No abstract available.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[629:SPOAPI]2.0.CO;2","usgsCitation":"Coats, R., 1960, Stereoscopic-pair projection of aerial photographs in map compilation: Bulletin of the Geological Society of America, v. 71, no. 5, p. 629-630, https://doi.org/10.1130/0016-7606(1960)71[629:SPOAPI]2.0.CO;2.","productDescription":"2 p.","startPage":"629","endPage":"630","costCenters":[],"links":[{"id":385719,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Coats, R.R.","contributorId":78339,"corporation":false,"usgs":true,"family":"Coats","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":815909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220531,"text":"70220531 - 1960 - Glaciation of the east slope of Rocky Mountain National Park, Colorado","interactions":[],"lastModifiedDate":"2021-05-18T17:21:49.125233","indexId":"70220531","displayToPublicDate":"1960-12-31T12:16:55","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Glaciation of the east slope of Rocky Mountain National Park, Colorado","docAbstract":"The eastern slope of Rocky Mountain National Park, Colorado, has been subjected to at least three separate Pleistocene glaciations, which from oldest to youngest are correlated with the Buffalo, Bull Lake, and Pinedale glaciations of Blackwelder in the Wind River Mountains of Wyoming. In this area, deposits of the oldest glaciation are known from only one locality. Deposits of the Bull Lake glaciation comprise two sets of moraines indicative of two advances of ice separated by a significant recession; those of the Pinedale glaciation comprise three sets of moraines indicative of a maximum advance of the ice and two recessional halts or minor readvances. Moraines of two minor advances of the ice, correlated with the Temple Lake and historic stades of Neoglaciation in the Wind River Mountains, occur in the cirque heads.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[1371:GOTESO]2.0.CO;2","usgsCitation":"Richmond, G.M., 1960, Glaciation of the east slope of Rocky Mountain National Park, Colorado: Bulletin of the Geological Society of America, v. 71, no. 9, p. 1371-1382, https://doi.org/10.1130/0016-7606(1960)71[1371:GOTESO]2.0.CO;2.","productDescription":"12 p.","startPage":"1371","endPage":"1382","costCenters":[],"links":[{"id":385718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Rocky Mountain National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.051025390625,\n 40.16208338164617\n ],\n [\n -105.4193115234375,\n 40.16208338164617\n ],\n [\n -105.4193115234375,\n 40.58267063809529\n ],\n [\n -106.051025390625,\n 40.58267063809529\n ],\n [\n -106.051025390625,\n 40.16208338164617\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"71","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Richmond, Gerald M","contributorId":127101,"corporation":false,"usgs":true,"family":"Richmond","given":"Gerald","email":"","middleInitial":"M","affiliations":[],"preferred":false,"id":815908,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220530,"text":"70220530 - 1960 - Mineral paragenesis of precambrian rocks in the Tenmile Range, Colorado","interactions":[],"lastModifiedDate":"2021-05-18T17:15:38.790336","indexId":"70220530","displayToPublicDate":"1960-12-31T12:10:23","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Mineral paragenesis of precambrian rocks in the Tenmile Range, Colorado","docAbstract":"A Precambrian complex of granulite, gneiss, and migmatite, intruded by numerous plutons of granitic rocks correlated with the Silver Plume granite, is exposed in a long narrow belt along the crest and upper slopes of the Tenmile Range, Colorado. The metamorphic rocks are predominantly felsic; bands, lenses, and irregular bodies of mafic rocks rich in biotite, hornblende, and locally in sillimanite and garnet, are interlayered with the felsic rocks. The major lithologic variations in the metamorphic rock complex are believed to be due chiefly to variations in the original sedimentary rocks, which probably were interbedded sandstone, shale, and limestone. The metamorphic rocks and the Silver Plume granite reveal the age relations of quartz and the feldspars, and these relations afford considerable information on the origin and progressive transformation of the rocks. Quartz is the earliest mineral in the metamorphic rocks and is probably a relict mineral of a sandstone. It has been partially replaced by feldspar. It occurs chiefly in irregular clusters, some of which show sutured grains, enclosed in a ramifying network of feldspar. Irregular small apophyses, barbs, and prongs of feldspar penetrate the quartz clusters along grain boundaries and healed fractures in the quartz. In some of the least feldspathized quartzose metamorphic rocks the feldspar is clearly interstitial to the quartz. Quartz also occurs in feldspar as small spherical inclusions. The relations of the quartz to the feldspars show clearly that a quartzose host rock was replaced by feldspar along quartz grain boundaries, pre-existing healed fractures, and margins of shadowy areas in strained quartz grains. The textural relations of the other principal minerals in the metamorphic rocks show that plagioclase formed earlier than the microcline and that the micas were the last of the principal minerals to form. Identical paragenetic relations are found in the Silver Plume granite, and the writer concludes that the Silver Plume granite was derived by partial fusion of quartzose metamorphic rocks.