{"pageNumber":"4463","pageRowStart":"111550","pageSize":"25","recordCount":184800,"records":[{"id":70015874,"text":"70015874 - 1990 - Genesis of the tabular-type vanadium-uranium deposits of the Henry Basin, Utah","interactions":[],"lastModifiedDate":"2020-01-14T12:48:25","indexId":"70015874","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","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":"Genesis of the tabular-type vanadium-uranium deposits of the Henry Basin, Utah","docAbstract":"Tabular-type vanadium-uranium deposits occur in fluvial sandstones of the Salt Wash Member of the Morrison Formation of Late Jurassic age The mineralized intervals and the weakly mineralized lateral extensions are bounded both above and below by zones rich in dolomite cement. Carbon isotope values of dolomite cements indicate that at least two sources of carbon existed. One source appears to be the same as that which formed the bedded carbonates in the evaporites in the Tidwell Member of the Morrison Formation stratigraphically below the mineralized interval. The second carbon source is typical of terrestrially deposited carbonates generally associated with meteoric water-dominated environments. Oxygen isotope values of these dolomites show the same trend of isotopically light values above the mineralized interval and isotopically heavier values in and below that interval; they indicate that two isotopically distinct fluids were involved in the mineralizing process. Some aspects of the origin of gangue and ore phases are explainable on the basis of processes which occurred solely within the saline fluid, but key aspects of ore genesis involved the interaction of the saline and meteoric waters. It is postulated that the solution interface migrated vertically within the stratigraphic section. -from Authors","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.85.2.215","issn":"03610128","usgsCitation":"Northrop, H.R., Goldhaber, M., Landis, G.P., Unruh, J., Reynolds, R.J., Campbell, J.A., Wanty, R.B., Grauch, R.I., Whitney, G., and Rye, R.O., 1990, Genesis of the tabular-type vanadium-uranium deposits of the Henry Basin, Utah: Economic Geology, v. 85, no. 2, p. 215-269, https://doi.org/10.2113/gsecongeo.85.2.215.","productDescription":"55 p.","startPage":"215","endPage":"269","numberOfPages":"55","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":223484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Henry Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.6815185546875,\n              37.278423856453706\n            ],\n            [\n              -109.64355468749999,\n              37.278423856453706\n            ],\n            [\n              -109.64355468749999,\n              39.23650795487107\n            ],\n            [\n              -111.6815185546875,\n              39.23650795487107\n            ],\n            [\n              -111.6815185546875,\n              37.278423856453706\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"85","issue":"2","noUsgsAuthors":false,"publicationDate":"1990-04-01","publicationStatus":"PW","scienceBaseUri":"505a155ee4b0c8380cd54da6","contributors":{"authors":[{"text":"Northrop, H. R.","contributorId":40735,"corporation":false,"usgs":true,"family":"Northrop","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":371974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":371975,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Landis, Gary P.","contributorId":72405,"corporation":false,"usgs":true,"family":"Landis","given":"Gary","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":779384,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Unruh, J.W.","contributorId":105756,"corporation":false,"usgs":true,"family":"Unruh","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":779385,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reynolds, Richard J. 0000-0001-5032-6613 rjreynol@usgs.gov","orcid":"https://orcid.org/0000-0001-5032-6613","contributorId":1082,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rjreynol@usgs.gov","middleInitial":"J.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":779386,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Campbell, John A.","contributorId":67089,"corporation":false,"usgs":true,"family":"Campbell","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":779387,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wanty, Richard B. 0000-0002-2063-6423 rwanty@usgs.gov","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":443,"corporation":false,"usgs":true,"family":"Wanty","given":"Richard","email":"rwanty@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":779388,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Grauch, Richard I. 0000-0002-1763-0813 rgrauch@usgs.gov","orcid":"https://orcid.org/0000-0002-1763-0813","contributorId":1193,"corporation":false,"usgs":true,"family":"Grauch","given":"Richard","email":"rgrauch@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":779389,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Whitney, Gene","contributorId":27049,"corporation":false,"usgs":true,"family":"Whitney","given":"Gene","email":"","affiliations":[],"preferred":false,"id":779390,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Rye, Robert O. rrye@usgs.gov","contributorId":1486,"corporation":false,"usgs":true,"family":"Rye","given":"Robert","email":"rrye@usgs.gov","middleInitial":"O.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":779391,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70015824,"text":"70015824 - 1990 - Geochemical hosts of solubilized radionuclides in uranium mill tailings","interactions":[],"lastModifiedDate":"2024-01-22T16:23:29.042822","indexId":"70015824","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1930,"text":"Hydrometallurgy","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical hosts of solubilized radionuclides in uranium mill tailings","docAbstract":"<p><span>The solubilization and subsequent resorption of radionuclides by ore components or by reaction products during the milling of uranium ores may have both economic and environmental consequences. Particle-size redistribution of radium during milling has been demonstrated by previous investigators; however, the identification of sorbing components in the tailings has received little experimental attention. In this study, uranium-bearing sandstone ore was milled, on a laboratory scale, with sulfuric acid. At regular intervals, filtrate from this suspension was placed in contact with mixtures of quartz sand and various potential sorbents which occur as gangue in uranium ores; the potential sorbents included clay minerals, iron and aluminum oxides, feldspar, fluorspar, barite, jarosite, coal, and volcanic glass. After equilibration, the quartz sand-sorbent mixtures were separated from the filtrate and radioassayed by gamma-spectrometry to determine the quantities of&nbsp;</span><sup>238</sup><span>U,&nbsp;</span><sup>230</sup><span>Th,&nbsp;</span><sup>226</sup><span>Ra, and&nbsp;</span><sup>210</sup><span>Pb sorbed, and the radon emanation coefficients. Sorption of&nbsp;</span><sup>238</sup><span>U was low in all cases, with maximal sorptions of 1–2% by the bentonite- and coal-bearing samples.&nbsp;</span><sup>230</sup><span>Th sorption also was generally less than 1%; maximal sorption here was observed in the fluorspar-bearing sample and appears to be associated with the formation of gypsum during milling.&nbsp;</span><sup>226</sup><span>Ra and&nbsp;</span><sup>210</sup><span>&nbsp;Pb generally showed higher sorption than the other nuclides - more than 60% of the&nbsp;</span><sup>26</sup><span>Ra solubilized from the ore was sorbed on the barite-bearing sample. The mechanism (s) for this sorption by a wide variety of substrates is not yet understood. Radon emanation coefficients of the samples ranged from about 5 to 30%, with the coal-bearing samples clearly demonstrating an emanating power higher than any of the other materials.