{"pageNumber":"6729","pageRowStart":"168200","pageSize":"25","recordCount":184552,"records":[{"id":70010629,"text":"70010629 - 1963 - Radiocarbon activity of shells from living clams and snails","interactions":[],"lastModifiedDate":"2026-02-19T16:23:18.908572","indexId":"70010629","displayToPublicDate":"1963-08-16T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Radiocarbon activity of shells from living clams and snails","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.141.3581.637.a","issn":"00368075","usgsCitation":"Rubin, M., and Taylor, D., 1963, Radiocarbon activity of shells from living clams and snails: Science, v. 141, no. 3581, p. 637-637, https://doi.org/10.1126/science.141.3581.637.a.","productDescription":"1 p.","startPage":"637","endPage":"637","costCenters":[],"links":[{"id":219176,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3581","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a93cfe4b0c8380cd8103b","contributors":{"authors":[{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, D.W.","contributorId":92323,"corporation":false,"usgs":true,"family":"Taylor","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":359297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70213469,"text":"70213469 - 1963 - Elastic constants of calcite","interactions":[],"lastModifiedDate":"2020-09-18T20:25:27.36075","indexId":"70213469","displayToPublicDate":"1963-08-01T14:52:56","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Elastic constants of calcite","docAbstract":"

No abstract available.

","language":"English","publisher":"American Institute of Physics","doi":"10.1063/1.1702777","usgsCitation":"Peselnick, L., and Robie, R.A., 1963, Elastic constants of calcite: Journal of Applied Physics, v. 34, p. 2494-2495, https://doi.org/10.1063/1.1702777.","productDescription":"2 p.","startPage":"2494","endPage":"2495","costCenters":[],"links":[{"id":378564,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Peselnick, L.","contributorId":66825,"corporation":false,"usgs":true,"family":"Peselnick","given":"L.","affiliations":[],"preferred":false,"id":799230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robie, Richard A.","contributorId":92235,"corporation":false,"usgs":true,"family":"Robie","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":799231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37747,"text":"37747 - 1963 - Birds protected by Federal law","interactions":[],"lastModifiedDate":"2014-07-24T13:44:05","indexId":"37747","displayToPublicDate":"1963-08-01T13:43:29","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"455","title":"Birds protected by Federal law","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled by the Branch of Management and Enforcement.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1963, Birds protected by Federal law (Supersedes WL 432, May 1961): Wildlife Leaflet 455, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290933,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Supersedes WL 432, May 1961","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcfdae4b0824b2d17612e","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221079,"text":"70221079 - 1963 - Correlations and problems in belt series stratigraphy, Northern idaho and western Montana","interactions":[],"lastModifiedDate":"2021-06-02T12:06:12.985609","indexId":"70221079","displayToPublicDate":"1963-08-01T13:08:36","publicationYear":"1963","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":"Correlations and problems in belt series stratigraphy, Northern idaho and western Montana","docAbstract":"

A continuous strip of geologic maps has recently been completed along the Idaho-Montana state line between Clark Fork, Idaho, and Superior, Montana. New stratigraphic and petrographic information provides the basis for stratigraphic correlations and for the interpretation of facies changes in this part of the basin of deposition of the Precambrian Belt Series. Identification of facies changes is aided by the recognition of siltite (low-grade metamorphosed siltstone) as a valid rock type, in addition to quartzite and argillite, to classify most of these rocks and to establish mappable units. The older Belt rocks (Prichard through Wallace Formations) were deposited in a trough whose axis trended northwestward, perhaps approximately through Libby, Montana. Subtle facies changes suggest an ancient shore line southwest of the Coeur d'Alene district, Idaho, perhaps near the present exposed edge of the Idaho batholith. The younger Belt formations of the Missoula Group, however, thicken markedly southeastward toward Superior. Thus, the younger Belt rocks were deposited in a trough whose main axis was about at right angles to that of the older trough and perhaps was near Missoula, Montana. Deposition in the Clark Fork area was scant and often interrupted in Missoula time. The young major cross-warp in the old Belt geosyncline undoubtedly has contributed complexities to Belt correlation farther north. Detailed petrographic studies indicate that the Belt rocks from the Pend Oreille area, Idaho, are remarkably uniform in the mineralogic composition of similar rock types throughout 40,000 feet of strata. Further mineralogic studies are required to determine whether this uniformity is local or widespread. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1413:CAPIBS]2.0.CO;2","usgsCitation":"Harrison, J.E., and Campbell, A., 1963, Correlations and problems in belt series stratigraphy, Northern idaho and western Montana: Geological Society of America Bulletin, v. 74, no. 12, p. 1413-1427, https://doi.org/10.1130/0016-7606(1963)74[1413:CAPIBS]2.0.CO;2.","productDescription":"15 p.","startPage":"1413","endPage":"1427","costCenters":[],"links":[{"id":386109,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Montana","otherGeospatial":"northern Idaho, western Montana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.98242187499999,\n 46.40756396630067\n ],\n [\n -110.12695312499999,\n 46.40756396630067\n ],\n [\n -110.12695312499999,\n 49.009050809382046\n ],\n [\n -116.98242187499999,\n 49.009050809382046\n ],\n [\n -116.98242187499999,\n 46.40756396630067\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Harrison, J. E.","contributorId":54532,"corporation":false,"usgs":true,"family":"Harrison","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, A.B.","contributorId":22764,"corporation":false,"usgs":true,"family":"Campbell","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":816785,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221075,"text":"70221075 - 1963 - Anomalous gravity field in east-central California","interactions":[],"lastModifiedDate":"2021-06-01T17:44:28.299887","indexId":"70221075","displayToPublicDate":"1963-08-01T12:40:40","publicationYear":"1963","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":"Anomalous gravity field in east-central California","docAbstract":"