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[1357:MPOPRI]2.0.CO;2","usgsCitation":"Koschmann, A.H., 1960, Mineral paragenesis of precambrian rocks in the Tenmile Range, Colorado: Bulletin of the Geological Society of America, v. 71, no. 9, p. 1357-1370, https://doi.org/10.1130/0016-7606(1960)71[1357:MPOPRI]2.0.CO;2.","productDescription":"14 p.","startPage":"1357","endPage":"1370","costCenters":[],"links":[{"id":385717,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Tenmile Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.52319335937499,\n 39.198205348894795\n ],\n [\n -105.5126953125,\n 39.198205348894795\n ],\n [\n -105.5126953125,\n 39.9602803542957\n ],\n [\n -107.52319335937499,\n 39.9602803542957\n ],\n [\n -107.52319335937499,\n 39.198205348894795\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"71","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Koschmann, A. H.","contributorId":55455,"corporation":false,"usgs":true,"family":"Koschmann","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":815907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220527,"text":"70220527 - 1960 - Geophysical investigation of Mono Basin, California","interactions":[],"lastModifiedDate":"2021-05-18T16:58:19.33331","indexId":"70220527","displayToPublicDate":"1960-12-31T11:53:55","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Geophysical investigation of Mono Basin, California","docAbstract":"Gravity and seismic studies in Mono Basin, Mono County, California, completed during the summer of 1957 revealed a large, roughly triangular block that had subsided about 18,000 ± 5000 feet and received an accumulation of about 300 ± 100 cubic miles of light clastic sediments and volcanic material of Cenozoic age. The seemingly near-vertical faults that bound this great block are displaced toward the center of the basin from the surrounding mountain masses, but in general they are parallel to well-defined Basin and Range trends. The gravity minimum anomaly associated with the Mono Basin structure has a residual gravity relief of about 50 mgals, and the lowest gravity readings (on Paoha Island) yield a complete Bouguer gravity value of about - 260 mgals with respect to the International Ellipsoid. The computed depth of subsidence is based on a density of 2.3 gms/ cm3 for the basin fill and 2.7 gms/cm3 for the basement rocks. Seismic-refraction profiles at several places in the basin demonstrate that the Cenozoic deposits are thick where the gravity is low and relatively thin where the gravity is higher. Along common seismic and gravity profiles steep seismic dips coincide with steep gravity gradients. Numerous seismic reflections are present within the basin fill. Anomalies on four aeromagnetic profiles are related in part to volcanic material within the Cenozoic section. It is concluded that Mono Basin may be a volcano-tectonic depression caused by subsidence along faults, following extrusion of magma from a magma chamber at depth. Volcanic rocks of Pliocene(?) and Pleistocene ages are exceptionally abundant in this area.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[415:GIOMBC]2.0.CO;2","usgsCitation":"Pakisek, L., Press, F., and Kane, M.F., 1960, Geophysical investigation of Mono Basin, California: Bulletin of the Geological Society of America, v. 71, no. 4, p. 415-448, https://doi.org/10.1130/0016-7606(1960)71[415:GIOMBC]2.0.CO;2.","productDescription":"34 p.","startPage":"415","endPage":"448","costCenters":[],"links":[{"id":385714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mono Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.20303344726562,\n 37.8813571797486\n ],\n [\n -118.72100830078125,\n 37.8813571797486\n ],\n [\n -118.72100830078125,\n 38.08701320402273\n ],\n [\n -119.20303344726562,\n 38.08701320402273\n ],\n [\n -119.20303344726562,\n 37.8813571797486\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"71","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pakisek, L.C.","contributorId":258180,"corporation":false,"usgs":false,"family":"Pakisek","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":815902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Press, F.","contributorId":167282,"corporation":false,"usgs":false,"family":"Press","given":"F.","email":"","affiliations":[],"preferred":false,"id":815903,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kane, M. F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":815904,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70220524,"text":"70220524 - 1960 - Application of seismic methods to a ground-water problem in northeastern Ohio","interactions":[],"lastModifiedDate":"2021-05-18T16:25:46.270443","indexId":"70220524","displayToPublicDate":"1960-12-31T10:57:42","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Application of seismic methods to a ground-water problem in northeastern Ohio","docAbstract":"Valleys cut in the bedrock in northeastern Ohio by Tertiary and Pleistocene streams have been filled by Pleistocene glacial drift so that there is little surface evidence of their existence. Some of these buried valleys are good sources of ground water, so information regarding the location, depth, and cross-section of the buried valleys is important in water-supply investigations. Detailed knowledge of the configuration of the buried valleys is useful also in interpreting the glacial history of the region. Test surveys in Portage and Summit Counties, Ohio, by the U.S. Geological Survey indicate that seismic methods can be used to determine depth to bedrock and thus to be applicable to the study of the buried valleys.