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0304-386X(90)90099-N","issn":"0304386X","usgsCitation":"Landa, E.R., and Bush, C.A., 1990, Geochemical hosts of solubilized radionuclides in uranium mill tailings: Hydrometallurgy, v. 24, no. 3, p. 361-372, https://doi.org/10.1016/0304-386X(90)90099-N.","productDescription":"12 p.","startPage":"361","endPage":"372","numberOfPages":"12","costCenters":[],"links":[{"id":223482,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1641e4b0c8380cd550ed","contributors":{"authors":[{"text":"Landa, E. R.","contributorId":100002,"corporation":false,"usgs":true,"family":"Landa","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":371853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, C. A.","contributorId":43344,"corporation":false,"usgs":true,"family":"Bush","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":371852,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015745,"text":"70015745 - 1990 - Crystal chemistry of the natural vanadium bronzes","interactions":[],"lastModifiedDate":"2012-03-12T17:18:59","indexId":"70015745","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Crystal chemistry of the natural vanadium bronzes","docAbstract":"The crystal chemistry of the natural vanadium bronze minerals is reviewed on the basis of published information and new studies (mainly by X-ray powder-diffraction methods) using type material wherever possible. The known V bronze minerals are divided into three categories: 1) the hewettite group, 2) the straczekite group, 3) other structure types including navajoite, schubnelite, fervanite, shcherbinaite, bannermanite, and melanovanadite. All known structures associated with the fibrous V bronzes (fiber spacing 3.6 A??) can be considered as various lateral linkages (into sheets or networks) of only two types of polyvanadate chains: 1) a divanadate chain (V2O6)n consisting of alternating square pyramids, and 2) a tetravanadate chain (V4O12)n consisting of four highly condensed single octahedral chains. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0003004X","usgsCitation":"Evans, H.T., and Hughes, J., 1990, Crystal chemistry of the natural vanadium bronzes: American Mineralogist, v. 75, no. 5-6, p. 508-521.","startPage":"508","endPage":"521","numberOfPages":"14","costCenters":[],"links":[{"id":224005,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fcfae4b0c8380cd4e55d","contributors":{"authors":[{"text":"Evans, H. T. Jr.","contributorId":41859,"corporation":false,"usgs":true,"family":"Evans","given":"H.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":371670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, J.M.","contributorId":18911,"corporation":false,"usgs":true,"family":"Hughes","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":371669,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015810,"text":"70015810 - 1990 - The 1989 earthquake swarm beneath Mammoth Mountain, California: An initial look at the 4 May through 30 September activity","interactions":[],"lastModifiedDate":"2024-04-10T15:45:45.342772","indexId":"70015810","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"The 1989 earthquake swarm beneath Mammoth Mountain, California: An initial look at the 4 May through 30 September activity","docAbstract":"<p>Mammoth Mountain is a 50,000- to 200,000-year-old cumulovolcano standing on the southwestern rim of Long Valley in eastern California. On 4 May 1989, two M = 1 earthquakes beneath the south flank of the mountain marked the onset of a swarm that has continued for more than 6 months. In addition to its longevity, noteworthy aspects of this persistent swarm include (1) an exponential-like increase in the rate of activity through the first month; (2) a vertically oriented, planar distribution of hypocenters at depths between 6 and 9 km with a north-northeast strike (roughly perpendicular to the average T-axis orientation for the swarm earthquakes); (3) recurring spasmodic bursts (rapid-fire sequences of similar-sized earthquakes with overlapping coda) and occasional earthquakes with enhanced low-frequency energy; (4) a uniform temporal distribution of the four largest (M ≈ 3) events over the first 4 months of the swarm with a cumulative seismic moment for the entire sequence through 30 September corresponding to a single M ≈ 4 earthquake; (5) a b-value of 1.2; and (6) submicrostrain perturbations on the nearby borehole dilatometer, the first of which led the onset of swarm activity by more than 2 weeks. These aspects of the swarm, together with its location along the southern extension of the youthful Mono-Inyo volcanic chain, which last erupted 500 to 600 years ago, point to a magmatic source for the modest but persistent influx of strain energy into the crust beneath Mammoth Mountain.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0800020325","usgsCitation":"Hill, D., 1990, The 1989 earthquake swarm beneath Mammoth Mountain, California: An initial look at the 4 May through 30 September activity: Bulletin of the Seismological Society of America, v. 80, no. 2, p. 325-339, https://doi.org/10.1785/BSSA0800020325.","productDescription":"15 p.","startPage":"325","endPage":"339","numberOfPages":"15","costCenters":[],"links":[{"id":223281,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"80","issue":"2","noUsgsAuthors":false,"publicationDate":"1990-04-01","publicationStatus":"PW","scienceBaseUri":"505ba62de4b08c986b320f40","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":371827,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015729,"text":"70015729 - 1990 - What killed the dinosaurs?","interactions":[],"lastModifiedDate":"2012-03-12T17:19:00","indexId":"70015729","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":743,"text":"American Scientist","active":true,"publicationSubtype":{"id":10}},"title":"What killed the dinosaurs?","docAbstract":"Out of a number of earlier attempts to explain mass extinctions, only the volcanism alternative to the impact hypothesis remains under serious consideration. The evidence for an impact is reviewed, and the mechanisms which might have brought about the apocalyptic series of extinctions at the Cretaceous-Tertiary (K-T) boundary are reviewed, referring to Alvarez's and other research teams working on the problem. As suggested by the patterns of extinctions and the periodicity of this and other mass extinctions, the \"volcanist alternative' is introduced. This would produce a series of selective extinctions spread over a considerable length of time, and which is similar to what the fossil record shows, and could account for the iridium anomaly at the K-T boundary. More support for this theory comes from models put forward by volcanist exponents, but it is concluded that the debate is far from ended. -J.W.Cooper","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Scientist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00030996","usgsCitation":"Glen, W., 1990, What killed the dinosaurs?: American Scientist, v. 78, no. 4, p. 354-370.","startPage":"354","endPage":"370","numberOfPages":"17","costCenters":[],"links":[{"id":223836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd041e4b08c986b32ed5c","contributors":{"authors":[{"text":"Glen, W.","contributorId":52728,"corporation":false,"usgs":true,"family":"Glen","given":"W.","email":"","affiliations":[],"preferred":false,"id":371635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015928,"text":"70015928 - 1990 - Radium distribution and indoor radon in the Pacific Northwest","interactions":[],"lastModifiedDate":"2024-02-13T01:13:17.237124","indexId":"70015928","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Radium distribution and indoor radon in the Pacific Northwest","docAbstract":"<div class=\"\"><div class=\"article-section__content en main\"><p>Aerial gamma-ray data were compiled to produce a map showing the distribution of radium (<sup>226</sup>Ra) in near-surface materials in the Pacific Northwest (Washington, Oregon, and Idaho, and parts of Montana, Wyoming, California, Nevada, and Utah). A comparison of measurements of indoor concentration levels of radon (<sup>222</sup>Rn) in homes with the apparent surface concentration of radium shows that aerial gamma-ray data provide a first order estimate of the relative amounts of indoor radon for township-sized areas where soils have low to moderate permeability. Townships with average indoor radon levels above the general trend of the data are almost all characterized by soils that have higher intrinsic permeabilities.