Bouguer gravity values at about 11,000 stations in east-central California range from -14 mgal near Merced to -274 mgal in Long Valley. Gravity lows in the west and south parts of the San Joaquin Valley and over local basins south and east of the Sierra Nevada are produced by large thicknesses of Upper Cretaceous and Cenozoic deposits. A large regional gravity low over the Sierra Nevada can be explained by isostatic compensation of the range together with the effect of the relatively low-density rocks of the Sierra Nevada batholith. A broad gravity ridge along the east side of the San Joaquin Valley shows excellent correlation with a similar magnetic ridge where the two sets of data are available, suggesting that both anomalies are caused by a dense, magnetic mass buried at an estimated depth of 5-10 miles. Seismic refraction measurements further indicate that the thickness of the earth's crust under the valley is less than 12 miles. Thus, the anomalous mass is in the lower part of the earth's crust and is conceivably related to the more mafic rocks of the earth's upper mantle. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1293:AGFIEC]2.0.CO;2","usgsCitation":"Oliver, H., and Mabey, D.R., 1963, Anomalous gravity field in east-central California: Geological Society of America Bulletin, v. 74, no. 10, p. 1293-1298, https://doi.org/10.1130/0016-7606(1963)74[1293:AGFIEC]2.0.CO;2.","productDescription":"6 p.","startPage":"1293","endPage":"1298","costCenters":[],"links":[{"id":386048,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"California","otherGeospatial":"east-central California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.51953124999999,\n 41.96765920367816\n ],\n [\n -120.5419921875,\n 37.055177106660814\n ],\n [\n -114.697265625,\n 33.247875947924385\n ],\n [\n -114.2578125,\n 34.415973384481866\n ],\n [\n -115.04882812499999,\n 35.35321610123823\n ],\n [\n -119.970703125,\n 38.993572058209466\n ],\n [\n -119.970703125,\n 41.96765920367816\n ],\n [\n -122.51953124999999,\n 41.96765920367816\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Oliver, Howard W.","contributorId":78704,"corporation":false,"usgs":true,"family":"Oliver","given":"Howard W.","affiliations":[],"preferred":false,"id":816703,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mabey, Don R.","contributorId":43741,"corporation":false,"usgs":true,"family":"Mabey","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":816704,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221070,"text":"70221070 - 1963 - Facies and types of hydrothermal alteration","interactions":[],"lastModifiedDate":"2021-06-01T17:15:36.664729","indexId":"70221070","displayToPublicDate":"1963-08-01T12:11:17","publicationYear":"1963","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":"Facies and types of hydrothermal alteration","docAbstract":"

No abstract available. 

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.58.5.808","usgsCitation":"Hemley, J., and Hostetler, P.B., 1963, Facies and types of hydrothermal alteration: Economic Geology, v. 58, no. 5, p. 808-811, https://doi.org/10.2113/gsecongeo.58.5.808.","productDescription":"4 p.","startPage":"808","endPage":"811","costCenters":[],"links":[{"id":386043,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"5","noUsgsAuthors":false,"publicationDate":"1963-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hemley, J.J.","contributorId":59556,"corporation":false,"usgs":true,"family":"Hemley","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":816693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hostetler, P. B.","contributorId":107849,"corporation":false,"usgs":false,"family":"Hostetler","given":"P.","email":"","middleInitial":"B.","affiliations":[{"id":13719,"text":"Department of Geology, University of Missouri","active":true,"usgs":false}],"preferred":false,"id":816694,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221120,"text":"70221120 - 1963 - Two pollen diagrams from southeastern Minnesota: Problems in the regional late-glacial and postglacial vegetational history","interactions":[],"lastModifiedDate":"2021-06-02T16:23:13.324044","indexId":"70221120","displayToPublicDate":"1963-08-01T11:18:24","publicationYear":"1963","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":"Two pollen diagrams from southeastern Minnesota: Problems in the regional late-glacial and postglacial vegetational history","docAbstract":"