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1438722","usgsCitation":"Warrick, R., and Winslow, J., 1960, Application of seismic methods to a ground-water problem in northeastern Ohio: Geophysics, v. 25, no. 2, p. 505-519, https://doi.org/10.1190/1.1438722.","productDescription":"15 p.","startPage":"505","endPage":"519","costCenters":[],"links":[{"id":385708,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Ohio","otherGeospatial":"northwest Ohio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.83642578125,\n 39.67337039176558\n ],\n [\n -82.33154296875,\n 39.67337039176558\n ],\n [\n -82.33154296875,\n 41.68932225997044\n ],\n [\n -84.83642578125,\n 41.68932225997044\n ],\n [\n -84.83642578125,\n 39.67337039176558\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"25","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Warrick, R. E.","contributorId":258173,"corporation":false,"usgs":false,"family":"Warrick","given":"R. E.","affiliations":[],"preferred":false,"id":815889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winslow, J.D.","contributorId":258174,"corporation":false,"usgs":false,"family":"Winslow","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":815890,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220580,"text":"70220580 - 1960 - Geology of the Mayagüez area, Puerto Rico","interactions":[],"lastModifiedDate":"2021-05-19T15:12:37.584864","indexId":"70220580","displayToPublicDate":"1960-12-31T10:07:45","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the Mayagüez area, Puerto Rico","docAbstract":"The Mayagüez area forms the southwestern corner of Puerto Rico, west of 67° W. and south of 18° 15' N. One-third of the 640 square kms is covered by thick alluvium. Unconformities separate a basal complex, two sequences of highly folded igneous and sedimentary rocks, and a younger sequence of gently dipping sedimentary rock. The basal Bermeja complex contains serpentinite, silicified porphyritic volcanic rock with some sedimentary rock, and minor spilite, amphibolitized spilite, and amphibolite. It is exposed chiefly in some anticlinal cores in southwestern Puerto Rico. Limestone, mudstone, andesite, and basalt form the older folded sequence. The Río Loco formation, bronzite andesite porphyry in part with pillow structures, was extruded perhaps in the Cenomanian. The Mayagüez group includes most of the rocks in southwestern Puerto Rico: the Yauco mudstone, Parguera limestone, Brujo limestone, Melones limestone, Maricao basalt, Sabana Grande andesite, and El Rayo volcanic rocks. The maximum possible age range is Turonian to Maestrichtian. The group ranges in thickness from about 800 m in the south to 3800 m in the north, and it varies in lithology from limestone in the south to mudstone and volcanic rock in the north, indicating a volcanic center to the north during that time. The second folded sequence contains andesitic volcanic rock, bedded tuff, and massive limestone. The San Germán formation (Maestrichtian) includes andesite, the Cabo Rojo agglomerate member, and the Cotui limestone member. The Jicara formation, massive limestone and bedded tuff, is Paleocene; there is one exposure of an unnamed ? Eocene marl. Post-Eocene limestone and conglomerate are also exposed in the area. The structure of the basement complex is obscured by its massiveness and by the cover of younger rocks. Two major deformations have affected the rocks of southwestern Puerto Rico since Cenomanian to Santonian time. In the Maestrichtian, the first of these formed folds with a N. 60° W. trend, asymmetric or overturned to the south. Near the south coast the folding of thin Mayagüez group rocks was probably influenced by trends in the Bermeja complex which caused deviations in the regional trends and also some overturning to the north. The San Germán formation, deposited unconformably on the eroded surface of the folded Mayagüez group, contains large allochthonous blocks of older and contemporaneous rocks. These blocks, up to 2 km by 1 km in exposure, were deposited by slumping or sliding due to gravity within and at the base and top of the San Germán formation near Lajas and San Germán. Most rocks in the blocks are extremely contorted and contain deformed Foraminifera. The San Germán and Jicara formations and perhaps the ?Eocene marls were deformed into gentle open folds trending east in the area covered by this report. Oligocene, Miocene, and younger sedimentary rocks have been tilted and uplifted. Large east-west left-lateral transcurrent faults cross the area, offsetting and offset by two sets of transverse faults (N. 45° E., N. 20° W.): most faults are probably Maestrichtian to Oligocene, although minor faulting has continued to the present. Dikes and sills of quartz diorite porphyry and mica-quartz dacite porphyry intrude the ?Maestrichtian San Germán formation and older units. A diorite plug cuts the Bermeja complex, and a granodiorite plug intrudes the Mayagüez group.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[319:GOTMAP]2.0.CO;2","usgsCitation":"Mattson, P.H., 1960, Geology of the Mayagüez area, Puerto Rico: Bulletin of the Geological Society of America, v. 71, no. 3, p. 319-362, https://doi.org/10.1130/0016-7606(1960)71[319:GOTMAP]2.0.CO;2.","productDescription":"44 p.","startPage":"319","endPage":"362","costCenters":[],"links":[{"id":385772,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Puerto Rico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.52197265625,\n 17.832374329567518\n ],\n [\n -65.302734375,\n 17.832374329567518\n ],\n [\n -65.302734375,\n 18.58377568837094\n ],\n [\n -67.52197265625,\n 18.58377568837094\n ],\n [\n -67.52197265625,\n 17.832374329567518\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"71","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mattson, Peter H.","contributorId":72659,"corporation":false,"usgs":true,"family":"Mattson","given":"Peter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":816069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220579,"text":"70220579 - 1960 - Rapid determination of fluorine in phosphate rocks","interactions":[],"lastModifiedDate":"2021-05-19T15:02:17.090391","indexId":"70220579","displayToPublicDate":"1960-12-31T09:59:06","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Rapid determination of fluorine in phosphate rocks","docAbstract":"No abstract available.