</p></div></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/GL017i006p00801","issn":"00948276","usgsCitation":"Duval, J.S., and Otton, J.K., 1990, Radium distribution and indoor radon in the Pacific Northwest: Geophysical Research Letters, v. 17, no. 6, p. 801-804, https://doi.org/10.1029/GL017i006p00801.","productDescription":"4 p.","startPage":"801","endPage":"804","numberOfPages":"4","costCenters":[],"links":[{"id":223438,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","scienceBaseUri":"505a942ce4b0c8380cd81245","contributors":{"authors":[{"text":"Duval, J. S.","contributorId":15200,"corporation":false,"usgs":true,"family":"Duval","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":372100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Otton, J. K.","contributorId":52589,"corporation":false,"usgs":true,"family":"Otton","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":372101,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015814,"text":"70015814 - 1990 - Double-diffusive convection in geothermal systems: the Salton Sea, California, geothermal system as a likely candidate","interactions":[],"lastModifiedDate":"2024-04-19T18:53:38.843622","indexId":"70015814","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"Double-diffusive convection in geothermal systems: the Salton Sea, California, geothermal system as a likely candidate","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Much has been published about double-diffusive convection as a mechanism for explaining variations in composition and temperature within all-liquid natural systems. However, relatively little is known about the applicability of this phenomenon within the heterogeneous rocks of currently active geothermal systems where primary porosity may control fluid flow in some places and fractures may control it in others. The main appeal of double-diffusive convection within hydrothermal systems is-that it is a mechanism that may allow efficient transfer of heat mainly by convection, while at the same time maintaining vertical and lateral salinity gradients.</p><p>The Salton Sea geothermal system exhibits the following reservoir characteristics: (1) decreasing salinity and temperature from bottom to top and center toward the sides, (2) a very high heat flow from the top of the system that seems to require a major component of convective transfer of heat within the chemically stratified main reservoir, and (3) a relatively uniform density of the reservoir fluid throughout the system at all combinations of subsurface temperature, pressure, and salinity. Double-diffusive convection can account for these characteristics very nicely whereas other previously suggested models appear to account either for the thermal structure or for the salinity variations, but not both. Hydrologists, reservoir engineers, and particularly geochemists should consider the possibility and consequences of double-diffusive convection when formulating models of hydrothermal processes, and of the response of reservoirs to testing and production.</p></div></div></div></div><div id=\"preview-section-introduction\"><br></div><div id=\"preview-section-snippets\"><br></div><div id=\"preview-section-references\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(90)90001-R","issn":"03756505","usgsCitation":"Fournier, R., 1990, Double-diffusive convection in geothermal systems: the Salton Sea, California, geothermal system as a likely candidate: Geothermics, v. 19, no. 6, p. 481-496, https://doi.org/10.1016/0375-6505(90)90001-R.","productDescription":"16 p.","startPage":"481","endPage":"496","numberOfPages":"16","costCenters":[],"links":[{"id":223382,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a03ade4b0c8380cd505d9","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":371836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015929,"text":"70015929 - 1990 - Fluid-inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectance geothermometer","interactions":[],"lastModifiedDate":"2024-01-24T01:23:10.162313","indexId":"70015929","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Fluid-inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectance geothermometer","docAbstract":"<p>Theory, laboratory experiments, and empirical observation suggest that many aqueous fluid inclusions in calcite reequilibrate during overheating, and therefore some homogenization temperatures (<i>T</i><sub>h</sub>) record a temperature close to the maximum reached by the rock. This characteristic suggests that aqueous fluid inclusions in calcite can be used to establish maximum temperature (<i>T</i><sub>peak</sub>). To test this hypothesis, we have compiled fluid inclusion<span>&nbsp;</span><i>T</i><sub>peak</sub>, mean random vitrinite reflectance (<i>R</i><sub>m</sub>), and present-day<span>&nbsp;</span><i>T</i><sub>peak</sub><span>&nbsp;</span>from 46 diverse geologic systems that have been at<span>&nbsp;</span><i>T</i><sub>peak</sub><span>&nbsp;</span>from 10<sup>4</sup><span>&nbsp;</span>to 10<sup>6</sup><span>&nbsp;</span>yr. Present<span>&nbsp;</span><i>T</i><sub>peak</sub><span>&nbsp;</span>ranged from 65 to 345 °C,<span>&nbsp;</span><i>T</i><sub>h</sub><span>&nbsp;</span>modes and means ranged from 59 to 350 °C, and<span>&nbsp;</span><i>R</i><sub>m</sub><span>&nbsp;</span>data ranged from 0.4% to 4.6%, spanning the temperature and thermal maturity range associated with burial diagenesis, hydrothermal alteration, and low-grade metamorphism.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1990)018<1003:FITFDM>2.3.CO;2","issn":"00917613","usgsCitation":"Barker, C., and Goldstein, R., 1990, Fluid-inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectance geothermometer: Geology, v. 18, no. 10, p. 1003-1006, https://doi.org/10.1130/0091-7613(1990)018<1003:FITFDM>2.3.CO;2.","productDescription":"4 p.","startPage":"1003","endPage":"1006","numberOfPages":"4","costCenters":[],"links":[{"id":223439,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a127be4b0c8380cd54317","contributors":{"authors":[{"text":"Barker, C.E.","contributorId":69991,"corporation":false,"usgs":true,"family":"Barker","given":"C.E.","affiliations":[],"preferred":false,"id":372103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldstein, R.H.","contributorId":18908,"corporation":false,"usgs":true,"family":"Goldstein","given":"R.H.","affiliations":[],"preferred":false,"id":372102,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015734,"text":"70015734 - 1990 - Late Cenozoic volcanism, subduction, and extension in the Lassen region of California, southern Cascade Range","interactions":[],"lastModifiedDate":"2024-05-29T16:19:09.532394","indexId":"70015734","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Late Cenozoic volcanism, subduction, and extension in the Lassen region of California, southern Cascade Range","docAbstract":"Some 537 volcanic vents younger than 7 Ma are identified and these are classified into five age intervals and five compositional categories based on SiO2 content. Maps of vents by age and composition illustrate regionally representative volcanic trends. By 2 Ma, the eastern limit of volcanism had contracted westward toward the late Quaternary arc. Late Quaternary volcanism is concentrated around and north of the silicic Lassen volcanic center. The belt of most recent volcanism (25-0 ka) has been active since at least 2 Ma. Most mafic volcanism is calcalkaline basalt and basaltic andesite. Normal faults and linear groups of vents are evidence of widespread crustal extension throughout most of the Lassen region. NNW orientation of maximum horizontal stress is indicated. The Lassen volcanic region is thought to occur above the subducting Gorda North plate but also within a broad zone of distributed extension that occurs in the North American lithosphere east and southeast of the present Cascadia subduction zone. The scarcity of volcanic rocks older than 7 Ma suggests