Kirchner Marsh and Lake Carlson are located 3 miles apart in Dakota County about 15 miles south of Minneapolis in the St. Croix moraine, which was formed by the Superior lobe during the Gary phase of the Wisconsin glaciation. During the Mankato phase that followed, the Des Moines lobe advanced to within a few miles of the sites. The region today is in a mixed-oak forest, with a maplebasswood forest 15 miles to the west and a re-entrant of the prairie on the sand plain south of the moraine. The general limit of coniferous trees is about 50 miles northeast of the sites, although outliers, especially of Pinus strobus, may be found along the Mississippi Valley a few miles to the east. One sediment core 12-13 m long from each site was analyzed for pollen content at 5-25-cm intervals. Diagrams based on percentage of total pollen (trees, shrubs, wind-pollinated herbs) show essentially identical sequences at the two sites, starting with the late-glacial phase of ice retreat. The diagrams have been subdivided into pollen zones according to the A-B-C sequence introduced by Deevey for New England. The late-glacial pollen record starts at Kirchner Marsh with a short Picea-Cyperaceae-Gramineae phase (Zone K), believed to represent a spruce parkland. Its C-14 date of 13,270 BP and the stratigraphy indicate a pre-Two Creeks and post- Gary correlation. Apparently the Kirchner site did not become established as a lake until this time owing to persistence of dead ice in the moraine. The absence of pollen of specific tundra indicators and the presence of pollen of such thermophilous plants as Fraxinus, Quercus, Corylus, Ambrosia, Humulus, and Typha latifolia imply that the climate was cool rather than cold. Zone A-a, which follows, correlates with the Two Creeks interstade. It is marked by the dominance of Picea, with appreciable percentages of Fraxinus and Ambrosia and with minor amounts of other thermophilous plants and the normal boreal associates of spruce like Betula, Larix, and Salix. Zone A-b, starting 12,050 C-14 years ago, correlates with the Valders ice advance. It is represented at both Kirchner and Carlson and shows the withdrawal of Fraxinus and Ambrosia and the slight rise of Artemisia. Except for the absence of pine in the late-glacial assemblage the vegetation implied by these three zones seems to have its closest modern counterpart in the southern fringe of the Boreal Forest of the Riding Mountain region of southwest Manitoba. It is concluded that pine did not migrate southward with the spruce during the Wisconsin glaciation, at least in the western Great Lakes region, and was thus eliminated from this region. During the lateglacial phases of ice retreat, herbs and spruce pioneered on the deglaciated terrain; pine did not follow until the destruction of the spruce forest at the end of the late-glacial phase. Zone B introduces postglacial time. It represents the time of rapid Vegetational succession following the deterioration of the spruce forest. Simultaneous maxima of Betula, Alnus, Fraxinus, and Abies occurred 10,230 years ago at Kirchner Marsh. These were followed rapidly by a Pinus maximum and then a rise of Ulmus, Quercus, and other deciduous types, dated as 9300 years ago at the correlative site of Madeha. This succession may represent differential rates of migration from refuges south and east of Minnesota. Deciduous trees dominate the C Zones. Zone C-a shows Ulmus and Ostrya /Carpinus followed by Quercus; it probably represents principally a mesic maple-basswood forest changing to oak. Zone C-b represents the advance of prairie into the region at the expense of the oak woodland or savanna. The large and abrupt fluctuations in the curves for Ambrosia-type and Chenopodiineae, especially at the Carlson site, may record encroachment of annual weeds onto intermittently dried lake bottoms. C-14 dates place Zone C-b between 7100 and 5100 years ago. In Zone C-c the Quercus again dominates until the abrupt increase in Ambrosiatype and Chenopodiineae that marks the time of forest clearance and land settlement 50-75 years ago. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1371:TPDFSM]2.0.CO;2","usgsCitation":"Wright, H., Winter, T.C., and Patten, H.L., 1963, Two pollen diagrams from southeastern Minnesota: Problems in the regional late-glacial and postglacial vegetational history: Geological Society of America Bulletin, v. 74, no. 11, p. 1371-1396, https://doi.org/10.1130/0016-7606(1963)74[1371:TPDFSM]2.0.CO;2.","productDescription":"26 p.","startPage":"1371","endPage":"1396","costCenters":[],"links":[{"id":386134,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"southeastern Minnesota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.39453125,\n 43.58039085560784\n ],\n [\n -91.14257812499999,\n 43.58039085560784\n ],\n [\n -91.14257812499999,\n 45.182036837015886\n ],\n [\n -94.39453125,\n 45.182036837015886\n ],\n [\n -94.39453125,\n 43.58039085560784\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wright, H.E. Jr.","contributorId":56369,"corporation":false,"usgs":true,"family":"Wright","given":"H.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":816797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":816798,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patten, Harvey L.","contributorId":259197,"corporation":false,"usgs":false,"family":"Patten","given":"Harvey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816799,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221119,"text":"70221119 - 1963 - Early pennsylvanian currents in the southern Appalachian Mountains","interactions":[],"lastModifiedDate":"2021-06-02T16:06:25.298065","indexId":"70221119","displayToPublicDate":"1963-08-01T11:00:12","publicationYear":"1963","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":"Early pennsylvanian currents in the southern Appalachian Mountains","docAbstract":"