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac60160a041","usgsCitation":"Shapiro, L., 1960, Rapid determination of fluorine in phosphate rocks: Analytical Chemistry, v. 32, no. 4, p. 569-570, https://doi.org/10.1021/ac60160a041.","productDescription":"2 p.","startPage":"569","endPage":"570","costCenters":[],"links":[{"id":385771,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Shapiro, Leonard","contributorId":61406,"corporation":false,"usgs":true,"family":"Shapiro","given":"Leonard","email":"","affiliations":[],"preferred":false,"id":816068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220578,"text":"70220578 - 1960 - Terrestrial ostracodes","interactions":[],"lastModifiedDate":"2021-05-20T12:29:30.347357","indexId":"70220578","displayToPublicDate":"1960-12-31T09:53:53","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Terrestrial ostracodes","docAbstract":"No abstract available.
","language":"English","publisher":"AAAS","doi":"10.1126/science.132.3423.366-b","usgsCitation":"Sohn, I.G., 1960, Terrestrial ostracodes: Science, v. 132, no. 3423, p. 366-368, https://doi.org/10.1126/science.132.3423.366-b.","productDescription":"3 p.","startPage":"366","endPage":"368","costCenters":[],"links":[{"id":385770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"132","issue":"3423","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sohn, I. G.","contributorId":70751,"corporation":false,"usgs":true,"family":"Sohn","given":"I.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":816067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220577,"text":"70220577 - 1960 - Notes on the preparation and construction of silver reductor columns","interactions":[],"lastModifiedDate":"2021-05-19T14:52:23.766753","indexId":"70220577","displayToPublicDate":"1960-12-31T09:49:34","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Notes on the preparation and construction of silver reductor columns","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(60)80069-4","usgsCitation":"Dinnin, J., 1960, Notes on the preparation and construction of silver reductor columns: Analytica Chimica Acta, v. 23, p. 295-296, https://doi.org/10.1016/S0003-2670(60)80069-4.","productDescription":"2 p.","startPage":"295","endPage":"296","costCenters":[],"links":[{"id":385769,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dinnin, J. I.","contributorId":50886,"corporation":false,"usgs":true,"family":"Dinnin","given":"J. I.","affiliations":[],"preferred":false,"id":816066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207019,"text":"70207019 - 1960 - Structure associated with rock creep in the Black Hills, South Dakota","interactions":[],"lastModifiedDate":"2019-12-03T08:04:21","indexId":"70207019","displayToPublicDate":"1960-12-31T07:04:01","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":" Structure associated with rock creep in the Black Hills, South Dakota","docAbstract":"Many areas of schist in the southern Black Hills, South Dakota, have a thin zone of disintegrated rock that is 4-10 feet below the ground surface and parallel to it. Fresh, undeformed schist overlying this zone has moved downhill in a mass-wasting process since the present surface was formed.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[1109:SAWRCI]2.0.CO;2","issn":" 00167606","usgsCitation":"Norton, J., and Redden, J.A., 1960, Structure associated with rock creep in the Black Hills, South Dakota: Geological Society of America Bulletin, v. 71, no. 7, p. 1109-1112, https://doi.org/10.1130/0016-7606(1960)71[1109:SAWRCI]2.0.CO;2.","productDescription":"4 p.","startPage":"1109","endPage":"1112","costCenters":[],"links":[{"id":369848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota ","otherGeospatial":"Black Hills","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.0625,\n 43.193162620926074\n ],\n [\n -103.16162109375,\n 43.193162620926074\n ],\n [\n -103.16162109375,\n 44.58655513209543\n ],\n [\n -104.0625,\n 44.58655513209543\n ],\n [\n -104.0625,\n 43.193162620926074\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"71","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Norton, J.J.","contributorId":25573,"corporation":false,"usgs":true,"family":"Norton","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":776525,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Redden, J. A.","contributorId":120840,"corporation":false,"usgs":true,"family":"Redden","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":776526,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70197731,"text":"70197731 - 1960 - Geologic description along U.S. Highway 299, between Weaverville and Arcata, California","interactions":[],"lastModifiedDate":"2018-06-19T12:27:19","indexId":"70197731","displayToPublicDate":"1960-12-31T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Geologic description along U.S. Highway 299, between Weaverville and Arcata, California","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geological Society of Sacramento, Annual Field Trip, June 1960, Guidebook","language":"English","publisher":"Geological Society of Sacramento","usgsCitation":"Irwin, W., 1960, Geologic description along U.S. Highway 299, between Weaverville and Arcata, California, chap. of Geological Society of Sacramento, Annual Field Trip, June 1960, Guidebook, p. 22-31.","productDescription":"10 p.","startPage":"22","endPage":"31","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70197735,"text":"70197735 - 1960 - Geologic reconnaissance of the northern Coast Ranges and Klamath Mountains, California, with a summary of the mineral resources","interactions":[],"lastModifiedDate":"2018-06-19T13:13:11","indexId":"70197735","displayToPublicDate":"1960-12-31T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5710,"text":"California Division of Mines and Geology Bulletin","active":true,"publicationSubtype":{"id":2}},"title":"Geologic reconnaissance of the northern Coast Ranges and Klamath Mountains, California, with a summary of the mineral resources","docAbstract":"No abstract available.