that a more compressive lithospheric stress regime prior to the late Miocene extensional episode may have suppressed volcanism. -from Authors","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB095iB12p19453","issn":"01480227","usgsCitation":"Guffanti, M., Clynne, M., Smith, J., Muffler, L., and Bullen, T., 1990, Late Cenozoic volcanism, subduction, and extension in the Lassen region of California, southern Cascade Range: Journal of Geophysical Research Solid Earth, v. 95, no. B12, p. 19543-19464, https://doi.org/10.1029/JB095iB12p19453.","productDescription":"12 p.","startPage":"19543","endPage":"19464","costCenters":[],"links":[{"id":223897,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"95","issue":"B12","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a44d1e4b0c8380cd66de8","contributors":{"authors":[{"text":"Guffanti, M.","contributorId":75693,"corporation":false,"usgs":true,"family":"Guffanti","given":"M.","affiliations":[],"preferred":false,"id":371645,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clynne, M.A.","contributorId":90722,"corporation":false,"usgs":true,"family":"Clynne","given":"M.A.","affiliations":[],"preferred":false,"id":371647,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, James G.","contributorId":44534,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":371643,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Muffler, L.J.P.","contributorId":63383,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.P.","affiliations":[],"preferred":false,"id":371644,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bullen, T.D.","contributorId":79911,"corporation":false,"usgs":true,"family":"Bullen","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":371646,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70015727,"text":"70015727 - 1990 - Discontinuities in the shallow Martian crust at Lunae, Syria, and Sinai Plana","interactions":[],"lastModifiedDate":"2024-05-29T16:25:12.424398","indexId":"70015727","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Discontinuities in the shallow Martian crust at Lunae, Syria, and Sinai Plana","docAbstract":"<p><span>Detailed photoclinometric profiles across 125 erosional features and 141 grabens in the western equatorial region of Mars indicate the presence of three discontinuities within the shallow crust. Pits, troughs, and wall valleys (tributary canyons) within Noctis Labyrinthus and Valles Marineris and escarpments within the fretted terrain of Sacra Fossae and Kasei Valles show distinct erosional base levels at depths of 0.3–0.6 km, 1 km, and 2–3 km. The shallowest discontinuity corresponds to thickness estimates for the ridged plains unit in this region, and thus the discontinuity probably is the contact between a sequence of layered rock making up this unit and the underlying megaregolith. The 1-km discontinuity is reflected in the base levels of erosion of all the features studied, and it may correspond to the base of the proposed layer of ground ice. Model calculations using photoclinometric profiles of simple grabens (corrected for the effects of mass wasting) and the 60° dip of bounding faults (measured from the exposed traces of faults on trough walls) show that graben-bounding faults consistently intersect at the mechanical discontinuity at about 1 km depth. This discontinuity may represent an interface between ice-laden and dry regolith, ice-laden and water-laden regolith, or pristine and cemented regolith. A correlation between wall valley head depth and local thickness of the faulted layer suggests that the 1-km discontinuity also controlled the depth of the heads of sapping canyons. There is no apparent relation between the pit and trough depths and the local thickness of the faulted layer, which can be explained if pits and troughs developed by subsidence into underlying tension cracks that disrupted the 1-km discontinuity. The data do suggest, however, that erosion of shallow pits and troughs was influenced by the 1-km discontinuity. The third discontinuity, at a depth of 2–3 km, corresponds to the proposed base of the Martian megaregolith and is probably the interface between overlying, ejected breccia and in situ, fractured basement rocks.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB095iB09p14231","issn":"01480227","usgsCitation":"Davis, P.A., and Golombek, M., 1990, Discontinuities in the shallow Martian crust at Lunae, Syria, and Sinai Plana: Journal of Geophysical Research Solid Earth, v. 95, no. B9, p. 14231-14248, https://doi.org/10.1029/JB095iB09p14231.","productDescription":"18 p.","startPage":"14231","endPage":"14248","costCenters":[],"links":[{"id":223786,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"95","issue":"B9","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a01ebe4b0c8380cd4fdb7","contributors":{"authors":[{"text":"Davis, P. A.","contributorId":74021,"corporation":false,"usgs":true,"family":"Davis","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":371633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golombek, M.P.","contributorId":52696,"corporation":false,"usgs":true,"family":"Golombek","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":371632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015962,"text":"70015962 - 1990 - The Ninole Basalt - Implications for the structural evolution of Mauna Loa volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:18:46","indexId":"70015962","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"The Ninole Basalt - Implications for the structural evolution of Mauna Loa volcano, Hawaii","docAbstract":"Lava flows of the Ninole Basalt, the oldest rocks exposed on the south side of the island of Hawaii, provide age and compositional constraints on the evolution of Mauna Loa volcano and the southeastward age progression of Hawaiian volcanism. Although the tholeiitic Ninole Basalt differs from historic lavas of Mauna Loa volcano in most major-element contents (e.g., variably lower K, Na, Si; higher Al, Fe, Ti, Ca), REE and other relatively immobile minor elements are similar to historic and prehistoric Mauna Loa lavas, and the present major-element differences are mainly due to incipient weathering in the tropical environment. New K-Ar whole-rock ages, from relatively fresh roadcut samples, suggest that the age of the Ninole Basalt is approximately 0.1-0.2 Ma, although resolution is poor because of low contents of K and radiogenic Ar. Originally considered the remnants of a separate volcano, the Ninole Hills are here interpreted as faulted remnants of the old south flank of Mauna Loa. Deep canyons in the Ninole Hills, eroded after massive landslide failure of flanks of the southwest rift zone, have been preserved from burial by younger lava due to westward migration of the rift zone. Landslide-induced depressurization of the southwest rift zone may also have induced phreatomagmatic eruptions that could have deposited widespread Basaltic ash that overlies the Ninole Basalt. Subaerial presence of the Ninole Basalt documents that the southern part of Hawaii Island had grown to much of its present size above sea level by 0.1-0.2 Ma, and places significant limits on subsequent enlargement of the south flank of Mauna Loa. ?? 