Measurement of more than 1200 cross-beds in lower Pennsylvanian sandstones of the southern Appalachian Mountains reveals a broad pattern of sediment transport to the southwest and west. Most of the sand appears to have been derived from the east and to have moved south-westward parallel to the axis of the Appalachian geosyncline. The pattern has a similar alignment to that in the Illinois basin, but it is at right angles to earlier Paleozoic dispersal directions in the Appalachian geosyncline. Little or no sand has been contributed from the Cincinnati arch. The cross-beds are in sheetlike sandstone formations; the sandstone is conglomeratic, contains plant impressions, and is composed of lenticular, channeling, quartzose sedimentation units. The variation in thickness and lateral persistence of sedimentation units is also reflected in a moderate variability of mean cross-bedding directions between adjacent formations, and even within the same formation. Cross-bedding variability between adjacent units is thought to be due to regional changes in the position and orientation of channel-way systems from deposition of one sandstone formation to the next. Changes of cross-bedding azimuths within the same formation may result from channel curvature of local meanderlike deposits or from channel migration as the sands coalesced into a blanket deposit. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1439:EPCITS]2.0.CO;2","usgsCitation":"Schlee, J., 1963, Early pennsylvanian currents in the southern Appalachian Mountains: Geological Society of America Bulletin, v. 74, no. 12, p. 1439-1451, https://doi.org/10.1130/0016-7606(1963)74[1439:EPCITS]2.0.CO;2.","productDescription":"13 p.","startPage":"1439","endPage":"1451","costCenters":[],"links":[{"id":386132,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky, Tennessee, Alabama, Georgia","otherGeospatial":"southern Appalachian Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.58447265624999,\n 37.16031654673677\n ],\n [\n -84.561767578125,\n 35.71975793933433\n ],\n [\n -86.59423828125,\n 34.66935854524543\n ],\n [\n -85.902099609375,\n 34.161818161230386\n ],\n [\n -81.090087890625,\n 36.54494944148322\n ],\n [\n -80.595703125,\n 37.06394430056685\n ],\n [\n -81.58447265624999,\n 37.16031654673677\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schlee, John","contributorId":16078,"corporation":false,"usgs":true,"family":"Schlee","given":"John","affiliations":[],"preferred":false,"id":816796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221116,"text":"70221116 - 1963 - Metasomatic origin of large parts of the Adirondack Phacoliths","interactions":[],"lastModifiedDate":"2021-06-02T15:48:00.635914","indexId":"70221116","displayToPublicDate":"1963-08-01T10:42:22","publicationYear":"1963","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":"Metasomatic origin of large parts of the Adirondack Phacoliths","docAbstract":"

A metasomatic origin seems established for large parts of the granite phacoliths in the northwest Adirondack Mountains, New York. This conclusion is based upon the discovery and detailed mapping of a blurred but widespread stratigraphic sequence in the phacoliths. Highly complicated patterns of relict beds are defined by alternations of granitic gneiss, amphibolite, oligoclase-quartz gneiss, and a predominant alaskitic granite. Regional reconstructions indicate these relict beds comprise a major basal formation, probably of arkosic and calcareous quartzites, in the exposed Grenville metasedimentary rocks. The existing amphibolite interlayers formed early in the metasomatic epoch, probably replacing the more calcareous quartzite beds. This mafic metasomatism was overlapped and followed by pervasive granitization of the arkosic and highly quartzose members. Pink alaskitic granite is the final metasomacic product. It tends to replace all pre-existing rock types, especially in the cores of the antiforms. This mafic and granitic metasomatism occurred during the evolution of the major folds in the metasedimentary sequence. As the folds evolved, rising domes in the quartzite probed upward into successively higher horizons in the overlying marbles. At least three quartzite antiforms (California, Clark Pond, and South Edwards phacoliths) punctured the overlying marble, invading the basal layers of the Adirondack paragneiss. The crests of the evolving folds in the basal quartzite, capped by carbonate-rich marble, acted as traps for aqueous and carbonated, alkali-bearing fluids, and perhaps some associated anatectic granitic magma generated in the deeper, hotter basement to the Grenville. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[349:MOOLPO]2.0.CO;2","usgsCitation":"Engel, A., and Engel, C., 1963, Metasomatic origin of large parts of the Adirondack Phacoliths: Geological Society of America Bulletin, v. 74, no. 3, p. 349-352, https://doi.org/10.1130/0016-7606(1963)74[349:MOOLPO]2.0.CO;2.","productDescription":"4 p.","startPage":"349","endPage":"352","costCenters":[],"links":[{"id":386130,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Adirondack Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.30578613281247,\n 42.98053954751645\n ],\n [\n -73.35021972656247,\n 42.98053954751645\n ],\n [\n -73.35021972656247,\n 44.902577996288876\n ],\n [\n -75.30578613281247,\n 44.902577996288876\n ],\n [\n -75.30578613281247,\n 42.98053954751645\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Engel, A.E.J.","contributorId":241621,"corporation":false,"usgs":false,"family":"Engel","given":"A.E.J.","affiliations":[],"preferred":false,"id":816794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engel, C.G.","contributorId":18489,"corporation":false,"usgs":true,"family":"Engel","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":816795,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221108,"text":"70221108 - 1963 - Natural radioactivity in Washington County, Maryland","interactions":[],"lastModifiedDate":"2021-06-02T12:42:32.671397","indexId":"70221108","displayToPublicDate":"1963-08-01T07:38:25","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Natural radioactivity in Washington County, Maryland","docAbstract":"

Natural gamma-radioactivity patterns in Washington County, Maryland, reflect the principal variations in lithology. The highest radioactivity is associated with the more argillaceous parts of the geologic section and with soils derived from high-potassium carbonate rocks. Surface radiation intensity ranges from about 5 to 30 microroentgens per hour, of which the rocks contribute 30 to 90 percent. From the aerial survey data, the surface radiation intensity from extended sources can be estimated to within about three microroentgens per hour and the equivalent uranium content can be estimated to within approximately 5 ppm. 