","largerWorkTitle":"California Division of Mines Bulletin 179","language":"English","publisher":"California Division of Mines","usgsCitation":"Irwin, W., 1960, Geologic reconnaissance of the northern Coast Ranges and Klamath Mountains, California, with a summary of the mineral resources: California Division of Mines and Geology Bulletin, 80 p.","productDescription":"80 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355163,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014191,"text":"1014191 - 1960 - Preparation of monolayer cell cultures from tissues of some lower vertebrates","interactions":[],"lastModifiedDate":"2026-02-26T15:34:05.862296","indexId":"1014191","displayToPublicDate":"1960-12-23T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Preparation of monolayer cell cultures from tissues of some lower vertebrates","docAbstract":"Cold trypsin dispersion at pH 7.2 was used to obtain cultivable cells and cell groups from tissues of six species of fresh-water bony fishes, a frog, and a turtle. The cells readily attached to glass and were capable of at least limited, and in some cases extended, division in media consisting of commercially available components.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.132.3443.1890","usgsCitation":"Wolf, K., Quimby, M.C., Pyle, E.A., and Dexter, R., 1960, Preparation of monolayer cell cultures from tissues of some lower vertebrates: Science, v. 132, no. 3443, p. 1890-1891.","productDescription":"2 p.","startPage":"1890","endPage":"1891","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":197311,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"132","issue":"3443","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66917a","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quimby, M. C.","contributorId":14334,"corporation":false,"usgs":true,"family":"Quimby","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":319938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pyle, E. A.","contributorId":51243,"corporation":false,"usgs":true,"family":"Pyle","given":"E.","middleInitial":"A.","affiliations":[],"preferred":false,"id":319940,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dexter, R.P.","contributorId":88447,"corporation":false,"usgs":true,"family":"Dexter","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":319941,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010536,"text":"70010536 - 1960 - Crystal structure refinement of reedmergnerite, the boron analog of albite","interactions":[],"lastModifiedDate":"2026-02-26T15:42:39.897743","indexId":"70010536","displayToPublicDate":"1960-12-16T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Crystal structure refinement of reedmergnerite, the boron analog of albite","docAbstract":"Ordering of boron in a feldspar crystallographic site T1(0) has been found in reedmergnerite, which has silicon-oxygen and sodium-oxygen distances comparable to those in isostructural low albite. If a simple ionic model is assumed, calculated bond strengths yield a considerable charge imbalance in reedmergnerite, an indication of the inadequacy of the model with respect to these complex structures and of the speculative nature of conclusions based on such a model.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.132.3442.1837","issn":"00368075","usgsCitation":"Clark, J.R., and Appleman, D., 1960, Crystal structure refinement of reedmergnerite, the boron analog of albite: Science, v. 132, no. 3442, p. 1837-1838.","productDescription":"2 p.","startPage":"1837","endPage":"1838","costCenters":[],"links":[{"id":219699,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"132","issue":"3442","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fcfde4b0c8380cd4e576","contributors":{"authors":[{"text":"Clark, J. R.","contributorId":55764,"corporation":false,"usgs":true,"family":"Clark","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Appleman, D.E.","contributorId":44909,"corporation":false,"usgs":true,"family":"Appleman","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":359126,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70260442,"text":"70260442 - 1960 - Synopsis of Strigeoidea (Trematoda) of fishes and their life cycles","interactions":[],"lastModifiedDate":"2024-11-01T14:50:53.671938","indexId":"70260442","displayToPublicDate":"1960-12-01T09:45:13","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Synopsis of Strigeoidea (Trematoda) of fishes and their life cycles","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hoffman, G.L., 1960, Synopsis of Strigeoidea (Trematoda) of fishes and their life cycles: Fishery Bulletin, v. 60, p. 439-469.","productDescription":"31 p.","startPage":"439","endPage":"469","costCenters":[],"links":[{"id":463540,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hoffman, Glenn L.","contributorId":95934,"corporation":false,"usgs":true,"family":"Hoffman","given":"Glenn","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":917705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220487,"text":"70220487 - 1960 - Position of the salt-water body in the magothy(?) formation in the Cedarhurst-Woodmere area of southwestern Nassau county, Long Island, N.Y.","interactions":[],"lastModifiedDate":"2021-05-18T12:15:02.115934","indexId":"70220487","displayToPublicDate":"1960-12-01T06:52:17","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Position of the salt-water body in the magothy(?) formation in the Cedarhurst-Woodmere area of southwestern Nassau county, Long Island, N.Y.","docAbstract":"The position and chloride concentration