1990 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Volcanology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00680316","issn":"02588900","usgsCitation":"Lipman, P.W., Rhodes, J., and Dalrymple, G.B., 1990, The Ninole Basalt - Implications for the structural evolution of Mauna Loa volcano, Hawaii: Bulletin of Volcanology, v. 53, no. 1, p. 1-19, https://doi.org/10.1007/BF00680316.","startPage":"1","endPage":"19","numberOfPages":"19","costCenters":[],"links":[{"id":205353,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00680316"},{"id":223238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba850e4b08c986b321b43","contributors":{"authors":[{"text":"Lipman, P. W.","contributorId":93470,"corporation":false,"usgs":true,"family":"Lipman","given":"P.","middleInitial":"W.","affiliations":[],"preferred":false,"id":372195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rhodes, J.M.","contributorId":31110,"corporation":false,"usgs":true,"family":"Rhodes","given":"J.M.","affiliations":[],"preferred":false,"id":372194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. B.","contributorId":10407,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":372193,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015879,"text":"70015879 - 1990 - Alkaline igneous rocks of Magnet Cove, Arkansas: Mineralogy and geochemistry of syenites","interactions":[],"lastModifiedDate":"2013-02-22T20:31:36","indexId":"70015879","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2588,"text":"LITHOS","active":true,"publicationSubtype":{"id":10}},"title":"Alkaline igneous rocks of Magnet Cove, Arkansas: Mineralogy and geochemistry of syenites","docAbstract":"Syenites from the Magnet Cove alkaline igneous complex form a diverse mineralogical and geochemical suite. Compositional zoning in primary and late-stage minerals indicates complex, multi-stage crystallization and replacement histories. Residual magmatic fluids, rich in F, Cl, CO2 and H2O, reacted with primary minerals to form complex intergrowths of minerals such as rinkite, fluorite, V-bearing magnetite, F-bearing garnet and aegirine. Abundant sodalite and natrolite formed in pegmatitic segregations within nepheline syenite where Cl- and Na-rich fluids were trapped. During autometasomatism compatible elements such as Mn, Ti, V and Zr were redistributed on a local scale and concentrated in late-stage minerals. Early crystallization of apatite and perovskite controlled the compatible behavior of P and Ti, respectively. The formation of melanite garnet also affected the behaviour of Ti, as well as Zr, Hf and the heavy rare-earth elements. Pseudoleucite syenite and garnet-nepheline syenite differentiated along separate trends, but the two groups are related to the same parental magma by early fractionation of leucite, the presumed precursor of intergrowths of K-feldspar and nepheline. The Diamond Jo nepheline syenite group defines a different differentiation trend. Sphene-nepheline syenite, alkali syenite and several miscellaneous nepheline syenites do not consistently plot with the other syenite groups or each other on element and oxide variation diagrams, indicating that they were derived from still other parental syenite magmas. Mineral assemblages indicate that relatively high f{hook};O2, at or above the fayalite-magnetite-quartz buffer, prevailed throughout the crystallization history of the syenites. ?? 1990.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"LITHOS","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0024-4937(90)90041-X","issn":"00244937","usgsCitation":"Flohr, M., and Ross, M., 1990, Alkaline igneous rocks of Magnet Cove, Arkansas: Mineralogy and geochemistry of syenites: LITHOS, v. 26, no. 1-2, p. 67-98, https://doi.org/10.1016/0024-4937(90)90041-X.","startPage":"67","endPage":"98","numberOfPages":"32","costCenters":[],"links":[{"id":223538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267965,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0024-4937(90)90041-X"}],"volume":"26","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e967e4b0c8380cd48262","contributors":{"authors":[{"text":"Flohr, M.J.K.","contributorId":73753,"corporation":false,"usgs":true,"family":"Flohr","given":"M.J.K.","email":"","affiliations":[],"preferred":false,"id":371986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, M.","contributorId":8026,"corporation":false,"usgs":true,"family":"Ross","given":"M.","email":"","affiliations":[],"preferred":false,"id":371985,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015816,"text":"70015816 - 1990 - Hydrogeology of an ancient arid closed basin: Implications for tabular sandstone-hosted uranium deposits","interactions":[],"lastModifiedDate":"2024-01-24T01:28:11.268759","indexId":"70015816","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Hydrogeology of an ancient arid closed basin: Implications for tabular sandstone-hosted uranium deposits","docAbstract":"<div id=\"15572774\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Hydrogeologic modeling shows that tabular-type uranium deposits in the Grants uranium region of the San Juan basin, New Mexico, formed in zones of ascending and discharging regional ground-water flow. The association of either lacustrine mudstone or actively subsiding structures and uranium deposits can best be explained by the occurrence of lakes at topographic depressions where ground water having different sources and compositions is likely to converge, mix, and discharge. Ascending and discharging flow also explains the association of uranium deposits with underlying evaporites and suggests a brine interface. The simulations contradict previous suggestions that ground water moved downward in the mudflat.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1990)018<1099:HOAAAC>2.3.CO;2","issn":"00917613","usgsCitation":"Sanford, R., 1990, Hydrogeology of an ancient arid closed basin: Implications for tabular sandstone-hosted uranium deposits: Geology, v. 18, no. 11, p. 1099-1102, https://doi.org/10.1130/0091-7613(1990)018<1099:HOAAAC>2.3.CO;2.","productDescription":"4 p.","startPage":"1099","endPage":"1102","numberOfPages":"4","costCenters":[],"links":[{"id":223384,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3487e4b0c8380cd5f82a","contributors":{"authors":[{"text":"Sanford, R.F.","contributorId":38562,"corporation":false,"usgs":true,"family":"Sanford","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":371838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014882,"text":"1014882 - 1990 - Immunological discrimination of Atlantic striped bass stocks","interactions":[],"lastModifiedDate":"2016-01-15T11:31:09","indexId":"1014882","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Immunological discrimination of Atlantic striped bass stocks","docAbstract":"<p><span>Stocks of Atlantic striped bass&nbsp;</span><i>Morone saxatilis</i><span>&nbsp;that were assumed to be geographically isolated during spawning showed strong antigenic differences in blood serum albumin. A discriminant function was estimated from the immunologic responses of northern (Canadian and Hudson River) and southern (Chesapeake Bay and Roanoke River) stocks to two reference antisera. The function correctly classified 92% of the northern and 95% of the southern fish in the training set. Cross-validation revealed similar percentages of correct classification for fish that were of known origin but not used to estimate the discriminant function. Monte Carlo experiments were used to evaluate the ability of the discriminant function to predict the relative contribution of northern fish in samples of various size and stock composition. Averages of predicted proportions of northern fish in the samples agreed well with actual proportions. Coefficients of variation (100 &times; SD/mean) in the predicted proportions ranged from 1.5 to 36% for samples of 50&ndash;400 fish that contained at least 10% northern stock. In samples that contained only 2% northern stock, however, at least 1,600 fish were required to achieve similar levels of precision.