Surviving birds from nine duck plague outbreaks in urban and confined waterfowl were sampled for duck plague (DP) virus and DP antibody during 1979-86. Duck plague virus was found in combined oral and cloacal swabs of birds from three outbreaks, and DP-neutralizing antibody was demonstrated in some birds from all nine outbreaks. Greater prevalence of DP antibody and higher titers were found in survivors from confined populations than from free-flying urban populations. Free-flying waterfowl from within 52 km of four DP outbreak sites were also sampled; virus was not found in any birds, but DP antibody was found in urban waterfowl in the vicinity of an outbreak in Potterville, Michigan. No evidence of exposure to or shedding of DP virus in migratory waterfowl was found in two regions where DP appears enzootic in urban and confined waterfowl (Eastern Shore of Maryland and the vicinity of Sacramento, California).
","language":"English","publisher":"American Association of Avian Pathologists","doi":"10.2307/1590991","usgsCitation":"Brand, C.J., and Docherty, D.E., 1988, Post-epizootic surveys of waterfowl for duck plague (duck virus enteritis): Avian Diseases, v. 32, no. 4, p. 722-730, https://doi.org/10.2307/1590991.","productDescription":"9 p.","startPage":"722","endPage":"730","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":129544,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.241455078125,\n 43.74728909225906\n ],\n [\n -86.099853515625,\n 43.52465500687185\n ],\n [\n -83.16650390625,\n 43.27720532212024\n ],\n [\n -82.90283203125,\n 42.42345651793833\n ],\n [\n -83.111572265625,\n 41.795888098191426\n ],\n [\n -84.44091796875,\n 40.95501133048621\n ],\n [\n -84.6826171875,\n 39.740986355883564\n ],\n [\n -87.451171875,\n 39.49556336059472\n ],\n [\n -91.351318359375,\n 39.68182601089365\n ],\n [\n -91.636962890625,\n 40.3130432088809\n ],\n [\n -91.329345703125,\n 40.9052096972736\n ],\n [\n -91.19750976562499,\n 41.51680395810118\n ],\n [\n -90.703125,\n 41.672911819602085\n ],\n [\n -90.47241210937499,\n 41.94314874732696\n ],\n [\n -91.14257812499999,\n 42.64204079304428\n ],\n [\n -91.241455078125,\n 43.74728909225906\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"32","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ac4","contributors":{"authors":[{"text":"Brand, C. J.","contributorId":8788,"corporation":false,"usgs":true,"family":"Brand","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":314220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Docherty, D. E.","contributorId":83469,"corporation":false,"usgs":true,"family":"Docherty","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":314221,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1003181,"text":"1003181 - 1988 - Fish hosts for glochidia of the endangered freshwater mussel Lampsilis higginsi Lea (Bivalvia: Unionidae)","interactions":[],"lastModifiedDate":"2012-02-02T00:10:40","indexId":"1003181","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2649,"text":"Malacological Review","active":true,"publicationSubtype":{"id":10}},"title":"Fish hosts for glochidia of the endangered freshwater mussel Lampsilis higginsi Lea (Bivalvia: Unionidae)","docAbstract":"Laboratory tests of nine species of fish as hosts for glochidia of Lampsilis higginsi Lea indicated that four species were fully suitable: largemouth bass (Micropterus salmoides Lacepede), smallmouth bass (M. dolomieui Lacepede), walleye (Stizostedion vitreum vitreum Mitchill), and yellow perch (Perca flavescens Mitchill). Juvenile L. higginsi also developed on green sunfish (Lepomis cyanellus Rafinesque) but some fish sloughed their infections prematurely.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Malacological Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Waller, D.L., and Holland Bartels, L.E., 1988, Fish hosts for glochidia of the endangered freshwater mussel Lampsilis higginsi Lea (Bivalvia: Unionidae): Malacological Review, v. 21, no. 1-2, p. 119-122.","productDescription":"pp. 119-122","startPage":"119","endPage":"122","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":173241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6e7","contributors":{"authors":[{"text":"Waller, D. L.","contributorId":43704,"corporation":false,"usgs":true,"family":"Waller","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":312885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holland Bartels, L. E.","contributorId":71505,"corporation":false,"usgs":true,"family":"Holland Bartels","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":312886,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1003182,"text":"1003182 - 1988 - Morphology of glochidia of Lampsilis higginsi (Bivalvia: Unionidae) compared with three related species","interactions":[],"lastModifiedDate":"2012-02-02T00:15:44","indexId":"1003182","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":735,"text":"American Malacological Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Morphology of glochidia of Lampsilis higginsi (Bivalvia: Unionidae) compared with three related species","docAbstract":"Glochidia of the endangered unionid mussel Lampsilis higginsi (Lea) are morphologically