","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1439174","usgsCitation":"Moxham, R., 1963, Natural radioactivity in Washington County, Maryland: Geophysics, v. 28, no. 2, p. 262-272, https://doi.org/10.1190/1.1439174.","productDescription":"11 p.","startPage":"262","endPage":"272","costCenters":[],"links":[{"id":386117,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","county":"Washington County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.4805908203125,\n 39.17691709496078\n ],\n [\n -77.552490234375,\n 39.17691709496078\n ],\n [\n -77.552490234375,\n 39.74521015328692\n ],\n [\n -79.4805908203125,\n 39.74521015328692\n ],\n [\n -79.4805908203125,\n 39.17691709496078\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"28","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":816786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010686,"text":"70010686 - 1963 - Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2026-02-19T16:31:54.252374","indexId":"70010686","displayToPublicDate":"1963-07-26T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska","docAbstract":"

Ostracods and Foraminifera, associated with mollusks, indicate a marine depositional environment for part of the Bootlegger Cove Clay. The definite Arctic and North Atlantic affinities of the microfauna suggest a possible migration through the Bering-Chukchi seaway during the late Pleistocene.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.141.3578.350","issn":"00368075","usgsCitation":"Schmidt, R., 1963, Pleistocene marine microfauna in the Bootlegger Cove Clay, Anchorage, Alaska: Science, v. 141, no. 3578, p. 350-351, https://doi.org/10.1126/science.141.3578.350.","productDescription":"2 p.","startPage":"350","endPage":"351","costCenters":[],"links":[{"id":219406,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -150.0872180734081,\n 61.27817705429962\n ],\n [\n -150.0872180734081,\n 61.1046048078652\n ],\n [\n -149.62700471668575,\n 61.1046048078652\n ],\n [\n -149.62700471668575,\n 61.27817705429962\n ],\n [\n -150.0872180734081,\n 61.27817705429962\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"141","issue":"3578","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7c4ee4b0c8380cd798f5","contributors":{"authors":[{"text":"Schmidt, R.A.M.","contributorId":85321,"corporation":false,"usgs":true,"family":"Schmidt","given":"R.A.M.","email":"","affiliations":[],"preferred":false,"id":359426,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70219984,"text":"70219984 - 1963 - A stimulating environment","interactions":[],"lastModifiedDate":"2021-04-16T16:31:14.356783","indexId":"70219984","displayToPublicDate":"1963-07-12T11:27:54","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"A stimulating environment","docAbstract":"

No abstract available. 

","language":"English","publisher":"AAAS","doi":"10.1126/science.141.3576.232-a","usgsCitation":"Bradley, W., 1963, A stimulating environment: Science, v. 141, no. 3576, https://doi.org/10.1126/science.141.3576.232-a.","productDescription":"1 p.","endPage":"232","numberOfPages":"232","costCenters":[],"links":[{"id":385159,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3576","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, W.H.","contributorId":220222,"corporation":false,"usgs":false,"family":"Bradley","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":814405,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010769,"text":"70010769 - 1963 - Transformation of montmorillonite to kaolinite during weathering","interactions":[],"lastModifiedDate":"2026-02-19T16:39:42.431537","indexId":"70010769","displayToPublicDate":"1963-07-12T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Transformation of montmorillonite to kaolinite during weathering","docAbstract":"Extensive deposits of kaolinite in Florida are formed by transformation of montmorillonite during low-temperature supergene weathering. The transformation occurs by intracrystalline leaching of interlayer cations and tetrahedral silica layers. Interposition of stripped layers within montmorillonite creates a regular 1:1 mixed-layered montmorillonite-kaolinite, a new clay structure. Kaolin-like layers are nourished by lateral epitaxy, as the iron-rich montmorillonite decomposes. Hexagonal outgrowths of new kaolinite develop at the edges of montmorillonite flakes and nucleate new vertical growth. Kaolinitic sands impregnated with goethite are ultimately formed, and the released silica enriches groundwater and forms secondary chert.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.141.3576.148","issn":"00368075","usgsCitation":"Altschuler, Z., Dwornik, E., and Kramer, H., 1963, Transformation of montmorillonite to kaolinite during weathering: Science, v. 141, no. 3576, p. 148-152, https://doi.org/10.1126/science.141.3576.148.","productDescription":"5 p.","startPage":"148","endPage":"152","costCenters":[],"links":[{"id":218657,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"141","issue":"3576","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb6d4e4b08c986b326ee2","contributors":{"authors":[{"text":"Altschuler, Z. S.","contributorId":42962,"corporation":false,"usgs":true,"family":"Altschuler","given":"Z. S.","affiliations":[],"preferred":false,"id":359606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dwornik, E.J.","contributorId":99128,"corporation":false,"usgs":true,"family":"Dwornik","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":359608,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kramer, H.","contributorId":68876,"corporation":false,"usgs":true,"family":"Kramer","given":"H.","affiliations":[],"preferred":false,"id":359607,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221798,"text":"70221798 - 1963 - Reef Creek Detachment Fault, Northwestern Wyoming","interactions":[],"lastModifiedDate":"2021-07-07T13:13:32.878063","indexId":"70221798","displayToPublicDate":"1963-07-07T08:10:45","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Reef Creek Detachment Fault, Northwestern Wyoming","docAbstract":"

he Reef Creek fault is in northwestern Wyoming, a few miles east of the northeast border of Yellowstone National Park. It lies within the area covered by the more extensive Heart Mountain fault. Like that fault, it is a décollement or detachment fault in which strata became detached along a basal shearing plane and moved laterally on a slightly inclined fault surface. At the most northwesterly exposures the Reef Creek fault parallels the bedding; southeastward it cuts upward across the bedding as a transgressive fault and becomes a fault in which the allochthonous blocks moved on the surface of the ground. The fault blocks consist chiefly of the Madison Limestone of Mississippian age and volcanic tuffs and breccias of the Cathedral Cliffs Formation of early or middle Eocene age. The Reef Creek fault blocks are scattered over a 7- by 14-mile area, but a considerable part of the scattering is due to “piggy-back” transportation on the Heart Mountain fault blocks.