of a sizable body of salt water, moving slowly landsyard from the south-shore bays of Long Island and the Atlantic Ocean were defined by recent test drilling in the Cedarhurst-Woodmere area of southwestern Nassau County, Long Island, N. Most of the salt-water body is in the lower part of a permeable artesian aquifer; the lowermost part of the salt-water body is in clay deposits underlying the permeable aquifer. The upper limit of the salt-water body in this area was found at depths increasing progressively in a landward direction. It was 318 feet below sea level at a well in Cedarhurst and 541 feet below sea level at a well in Woodmere. The lower limit of the salt-water body was determined at depths between 578 and 630 feet below sea level in the Cedarhurst-Woodmere area. The salt-water body is more than 300 feet thick at a well in Cedarhurst, and it thins out to zero in the vicinity of a pumping center about 1- miles northeast of the Cedarhurst well. Chloride concentration in the salt-water body in the Cedarhurst-Woodmere area ranged from about 40 to 16,000 ppm (parts per million). Isochlors define a zone of diffusion about a mile wide in the Cedarhurst-Woodmere area. They indicate a thickness of diffused water ranging from a few tens to more than 150 feet vertically. Electrical-log data show that the upper boundary of the salt-water body moved upward 21 feet between 1952 and 1958 at a site in Woodmere about half a mile southwest of the pumping center. ' From this information it is inferred that between 1952 and 1958 the leading edge of the saltwater front moved landward about 2,000 feet toward the pumping center.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.8.1739","usgsCitation":"Lusczynski, N., and Swarzenski, W., 1960, Position of the salt-water body in the magothy(?) formation in the Cedarhurst-Woodmere area of southwestern Nassau county, Long Island, N.Y.: Economic Geology, v. 55, no. 8, p. 1739-1750, https://doi.org/10.2113/gsecongeo.55.8.1739.","productDescription":"12 p.","startPage":"1739","endPage":"1750","costCenters":[],"links":[{"id":385667,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.79241943359375,\n 40.561807971278185\n ],\n [\n -73.48892211914062,\n 40.561807971278185\n ],\n [\n -73.48892211914062,\n 40.92388970852943\n ],\n [\n -73.79241943359375,\n 40.92388970852943\n ],\n [\n -73.79241943359375,\n 40.561807971278185\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"8","noUsgsAuthors":false,"publicationDate":"1960-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lusczynski, N.J.","contributorId":10779,"corporation":false,"usgs":true,"family":"Lusczynski","given":"N.J.","affiliations":[],"preferred":false,"id":815734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swarzenski, W.V.","contributorId":80243,"corporation":false,"usgs":true,"family":"Swarzenski","given":"W.V.","email":"","affiliations":[],"preferred":false,"id":815735,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220096,"text":"5220096 - 1960 - Peromyscus ranges at high and low population densities","interactions":[],"lastModifiedDate":"2025-03-06T22:51:26.994478","indexId":"5220096","displayToPublicDate":"1960-11-04T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Peromyscus ranges at high and low population densities","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70170699","usgsCitation":"Cotter, R.D., and Young, L., 1960, Municipal water supplies on the Mesabi and Vermillion Iron Ranges, northeastern Minnesota, 61 p., https://doi.org/10.3133/70170699.","productDescription":"61 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320732,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Mesabi and Vermillion Iron ranges","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57248673e4b0b13d39159654","contributors":{"authors":[{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":628118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, L.H.","contributorId":169025,"corporation":false,"usgs":false,"family":"Young","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":628119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70171289,"text":"70171289 - 1960 - An automatic-tracking device for visual-accumulation-tube analysis","interactions":[],"lastModifiedDate":"2018-04-02T10:39:29","indexId":"70171289","displayToPublicDate":"1960-11-01T12:15:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"An automatic-tracking device for visual-accumulation-tube analysis","docAbstract":"No abstract available.
","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","usgsCitation":"Skinner, J.V., 1960, An automatic-tracking device for visual-accumulation-tube analysis: Water Resources Bulletin, v. November, p. 135-137.","productDescription":"3 p.","startPage":"135","endPage":"137","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321734,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"November","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e2ce4b07e28b664db81","contributors":{"authors":[{"text":"Skinner, J. V.","contributorId":32504,"corporation":false,"usgs":true,"family":"Skinner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630447,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220495,"text":"70220495 - 1960 - The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history","interactions":[],"lastModifiedDate":"2021-05-17T13:54:52.042882","indexId":"70220495","displayToPublicDate":"1960-11-01T08:47:35","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history","docAbstract":"In 1955 exploration for base and precious metals was undertaken by Bear Creek Mining Company immediately north of the Main Tintic district, Utah. During the course of this work Bear Creek became interested in the East Tintic district, primarily as a result of the activities of the U.S. Geological Survey