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1990)119<0077:IDOASB>2.3.CO;2","usgsCitation":"Schill, W.B., and Dorazio, R., 1990, Immunological discrimination of Atlantic striped bass stocks: Transactions of the American Fisheries Society, v. 119, no. 1, p. 77-85, https://doi.org/10.1577/1548-8659(1990)119<0077:IDOASB>2.3.CO;2.","productDescription":"9 p.","startPage":"77","endPage":"85","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"119","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf46","contributors":{"authors":[{"text":"Schill, W. B.","contributorId":60146,"corporation":false,"usgs":true,"family":"Schill","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":321439,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorazio, R.M. 0000-0003-2663-0468","orcid":"https://orcid.org/0000-0003-2663-0468","contributorId":23475,"corporation":false,"usgs":true,"family":"Dorazio","given":"R.M.","affiliations":[],"preferred":false,"id":321438,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016156,"text":"70016156 - 1990 - Cold-front driven storm erosion and overwash in the central part of the Isles Dernieres, a Louisiana barrier-island arc","interactions":[],"lastModifiedDate":"2024-09-23T12:22:39.060085","indexId":"70016156","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Cold-front driven storm erosion and overwash in the central part of the Isles Dernieres, a Louisiana barrier-island arc","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><div class=\"u-margin-s-bottom\">Tropical and extratropical storms produce significant erosion on the barrier islands of Louisiana. Over the past 100 years, such storms have produced at least 2 km of northward beach-face retreat and the loss of 63% of the surface area of the Isles Dernieres, a low-lying barrier-island arc along the central Louisiana coast. Elevations on the islands within the arc are typically less than 2 m above mean sea level. The islands typically have a washover-flat topography with occasional, poorly developed, dune-terrace topography consisting of low-lying and broken dunes. The central part of the arc consists of salt-marsh deposits overlain by washover sands along the Gulf of Mexico shoreline. Sand thicknesses range from zero behind the beach, to less than 2 m under the berm crest, and back to zero in the first nearshore trough. The sand veneer is sufficiently thin that storms can strip all the sand from the beach face, exposing the underlying marsh deposits.</div><div class=\"u-margin-s-bottom\">The geomorphic changes produced by cold fronts, a type of extratropical storm that commonly affect the Isles Dernieres between late fall and early spring are described. Between August 1986 and September 1987, repeated surveys along eleven shore-normal transects that covered 400 m of shoreline revealed the timing and extent of cold-front-produced beach change along a typical section of the central Isles Dernieres. During the study period, the beach face retreated approximately 20 m during the cold-front season but did not rebuild during the subsequent summer. Because the volume of sand deposited on the backshore (5600 m<sup>3</sup>) was less than the volume of material lost from the beach face (19,200 m<sup>3</sup>), approximately 13,600 m<sup>3</sup><span>&nbsp;</span>of material disappeared. Assuming that underlying marsh deposits decrease in volume in direct proportion to the amount of beach-face retreat, an estimate of the mud loss during the study period is 14,000 m<sup>3</sup>. Thus, the decrease in volume along the profiles can be accounted for without removing any sand from the area, suggesting that a major effect of cold fronts is first to strip the sand from the beach face and then to erode the underlying marsh deposits. After being eroded, the mud is lost from the islands because currents transport it away from the islands.</div></div></div></div></div><div id=\"preview-section-introduction\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(90)90036-J","issn":"00253227","usgsCitation":"Dingler, J., and Reiss, T.E., 1990, Cold-front driven storm erosion and overwash in the central part of the Isles Dernieres, a Louisiana barrier-island arc: Marine Geology, v. 91, no. 3, p. 195-206, https://doi.org/10.1016/0025-3227(90)90036-J.","productDescription":"12 p.","startPage":"195","endPage":"206","numberOfPages":"12","costCenters":[],"links":[{"id":223046,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f7a7e4b0c8380cd4cc30","contributors":{"authors":[{"text":"Dingler, J.R.","contributorId":64247,"corporation":false,"usgs":true,"family":"Dingler","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":372691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiss, T. E.","contributorId":36940,"corporation":false,"usgs":true,"family":"Reiss","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":372690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015995,"text":"70015995 - 1990 - Geochemical evidence for Se mobilization by the weathering of pyritic shale, San Joaquin Valley, California, U.S.A.","interactions":[],"lastModifiedDate":"2023-03-06T13:14:39.575474","indexId":"70015995","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical evidence for Se mobilization by the weathering of pyritic shale, San Joaquin Valley, California, U.S.A.","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-gulliver text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id5\"><p>Acidic (pH 4) seeps issue from the weathered Upper Cretaceous-Paleocene marine sedimentary shales of the Moreno Formation in the semi-arid Coast Ranges of California. The chemistry of the acidic solutions is believed to be evidence of current reactions ultimately yielding hydrous sodium and magnesium sulfate salts, e.g. mirabilite and bloedite, from the oxidation of primary pyrite. The selenate form of Se is concentrated in these soluble salts, which act as temporary geological sinks. Theoretically, the open lattice structures of these hydrous minerals could incorporate the selenate (SeO<sub>4</sub><sup>−2</sup>) anion in the sulfate (SO<sub>4</sub><sup>−2</sup>) space. When coupled with a semi-arid to arid climate, fractional crystallization and evaporative concentration can occur creating a sodium-sulfate fluid that exceeds the U.S. Environmental Protection Agency limit of 1000 μg l<sup>−1</sup><span>&nbsp;</span>for a toxic Se waste. The oxidative alkaline conditions necessary to ensure the concentration of soluble selenate are provided in the accompanying marine sandstones of the Panoche and Lodo Formations and the eugeosynclinal Franciscan assemblage. Runoff and extensive mass wasting in the area reflect these processes and provide the mechanisms which transport Se to the farmlands of the west-central San Joaquin Valley. Subsurface drainage from these soils consequently transports Se to refuge areas in amounts elevated to cause a threat to wildlife.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(90)90066-E","issn":"08832927","usgsCitation":"Presser, T.S., and Swain, W.C., 1990, Geochemical evidence for Se mobilization by the weathering of pyritic shale, San Joaquin Valley, California, U.S.A.: Applied Geochemistry, v. 5, no. 5-6, p. 703-717, https://doi.org/10.1016/0883-2927(90)90066-E.","productDescription":"15 p","startPage":"703","endPage":"717","numberOfPages":"15","costCenters":[],"links":[{"id":223085,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.7017466323125,\n              40.5694611030122\n            ],\n            [\n              -122.17462673973856,\n              38.606272517653935\n            ],\n            [\n              -121.73536016259354,\n              37.429708159816826\n            ],\n            [\n              -119.71473390772617,\n              35.52252426806004\n            ],\n            [\n              -118.57264080714941,\n              35.45098974022697\n            ],\n            [\n              -118.30908086086218,\n              36.09250271779459\n            ],\n            [\n              -118.88012741115108,\n              36.93976778850208\n            ],\n            [\n              -120.4614870888729,\n              38.46883487093669\n            ],\n            [\n              -121.42787355859184,\n              39.49320079491261\n            ],\n            [\n              -121.6475068471641,\n              40.5694611030122\n            ],\n            [\n              -121.99892010888023,\n              41.10120922478529\n            ],\n            [\n              -122.52604000145416,\n              41.13430179469822\n            ],\n            [\n              -122.7017466323125,\n              40.5694611030122\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"5","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a162be4b0c8380cd55089","contributors":{"authors":[{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":372301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swain, W. C.","contributorId":36168,"corporation":false,"usgs":true,"family":"Swain","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":372300,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015873,"text":"70015873 - 1990 - The occurrence and distribution of trace metals in the Mississippi River and its tributaries","interactions":[],"lastModifiedDate":"2018-02-15T13:05:49","indexId":"70015873","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5331,"text":"Science of Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"The occurrence and distribution of trace metals in the Mississippi River and its tributaries","docAbstract":"Quantitative and semiquantitative analyses of dissolved trace metals are reported for designated sampling sites on the Mississippi River and its main tributaries utilizing depth-integrated and width-integrated sampling technology to collect statistically representative samples. Data are reported for three sampling periods, including: July-August 1987, November-December 1987, and May-June 1988. Concentrations of Al, As, Ba, Be, Cd, Co, Cr, Cu, Fe, Li, Mn, Mo, Pb, Sr, Tl, U, V, and Zn are reported quantitatively, with the remainder of the stable metals in the periodic table reported semiquantitatively. Correlations between As and V, Ba and U, Cu and Zn, Li and Ba, and Li and U are significant at the 99% confidence level for each of the sampling trips. Comparison of the results of this study for selected metals with other published data show generally good agreement for Cr, Cu, Fe, and Zn, moderate agreement for Mo, and poor agreement for Cd and V.","language":"English","publisher":"Elsevier ","doi":"10.1016/0048-9697(90)90251-O","issn":"00489697","usgsCitation":"Taylor, H.E., Garbarino, J., and Brinton, T., 1990, The occurrence and distribution of trace metals in the Mississippi River and its tributaries: Science of Total Environment, v. 97-98, p. 369-384, https://doi.org/10.1016/0048-9697(90)90251-O.","productDescription":"16 p.","startPage":"369","endPage":"384","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":205368,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0048-9697(90)90251-O"},{"id":223437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"97-98","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae35e4b08c986b323f54","contributors":{"authors":[{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":371971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garbarino, J.R.","contributorId":76326,"corporation":false,"usgs":true,"family":"Garbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":371972,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brinton, T.I.","contributorId":93922,"corporation":false,"usgs":true,"family":"Brinton","given":"T.I.","affiliations":[],"preferred":false,"id":371973,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015731,"text":"70015731 - 1990 - The magnetospheric disturbance ring current as a source for probing the deep earth electrical conductivity","interactions":[],"lastModifiedDate":"2012-03-12T17:19:00","indexId":"70015731","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3209,"text":"Pure and Applied Geophysics PAGEOPH","active":true,"publicationSubtype":{"id":10}},"title":"The magnetospheric disturbance ring current as a source for probing the deep earth electrical conductivity","docAbstract":"Two current rings have been observed in the equatorial plane of the earth at times of high geomagnetic activity. An eastward current exists between about 2 and 3.5 earth radii (Re) distant, and a larger, more variable companion current exists between about 4 and 9 Re. These current regions are loaded during geomagnetic substorms. They decay, almost exponentially, after the cessation of the particle influx that attends the solar wind disturbance. This review focuses upon characteristics needed for intelligent use of the ring current as a source for induction probing of the earth's mantle. Considerable difficulties are found with the assumption that Dst is a ring-current index. ?? 1990 Birkha??user Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics PAGEOPH","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Birkha??user-Verlag","doi":"10.1007/BF00878018","issn":"00334553","usgsCitation":"Campbell, W., 1990, The magnetospheric disturbance ring current as a source for probing the deep earth electrical conductivity: Pure and Applied Geophysics PAGEOPH, v. 134, no. 4, p. 541-557, https://doi.org/10.1007/BF00878018.","startPage":"541","endPage":"557","numberOfPages":"17","costCenters":[],"links":[{"id":205421,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00878018"},{"id":223838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505badb3e4b08c986b323d9b","contributors":{"authors":[{"text":"Campbell, W.H.","contributorId":30749,"corporation":false,"usgs":true,"family":"Campbell","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":371637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015922,"text":"70015922 - 1990 - Magmatic unrest at Long Valley Caldera, California, 1980-1990","interactions":[],"lastModifiedDate":"2012-03-12T17:18:45","indexId":"70015922","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1813,"text":"Geoscience Canada","active":true,"publicationSubtype":{"id":10}},"title":"Magmatic unrest at Long Valley Caldera, California, 1980-1990","docAbstract":"On May 25, 1980, the resort town of Mammoth Lakes, California, was shaken by a remarkable 48-hour-long earthquake sequence that included four M=6, two M=5 and 300 M=3 quakes. The nature of the precursory seismicity plus the unusual character of the May 25-27 sequence itself suggested that it was not typical of tectonic earthquakes in the region. Discovery of 25 cm of domical uplift centred on the resurgent dome within Long Valley caldera strongly implied that this activity was accompanied, if not caused, by influex of magma into the Long Valley magma chamber. -Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geoscience Canada","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03150941","usgsCitation":"Bailey, R., and Hill, D., 1990, Magmatic unrest at Long Valley Caldera, California, 1980-1990: Geoscience Canada, v. 17, no. 3, p. 175-179.","startPage":"175","endPage":"179","numberOfPages":"5","costCenters":[],"links":[{"id":223340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4b4fe4b0c8380cd6944b","contributors":{"authors":[{"text":"Bailey, R. A.","contributorId":87531,"corporation":false,"usgs":true,"family":"Bailey","given":"R. A.","affiliations":[],"preferred":false,"id":372083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":372082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043725,"text":"70043725 - 1990 - Publications of the U.S. Geological Survey, 1989","interactions":[],"lastModifiedDate":"2013-05-23T10:12:03","indexId":"70043725","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":378,"text":"Publications of the US Geological Survey","active":false,"publicationSubtype":{"id":6}},"title":"Publications of the U.S. Geological Survey, 1989","docAbstract":"This catalog is a list of (1) books and maps that were published during 1989, and (2) articles by Geological Survey personnel in non-Geological Survey journals and books that came to our attention in 1989; it supplements the permanent catalogs \"Publications of the Geological Survey, 1879-1961\", \"Publications of the Geological Survey; 1962-1970\", and ''Publications of the U.S. Geological Survey, 1971 through 1981.