The Reef Creek fault is younger than the Cathedral Cliffs Formation and older than the middle Eocene early basic breccia. Consequently, the rocks transported by it were emplaced either in late early Eocene or in early middle Eocene time. Both the Reef Creek fault and the South Fork fault are older than the principal movement along the Heart Mountain fault. The movement of all three fault masses was southeastward, and the mechanics of their emplacement is believed to have been similar. Movement was due in part to gravity, but considering the low slope involved, gravity alone seems to be inadequate. The shaking motion of many earthquakes is suggested as a contributing force which acted in conjunction with the constant force of gravity.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1225:RCDFNW]2.0.CO;2","usgsCitation":"Pierce, W., 1963, Reef Creek Detachment Fault, Northwestern Wyoming: GSA Bulletin, v. 74, no. 10, p. 1225-1236, https://doi.org/10.1130/0016-7606(1963)74[1225:RCDFNW]2.0.CO;2.","productDescription":"12 p.","startPage":"1225","endPage":"1236","costCenters":[],"links":[{"id":386990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Reef Creek Detachment Fault","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.23681640625,\n 44.22945656830167\n ],\n [\n -108.91845703124999,\n 44.22945656830167\n ],\n [\n -108.91845703124999,\n 45.089035564831036\n ],\n [\n -110.23681640625,\n 45.089035564831036\n ],\n [\n -110.23681640625,\n 44.22945656830167\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pierce, William G.","contributorId":103349,"corporation":false,"usgs":true,"family":"Pierce","given":"William G.","affiliations":[],"preferred":false,"id":818760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221797,"text":"70221797 - 1963 - Maskelynite: Formation by explosive shock","interactions":[],"lastModifiedDate":"2021-07-07T12:55:15.51846","indexId":"70221797","displayToPublicDate":"1963-07-07T07:51:20","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Maskelynite: Formation by explosive shock","docAbstract":"

When high pressure (250 to 300 kilobars) was applied suddenly (shock-loading) to gabbro, the plagioclase was transformed to a noncrystalline phase (maskelynite) by a solid-state reaction at a low temperature, while the proxene remained crystalline. The shock-loaded gabbro resembles meteorites of the shergottite class; this suggests that the latter formed as a result of shock. The shock-loading of gabbro at 600 to 800 kilobars raised the temperature above the melting range of the plagioclase.

","language":"English","publisher":"AAAS","doi":"10.1126/science.140.3567.670","usgsCitation":"Milton, D.J., and De Carli, P.S., 1963, Maskelynite: Formation by explosive shock: Science, v. 140, no. 3567, p. 670-671, https://doi.org/10.1126/science.140.3567.670.","productDescription":"2 p.","startPage":"670","endPage":"671","costCenters":[],"links":[{"id":386989,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"140","issue":"3567","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Milton, Daniel J.","contributorId":54963,"corporation":false,"usgs":true,"family":"Milton","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":818758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"De Carli, P. S.","contributorId":31520,"corporation":false,"usgs":true,"family":"De Carli","given":"P.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":818759,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014187,"text":"1014187 - 1963 - Egg-associated transmission of IPN virus of trouts","interactions":[],"lastModifiedDate":"2026-03-17T13:48:36.934882","indexId":"1014187","displayToPublicDate":"1963-07-02T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3696,"text":"Virology","active":true,"publicationSubtype":{"id":10}},"title":"Egg-associated transmission of IPN virus of trouts","docAbstract":"

Infectious pancreatic necrosis virus (IPN) of salmonid fishes has been isolated and identified in suspect but normal-appearing stocks of adult brook trout (Salvelinus fontinalis), and thus a pattern for the epizootiology of the virus has been demonstrated. Virus titers as high as 106.5 ID50 were found in egg fluids from 7 of 12 fish tested. In contrast, egg homogenates contained much less virus; their maximum titer was 101.8 ID50. The presence of virus within the eggs, however, was not established. Viral neutralizing ability of serum from the same fish showed an inverse relationship to the presence of virus in “ovarian fluid.” The highest serum titers occurred in those fish from which little or no virus had been isolated.

","language":"English","publisher":"Elsevier","doi":"10.1016/0042-6822(63)90192-2","usgsCitation":"Wolf, K., Quimby, M.C., and Bradford, A., 1963, Egg-associated transmission of IPN virus of trouts: Virology, v. 21, no. 3, p. 317-321, https://doi.org/10.1016/0042-6822(63)90192-2.","productDescription":"5 p.","startPage":"317","endPage":"321","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":197568,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60f0a4","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319925,"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":319924,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradford, A.D.","contributorId":96799,"corporation":false,"usgs":true,"family":"Bradford","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":319926,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221093,"text":"70221093 - 1963 - Hydrologic bench marks to distinguish the effects of climate vs. man","interactions":[],"lastModifiedDate":"2021-06-01T19:42:25.484388","indexId":"70221093","displayToPublicDate":"1963-07-01T14:39:43","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic bench marks to distinguish the effects of climate vs. man","docAbstract":"

There is a vital need for hydrologic data representing various environments that are free from the effects of man's activities. Without such data hydrologists will be stymied in distinguishing hydrologic changes caused by man from those caused by climate. To provide this background information, the U. S. Geological Survey is planning a nationwide hydrologic bench‐mark program in which runoff, transport of sediment, precipitation, changes in vegetation, fluctuations in ground water, and other hydrologic events will be studied in locales unaffected by the works of man. The knowledge gained in operating these bench marks will be invaluable in statistical appraisals of hydrologic data wherein a part of the record is affected by man's activities.

