is widespread in the surface and subsurface of northern Alaska. Four stratigraphic sections along about 70 miles of the front of the northeastern Brooks Range east of the Canning giver were examined and sampled in detail in 1968. These sections and six-step spectrographic and carbon analyses of the samples combined with other data to provide a preliminary local description of the highly organic unit and of the paleoenvironments. \r\n\r\nThicknesses measured between the overlying Kingak Shale of Jurassic age and the underlying Sadlerochit Formation of Permian and Triassic age range from 400 to more than 800 feet but the 400 feet, obtained from the most completely exposed section, may be closer to the real thickness across the region. The sections consist of organic-rich, phosphatic, and fossiliferous muddy, silty, or carbonate rocks. The general sequence consists, from the bottom up, of a lower unit of phosphatic siltstone, a middle unit of phosphatic carbonate rocks, and an upper unit of shale and carbonate rocks near the Canning River and shale, carbonate rocks, and sandstone to the east.\r\n\r\nAlthough previously designated a basal member of the Kingak Shale (Jurassic), the upper unit is here included with the Shublik on the basis of its regional lithologic relation. \r\n\r\nThe minor element compositions of the samples of the Shublik Formation are consistent with their carbonaceous and phosphatic natures in that relatively large amounts of copper, molybdenum, nickel, vanadium and rare earths are present. The predominantly sandy rocks of the underlying Sadlerochit Formation (Permian and Triassic) have low contents of most minor elements. The compositions of samples of Kingak Shale have a wide range not readily explicable by the nature of the rock: an efflorescent sulfate salt contains 1,500 ppm nickel and 1,500 ppm zinc and large amounts of other metals derived from weathering of pyrite and leaching of local shale. The only recorded occurrence of silver and 300 ppm lead in gouge along a shear plane may be the result of metals introduced from an extraneous source. \r\n\r\nThe deposits reflect a marine environment that deepened somewhat following deposition of the Sadlerochit Formation and then shoaled during deposition of the upper limestone-siltstone unit. This apparently resulted from a moderate transgression and regression of the sea with respect to a northwest-trending line between Barrow and the Brooks Range at the International Boundary. Nearer shore facies appear eastward. The phosphate in nodules, fossil molds and oolites, appears to have formed diagenetically within the uncompacted sediment.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr71284","usgsCitation":"Tourtelot, H.A., and Tailleur, I.L., 1971, The Shublik Formation and adjacent strata in northeastern Alaska description, minor elements, depositional environments and diagenesis: U.S. Geological Survey Open-File Report 71-284, i, 62 leaves :2 folded col. maps ;27 cm., https://doi.org/10.3133/ofr71284.","productDescription":"i, 62 leaves :2 folded col. maps ;27 cm.","costCenters":[],"links":[{"id":150502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0284/report-thumb.jpg"},{"id":45207,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0284/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45208,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0284/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a958","contributors":{"authors":[{"text":"Tourtelot, Harry Allison","contributorId":77937,"corporation":false,"usgs":true,"family":"Tourtelot","given":"Harry","email":"","middleInitial":"Allison","affiliations":[],"preferred":false,"id":172546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tailleur, Irvin L.","contributorId":105304,"corporation":false,"usgs":true,"family":"Tailleur","given":"Irvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":172547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13426,"text":"ofr7191 - 1971 - Early paleozoic fossils in the Neruokpuk Formation, northeast Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr7191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-91","title":"Early paleozoic fossils in the Neruokpuk Formation, northeast Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr7191","usgsCitation":"Dutro, J.T., Reiser, H.N., Detterman, R.L., and Brosge, W., 1971, Early paleozoic fossils in the Neruokpuk Formation, northeast Alaska: U.S. Geological Survey Open-File Report 71-91, 4 leaves ;27 cm.; 5 p., https://doi.org/10.3133/ofr7191.","productDescription":"4 leaves ;27 cm.; 5 p.","costCenters":[],"links":[{"id":111697,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10898","linkFileType":{"id":5,"text":"html"}},{"id":146484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c1e8","contributors":{"authors":[{"text":"Dutro, J. Thomas Jr.","contributorId":102878,"corporation":false,"usgs":true,"family":"Dutro","given":"J.","suffix":"Jr.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":167793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiser, H. N.","contributorId":13199,"corporation":false,"usgs":true,"family":"Reiser","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":167790,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Detterman, R. L.","contributorId":71525,"corporation":false,"usgs":true,"family":"Detterman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":167792,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brosge, W. P.","contributorId":58248,"corporation":false,"usgs":true,"family":"Brosge","given":"W. P.","affiliations":[],"preferred":false,"id":167791,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}