in that area. Data published on the East Tintic district by the Survey and others were studied and map data made available from various mining companies were compiled. Preliminary economic studies were made to determine the present day value of the type of ore body discovered previously in the district. Encouraging results from these investigations led to the selection of specific targets for exploration. Recommendations for a project program were made and approved. Negotiations were successfully concluded in mid-1956 for a unit lease agreement on lands in the East Tintic district owned by the Tintic Standard and Chief Consolidated mining companies and their subsidiaries. Of the targets selected for exploration, the Chief Oxide area seemed to be one of the most prominent. Our preliminary work in the Chief Oxide area corroborated the findings of the U.S. Geological Survey described in Part I of this paper. After careful consideration it was decided to gamble the cost of an exploration shaft in this area for the purpose of providing an underground drilling platform. We also hoped by means of underground workings to establish the existence and nature of the postulated fault. A limited amount of surface drilling was done prior to shaft sinking in order to locate a shaft site and also to obtain additional information of subvolcanic structure and alteration. Underground exploration in the Chief Oxide area was started in January, 1957. The Burgin shaft was sunk to a depth of 1,100 feet and by August, 1959, lateral development on the 1050 level totaled 4,721 feet and underground diamond drilling totaled 15,480 feet. Results of the work done to date are as follows: (a) Identification of the sedimentary rock section and an interpretation of the structure in the Burgin mine area. (b) Discovery by penetration of the previously postulated East Tintic thrust fault. (c) Discovery of large zones of manganese oxides and carbonates, which were found to be closely related to silver-lead-zinc mineralization. (d) Discovery of ore-grade lead-zinc mineralization within the footwall rocks of the East Tintic thrust. (e) Discovery of high-grade silver-lead ore within the thrust zone. Insofar as ore localization is concerned the most important structural feature in the Burgin mine area is the East Tintic thrust fault-a fact that opens up new ore potential over a large part of the East Tintic district not previously explored. Although the discoveries to date must be attributed essentially to the application of geology to exploration, the tools of geochemical prospecting and geophysics were also used, and the geochemical work, in particular, was found to be a definite aid in the selection of areas for further exploration.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1507","usgsCitation":"Bush, J., Cook, D., Lovering, T.S., and Morris, H.T., 1960, The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history: Economic Geology, v. 55, no. 7, p. 1507-1540, https://doi.org/10.2113/gsecongeo.55.7.1507.","productDescription":"34 p.","startPage":"1507","endPage":"1540","costCenters":[],"links":[{"id":385678,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"east Tintic Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.9287109375,\n 38.81831117374662\n ],\n [\n -110.8795166015625,\n 38.81831117374662\n ],\n [\n -110.8795166015625,\n 40.069664523297774\n ],\n [\n -111.9287109375,\n 40.069664523297774\n ],\n [\n -111.9287109375,\n 38.81831117374662\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Bush, J.B.","contributorId":258145,"corporation":false,"usgs":false,"family":"Bush","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":815769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cook, D.R.","contributorId":20585,"corporation":false,"usgs":true,"family":"Cook","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":815770,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovering, T. S.","contributorId":108085,"corporation":false,"usgs":true,"family":"Lovering","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":815771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":815772,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70220493,"text":"70220493 - 1960 - A rapid and accurate contour interpolator","interactions":[],"lastModifiedDate":"2021-05-17T12:29:58.643014","indexId":"70220493","displayToPublicDate":"1960-11-01T07:26:11","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"A rapid and accurate contour interpolator","docAbstract":"An instrument called a \"contourpolator\" is described. The device is constructed from readily available materials costing about $2.00 and consists of 4 primary parts. Detailed instructions are provided for its assembly and use.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1555","usgsCitation":"Marsh, O., 1960, A rapid and accurate contour interpolator: Economic Geology, v. 55, no. 7, p. 1555-1560, https://doi.org/10.2113/gsecongeo.55.7.1555.","productDescription":"6 p.","startPage":"1555","endPage":"1560","costCenters":[],"links":[{"id":385674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Marsh, O.T.","contributorId":64672,"corporation":false,"usgs":true,"family":"Marsh","given":"O.T.","email":"","affiliations":[],"preferred":false,"id":815763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220489,"text":"70220489 - 1960 - Metallization and post-mineral hypogene argillization, Lost River tin mine, Alaska","interactions":[],"lastModifiedDate":"2021-05-17T12:09:18.380166","indexId":"70220489","displayToPublicDate":"1960-11-01T07:04:22","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Metallization and post-mineral hypogene argillization, Lost River tin mine, Alaska","docAbstract":"The Lost River tin and tungsten deposit occurs in a buried granite pluton and in associated rhyolite