\"","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70043725","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, Publications of the U.S. Geological Survey, 1989: Publications of the US Geological Survey, iv, 399 p., https://doi.org/10.3133/70043725.","productDescription":"iv, 399 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":272671,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043725/report.pdf"},{"id":267711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70043725/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad66e4b0b6328103b507","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006700,"text":"70006700 - 1990 - Study indicates feather meal can be a good supplement in trout diets","interactions":[],"lastModifiedDate":"2013-02-20T08:54:41","indexId":"70006700","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3712,"text":"Water Farming Journal","active":true,"publicationSubtype":{"id":10}},"title":"Study indicates feather meal can be a good supplement in trout diets","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Farming Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"C.T. and A. Inc.","collaboration":"None","usgsCitation":"Hughes, S., 1990, Study indicates feather meal can be a good supplement in trout diets: Water Farming Journal, v. 5, no. 8, p. 16-16.","startPage":"16","endPage":"16","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":260242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ccfe4b08c986b31d4cc","contributors":{"authors":[{"text":"Hughes, S.","contributorId":10384,"corporation":false,"usgs":true,"family":"Hughes","given":"S.","affiliations":[],"preferred":false,"id":355041,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016049,"text":"70016049 - 1990 - Activators of photoluminescence in calcite: evidence from high-resolution, laser-excited luminescence spectroscopy","interactions":[],"lastModifiedDate":"2013-01-20T20:41:14","indexId":"70016049","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Activators of photoluminescence in calcite: evidence from high-resolution, laser-excited luminescence spectroscopy","docAbstract":"Laser-excited luminescence spectroscopy of a red-algal, biogenic calcite and a synthetic Mn-calcite can make the distinction between organic and trace-element activators of photoluminescence. Organic-activated photoluminescence in biogenic calcite is characterized by significant peak shifts and increasing intensity with shorter-wavelength excitation and by significant decreases in intensity after heating to ??? 400??C. In contrast, Mn-activated photoluminescence shows no peak shift, greatest intensity under green excitation and limited changes after heating. Examination of samples with a high-sensitivity spectrometer using several wavelengths of exciting light is necessary for identification of photoluminescence activators. ?? 1990.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(90)90112-K","issn":"00092541","usgsCitation":"Pedone, V., Cercone, K., and Burruss, R., 1990, Activators of photoluminescence in calcite: evidence from high-resolution, laser-excited luminescence spectroscopy: Chemical Geology, v. 88, no. 1-2, p. 183-190, https://doi.org/10.1016/0009-2541(90)90112-K.","startPage":"183","endPage":"190","numberOfPages":"8","costCenters":[],"links":[{"id":266080,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(90)90112-K"},{"id":223142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6a6e4b0c8380cd47570","contributors":{"authors":[{"text":"Pedone, V.A.","contributorId":35193,"corporation":false,"usgs":true,"family":"Pedone","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":372425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cercone, K.R.","contributorId":10677,"corporation":false,"usgs":true,"family":"Cercone","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":372424,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burruss, R.C. 0000-0001-6827-804X","orcid":"https://orcid.org/0000-0001-6827-804X","contributorId":99574,"corporation":false,"usgs":true,"family":"Burruss","given":"R.C.","affiliations":[],"preferred":false,"id":372426,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016323,"text":"70016323 - 1990 - Gas chromatographic separation of carbon dioxide and nitrous oxide for stable isotopic analysis of carbon dioxide","interactions":[],"lastModifiedDate":"2023-03-09T17:43:10.046757","indexId":"70016323","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","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":"Gas chromatographic separation of carbon dioxide and nitrous oxide for stable isotopic analysis of carbon dioxide","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac00208a014","usgsCitation":"Revesz, K., and Coplen, T.B., 1990, Gas chromatographic separation of carbon dioxide and nitrous oxide for stable isotopic analysis of carbon dioxide: Analytical Chemistry, v. 62, no. 9, p. 972-973, https://doi.org/10.1021/ac00208a014.","productDescription":"2 p.","startPage":"972","endPage":"973","numberOfPages":"2","costCenters":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"links":[{"id":223564,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"62","issue":"9","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a14c5e4b0c8380cd54b5f","contributors":{"authors":[{"text":"Revesz, Kinga","contributorId":54308,"corporation":false,"usgs":true,"family":"Revesz","given":"Kinga","affiliations":[],"preferred":false,"id":373183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coplen, Tyler B. 0000-0003-4884-6008 tbcoplen@usgs.gov","orcid":"https://orcid.org/0000-0003-4884-6008","contributorId":508,"corporation":false,"usgs":true,"family":"Coplen","given":"Tyler","email":"tbcoplen@usgs.gov","middleInitial":"B.","affiliations":[{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":373182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043727,"text":"70043727 - 1990 - Publications of the U.S. Geological Survey, 1990","interactions":[],"lastModifiedDate":"2013-05-23T10:12:30","indexId":"70043727","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":378,"text":"Publications of the US Geological Survey","active":false,"publicationSubtype":{"id":6}},"title":"Publications of the U.S. Geological Survey, 1990","docAbstract":"This catalog is a list of (1) books and maps 1 that were published during 1990, and (2) articles by Geological Survey personnel in non-Geological Survey journals and books that came to our attention in 1990; it supplements the permanent catalogs \"Publications of the Geological Survey, 1879-1961\", \"Publications of the Geological Survey, 1962-1970\", and \"Publications of the U.S. Geological Survey, 1971 through 1981.\"","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70043727","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, Publications of the U.S. Geological Survey, 1990: Publications of the US Geological Survey, v, 445 p., https://doi.org/10.3133/70043727.","productDescription":"v, 445 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":272672,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043727/report.pdf"},{"id":267714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70043727/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad66e4b0b6328103b50b","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003143,"text":"1003143 - 1990 - Use of fish corrals in the seine fishery of the Virgin Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:04:11","indexId":"1003143","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2665,"text":"Marine Fisheries Review","active":true,"publicationSubtype":{"id":10}},"title":"Use of fish corrals in the seine fishery of the Virgin Islands","docAbstract":"Although selected aspects of the commercial fishery in the Virgin Islands have been documented since the  early 1930's, fish corrals and their use have not been described. This account, based on personal observations  made during 1985-86, summarizes commercial fishing methods in the Virgin Islands (U.S. and British),  documents the use of fish corrals, and serves as an introduction to the methodologies of this harvesting  technique. Interviews of commercial fishermen about how and when fish corrals are used provided information  not available from direct observation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Fisheries Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Jennings, C., 1990, Use of fish corrals in the seine fishery of the Virgin Islands: Marine Fisheries Review, v. 52, no. 3, p. 18-19.","productDescription":"pp. 18-19","startPage":"18","endPage":"19","numberOfPages":"2","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":129223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60472f","contributors":{"authors":[{"text":"Jennings, Cecil A.","contributorId":38504,"corporation":false,"usgs":true,"family":"Jennings","given":"Cecil A.","affiliations":[],"preferred":false,"id":312820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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