","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01918.x","usgsCitation":"Wilson, H., 1963, Hydrologic bench marks to distinguish the effects of climate vs. man: Groundwater, v. 1, no. 3, p. 13-14, https://doi.org/10.1111/j.1745-6584.1963.tb01918.x.","productDescription":"2 p.","startPage":"13","endPage":"14","costCenters":[],"links":[{"id":386073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Wilson, H.D. Jr.","contributorId":51370,"corporation":false,"usgs":true,"family":"Wilson","given":"H.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":816734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221089,"text":"70221089 - 1963 - Saline ground water — A little used and unmapped resource","interactions":[],"lastModifiedDate":"2021-06-01T19:19:26.466115","indexId":"70221089","displayToPublicDate":"1963-07-01T14:16:32","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Saline ground water — A little used and unmapped resource","docAbstract":"

Vast quantities of saline ground water await new commercial uses and economical demineralization processes for recognition as a valuable resource. Saline ground water is more widely distributed than any other natural resource, occurring throughout the United States and in geologic formations ranging from the oldest to the youngest. The Coastal Plain has the greatest reserve of fresh water in the country, but at depths ranging from a few feet to about 3,500 feet most of the fresh‐water aquifers also contain large quantities of brackish water. Paleozoic formations in the east‐central United States have long been producers of saline water as commercial brines and in association with oil and gas. The volume of saline ground water perhaps exceeds the fresh ground‐water supply in the Great Plains Region. The greater part of the Western Mountain Region is generally deficient in fresh ground water; however, saline water is present in highly permeable deposits in numerous closed basins and along saline streams. In each of these major ground‐water regions small to very large amounts of saline water can be pumped from wells ranging from a few tens of feet to several thousand feet in depth. Knowledge of saline water distribution is general and inadequate, having been attained as a by‐product of investigations of fresh‐water supplies. This knowledge should be expanded as technological advances in demineralization processes enhance the importance of saline water for potential supply in numerous water‐deficient areas. 

","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01921.x","usgsCitation":"Poole, J.L., 1963, Saline ground water — A little used and unmapped resource: Groundwater, v. 1, no. 3, p. 18-20, https://doi.org/10.1111/j.1745-6584.1963.tb01921.x.","productDescription":"3 p.","startPage":"18","endPage":"20","costCenters":[],"links":[{"id":386068,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Poole, J. L.","contributorId":40583,"corporation":false,"usgs":true,"family":"Poole","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221087,"text":"70221087 - 1963 - Gibson peak pluton: A discordant composite intrusion in the southeastern Trinity Alps, northern California","interactions":[],"lastModifiedDate":"2021-06-01T19:12:37.423082","indexId":"70221087","displayToPublicDate":"1963-07-01T14:08:26","publicationYear":"1963","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":"Gibson peak pluton: A discordant composite intrusion in the southeastern Trinity Alps, northern California","docAbstract":"

Gibson Peak pluton is the most discordant of several dominantly granitic intrusions in the Trinity Alps of northern California. It formed during Nevadan (Late Jurassic) deformation by emplacement of at least five discrete rock units that define a successively more silicic series, ranging from hypersthene gabbro to trondhjemitic tonalite. Contact features suggest that several units were incompletely crystalline when intruded by succeeding phases. Deformation of wall rocks, mainly partly serpentinized peridotite, indicates forceful intrusion, despite remarkable discordance of the pluton to regional structures. The discordance probably was controlled by regional extension fracturing during late stages of Nevadan deformation. Chemical compositions, computed from average modes of the intrusive units, are characterized by high Fe2O3-FeO and Na2O-K2O ratios. Plots of normative feldspar define a trend of trondhjemitic differentiation that diverges markedly from typical calc-alkaline trends. Contact metamorphism to mineral assemblages of pyroxene hornfels facies has been largely obscured by later low-grade hydration reactions, resulting in a net increase in serpentinization of most country-rock peridotite within the contact aureole.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1259:GPPADC]2.0.CO;2","usgsCitation":"Lipman, P.W., 1963, Gibson peak pluton: A discordant composite intrusion in the southeastern Trinity Alps, northern California: Geological Society of America Bulletin, v. 74, no. 10, p. 1259-1280, https://doi.org/10.1130/0016-7606(1963)74[1259:GPPADC]2.0.CO;2.","productDescription":"22 p.","startPage":"1259","endPage":"1280","costCenters":[],"links":[{"id":386061,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"northern California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.98046874999999,\n 38.73694606567598\n ],\n [\n -119.79492187499997,\n 38.73694606567598\n ],\n [\n -119.79492187499997,\n 42.00032514831618\n ],\n [\n -124.98046874999999,\n 42.00032514831618\n ],\n [\n -124.98046874999999,\n 38.73694606567598\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lipman, Peter W. 0000-0001-9175-6118","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":203612,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":816719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221085,"text":"70221085 - 1963 - Composite dike of andesite and rhyolite at Klondyke, Arizona","interactions":[],"lastModifiedDate":"2021-06-01T19:01:24.681121","indexId":"70221085","displayToPublicDate":"1963-07-01T13:55:24","publicationYear":"1963","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":"Composite dike of andesite and rhyolite at Klondyke, Arizona","docAbstract":"