dikes that intrude Paleozoic limestone. The dikes and parts of the granite were greisenized and then argillized irregularly. Metallization accompanied greisenization rather than argilli-zation, although both processes probably were closely related in time. Iron-zinc ratios in sphalerite indicate that the ore minerals were deposited at a temperature between 425°C and 740°C. This temperature is within the range of the temperatures at which topaz, a comman associate of the ore minerals, has been synthesized in the laboratory. The temperature of deposition of the ore minerals is above the temperature interval in which clay minerals are stable. Thus, clay minerals could not have formed while ore was being deposited. As temperatures fell and entered the stability range of the clay minerals, argillic alteration encroached upon greisen ores and wall rocks. Reaction rims between quartz and topaz indicate that kaolinite could have formed according to the following reaction: topaz + quartz + water + limestone -* kaolinite + fluorite + Cajj\"C (Al,F)2Si04 + Si02 +3H2O+ CaCOa - Al2Si20B(OH)41 + CaF2 + H2CO3 The clay minerals, which formed from diverse rock types, consist of kaolinite, dickite, mixed-layered chlorite-montmorillonite, and minor montmorillonite, accompanied by variable amounts of muscovite and zinnwaldite. The dickite is most common in and near late veins that cut the earlier-formed greisen. Temperature is believed to be the principal agent governing the relations between ore deposition and argillization. Similar relations are to be expected in other high-temperature deposits where abundant veining and fracturing indicate that wall rocks reached an isothermal condition above a maximum temperature of 480°C during ore deposition.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1478","usgsCitation":"Sainsbury, C., 1960, Metallization and post-mineral hypogene argillization, Lost River tin mine, Alaska: Economic Geology, v. 55, no. 7, p. 1478-1506, https://doi.org/10.2113/gsecongeo.55.7.1478.","productDescription":"29 p.","startPage":"1478","endPage":"1506","costCenters":[],"links":[{"id":385669,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Bering land bridge","volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":815737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220488,"text":"70220488 - 1960 - Scheelite in the precambrian gneisses of Colorado","interactions":[],"lastModifiedDate":"2021-05-17T11:59:53.430829","indexId":"70220488","displayToPublicDate":"1960-11-01T06:56:15","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Scheelite in the precambrian gneisses of Colorado","docAbstract":"Scheelite of Precambrian age has been found at several localities in Colorado and Wyoming in recent years. Most of it is disseminated in regionally metamorphosed rocks, principally in calc-silicate gneiss, but also in amphibolite. Small amounts are found in pegmatites and in gold-or copper-quartz veins of Precambrian age. The scheelite in most of the deposits contains molybdenum, and much of it is accompanied by discrete powellite (CaMoCX). The scheelite deposits vary in age with the rocks that contain them and show no consistent genetic associations. Many of the deposits are products of some phase of the major plutonic stage that included regional metamorphism, migmatization, and emplacement of syntectonic granites, A few deposits may be related to younger Precambrian granites, and some are related to late diorite and pegmatite. Tungsten originally present in minor concentration in the sedimentary rocks that gave rise to the gneisses was evidently redistributed and r eery stall ized through successive Precambrian plutonic episodes. Reworked Precambrian deposits may have been a source of the tungsten in the economically important Tertiary deposits, and possibly also of molybdenum. The Precambrian scheelite deposits found thus far have proved to be of minor economic importance, but others are still being found, and many more can be presumed to exist; among these may be some of importance.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1406","usgsCitation":"Tweto, O., 1960, Scheelite in the precambrian gneisses of Colorado: Economic Geology, v. 55, no. 7, p. 1406-1428, https://doi.org/10.2113/gsecongeo.55.7.1406.","productDescription":"13 p.","startPage":"1406","endPage":"1428","costCenters":[],"links":[{"id":385668,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.072265625,\n 37.020098201368114\n ],\n [\n -102.0849609375,\n 37.020098201368114\n ],\n [\n -102.0849609375,\n 40.94671366508002\n ],\n [\n -109.072265625,\n 40.94671366508002\n ],\n [\n -109.072265625,\n 37.020098201368114\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Tweto, O.L.","contributorId":102873,"corporation":false,"usgs":true,"family":"Tweto","given":"O.L.","affiliations":[],"preferred":false,"id":815736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220751,"text":"5220751 - 1960 - Mallard age and sex determination from wings","interactions":[],"lastModifiedDate":"2025-02-05T15:08:23.791745","indexId":"5220751","displayToPublicDate":"1960-10-03T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Mallard age and sex determination from wings","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3796514","usgsCitation":"Carney, S., and Geis, A.D., 1960, Mallard age and sex determination from wings: Journal of Wildlife Management, v. 24, no. 4, p. 372-381, https://doi.org/10.2307/3796514.","productDescription":"10 p.","startPage":"372","endPage":"381","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487090,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3796514","text":"Publisher Index Page"},{"id":197416,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Louisiana, Minnesota, 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