A composite dike of probable Tertiary age intrudes Precambrian granodiorite 6 miles north of Klondyke, Arizona. The dike is exposed discontinuously for about 1500 feet along the strike and has a core of porphyritic rhyolite 15-20 feet thick flanked by coarsely porphyritic andesite 1-2 feet thick. Field evidence indicates that the rhyolite is later than the andesite but that the core of the original andesite dike was still hot and unconsolidated at the time of intrusion of the rhyolite. Chemically, the rhyolite is nearly identical to a large alkali granite pluton of Tertiary age exposed 1 mile east. The andesite component is similar both petrographically and chemically to lavas exposed in the region, but a direct relationship could not be established. Meager evidence suggests that the two dike components were derived from separate magma bodies rather than being differentiates of a single magma.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1049:CDOAAR]2.0.CO;2","usgsCitation":"Simons, F.S., 1963, Composite dike of andesite and rhyolite at Klondyke, Arizona: Geological Society of America Bulletin, v. 74, no. 8, p. 1049-1056, https://doi.org/10.1130/0016-7606(1963)74[1049:CDOAAR]2.0.CO;2.","productDescription":"8 p.","startPage":"1049","endPage":"1056","costCenters":[],"links":[{"id":386059,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Klondyke area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.61035156249999,\n 32.967195229355916\n ],\n [\n -110.2642822265625,\n 32.967195229355916\n ],\n [\n -110.2642822265625,\n 33.119150226768866\n ],\n [\n -110.61035156249999,\n 33.119150226768866\n ],\n [\n -110.61035156249999,\n 32.967195229355916\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Simons, Frank S.","contributorId":42203,"corporation":false,"usgs":true,"family":"Simons","given":"Frank","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":816714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221084,"text":"70221084 - 1963 - Some aspects of chemical equilibrium in ground water","interactions":[],"lastModifiedDate":"2021-06-01T18:51:47.135535","indexId":"70221084","displayToPublicDate":"1963-07-01T13:48:46","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Some aspects of chemical equilibrium in ground water","docAbstract":"

The influence of individual factors such as geologic and hydrologic characteristics of environment, biologic activity in soil, and pollutants on ground‐water composition is discussed. Aspects of chemical equilibria in ground water, sorption reactions, carbonate equilibria, chemistry of iron, and factors altering equilibria are presented.

","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01924.x","usgsCitation":"Hem, J., 1963, Some aspects of chemical equilibrium in ground water: Groundwater, v. 1, no. 3, p. 30-34, https://doi.org/10.1111/j.1745-6584.1963.tb01924.x.","productDescription":"5 p.","startPage":"30","endPage":"34","costCenters":[],"links":[{"id":386058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":816713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214095,"text":"70214095 - 1963 - Age of the Tordal, Norway pegmatite-A correction","interactions":[],"lastModifiedDate":"2020-09-22T16:24:45.527675","indexId":"70214095","displayToPublicDate":"1963-07-01T11:17:22","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Age of the Tordal, Norway pegmatite-A correction","docAbstract":"

No abstract available.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90047-4","usgsCitation":"Kulp, J.L., Kologrivov, R., Engels, J., Catanzaro, E.J., Neumann, H., and Nilssen, B., 1963, Age of the Tordal, Norway pegmatite-A correction: Geochimica et Cosmochimica Acta, v. 27, p. 847-848, https://doi.org/10.1016/0016-7037(63)90047-4.","productDescription":"2 p.","startPage":"847","endPage":"848","costCenters":[],"links":[{"id":378674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Norway","city":"Tordal","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 8.693103790283203,\n 59.14028591588303\n ],\n [\n 8.872489929199219,\n 59.14028591588303\n ],\n [\n 8.872489929199219,\n 59.20318495348292\n ],\n [\n 8.693103790283203,\n 59.20318495348292\n ],\n [\n 8.693103790283203,\n 59.14028591588303\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"27","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kulp, J. L.","contributorId":104573,"corporation":false,"usgs":false,"family":"Kulp","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":799440,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kologrivov, R.","contributorId":241057,"corporation":false,"usgs":false,"family":"Kologrivov","given":"R.","email":"","affiliations":[],"preferred":false,"id":799441,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Engels, J.","contributorId":70152,"corporation":false,"usgs":true,"family":"Engels","given":"J.","affiliations":[],"preferred":false,"id":799442,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Catanzaro, E. 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The old surface that extends over a long north-striking belt in northern Chile probably reached the mature stage of erosion by middle Tertiary time. Low areas are mantled by the piedmont deposits of the pampa, and the higher parts exhibit rock decay, oxidation, leaching, and super-gene enrichment of sulfide mineral deposits as a result of deep weathering. The surface and its deposits are deeply eroded south of the main pampa by the Río Copiapó and its tributaries. Numerous ore deposits in the thick secondary zones have not been eroded, but ore deposits are few in the youthful valleys where the primary zones extend to the surface. 

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