similar to those of several other species in the upper Mississippi River. Life history details, such as the timing of reproduction and identity of host fish, can be readily studied if the glochidia of L. higginsi can be distinguished from those of related species. Authors used light and scanning electron microscopy and statistical analyses of three shell measurements, shell length, shell height, and hinge length, to compare the glochidia of L. higginsi with those of L. radiata siliquoidea (Barnes), L. ventricosa (Barnes), and Ligumia recta (Lamarck). Glochidia of L. higginsi were differentiated by scanning electron microscopy on the basis of a combined examination of the position of the hinge ligament and the width of dorsal ridges, but were indistinguishable by light microscope examination or by statistical analyses of measurements.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Malacological Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Waller, D.L., Holland Bartels, L.E., and Mitchell, L.G., 1988, Morphology of glochidia of Lampsilis higginsi (Bivalvia: Unionidae) compared with three related species: American Malacological Bulletin, v. 6, no. 1, p. 39-43.","productDescription":"pp. 39-43","startPage":"39","endPage":"43","numberOfPages":"5","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":199738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698f63","contributors":{"authors":[{"text":"Waller, D. L.","contributorId":43704,"corporation":false,"usgs":true,"family":"Waller","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":312887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holland Bartels, L. E.","contributorId":71505,"corporation":false,"usgs":true,"family":"Holland Bartels","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":312888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, L. G.","contributorId":102978,"corporation":false,"usgs":true,"family":"Mitchell","given":"L.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":312889,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1003144,"text":"1003144 - 1988 - Residues of benzocaine in rainbow trout, largemouth bass, and fish meal","interactions":[],"lastModifiedDate":"2025-07-29T15:31:58.759456","indexId":"1003144","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Residues of benzocaine in rainbow trout, largemouth bass, and fish meal","docAbstract":"Residues of the anesthetic benzocaine in muscle tissue of rainbow trout (Salmo gairdneri) and largemouth bass (Micropterus salmoides) were determined after exposure of the fish to 50 mg benzocaine/L for 15 min and withdrawal times of 0–24 h. The mean concentration of benzocaine residues in fish sampled immediately after exposure was 14.0 μg/g in rainbow trout and 10.6 μg/g in largemouth bass. Residues were below the control value after 8 h of withdrawal in largemouth bass and near the control value after 4 h of withdrawal in rainbow trout. Although residues of benzocaine were high in fish immediately after exposure, the concentration declined rapidly when the fish were held in flowing fresh water. Fish meal prepared from Pacific salmon (Oncorhynchus sp.) that had been anesthetized with benzocaine or trieaine (MS‐222) contained residues of 45.1 μg benzocaine/g or 47.7 μg trieaine/g.
","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8640(1988)050%3C0059:ROBIRT%3E2.3.CO;2","usgsCitation":"Allen, J.L., 1988, Residues of benzocaine in rainbow trout, largemouth bass, and fish meal: Progressive Fish-Culturist, v. 50, no. 1, p. 59-60, https://doi.org/10.1577/1548-8640(1988)050%3C0059:ROBIRT%3E2.3.CO;2.","productDescription":"2 p.","startPage":"59","endPage":"60","numberOfPages":"2","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":134461,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a814f","contributors":{"authors":[{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":312821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014160,"text":"70014160 - 1988 - Hydrodynamics of Denver basin: Explanation of subnormal fluid pressures","interactions":[],"lastModifiedDate":"2023-01-17T15:50:27.948092","indexId":"70014160","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Hydrodynamics of Denver basin: Explanation of subnormal fluid pressures","docAbstract":"Anomalously low fluid potential (and hence subnormal fluid pressure) is found in Mesozoic and Paleozoic rocks of the Denver basin. The potentiometric surface for the Dakota and basal Cretaceous sandstones is 2,000-3,000 ft (600-900 m) beneath the land surface in parts of the Denver basin in Colorado and Nebraska. The potentiometric surface for pre-Pennsylvanian carbonate rocks is 1,500 ft (450 m) lower than the potentiometric surface for the Dakota Sandstone in southeastern Colorado and western Kansas. The low fluid potential seems especially anomalous considering the high elevation of the outcrops along the Laramie and Front Ranges and the Black Hills.
A quasi-three-dimensional numerical flow model is used to investigate the regional flow system in the Denver basin and adjacent Mid-Continent. The model simulates flow through the entire Phanerozoic sedimentary column and indicates that subnormal pressures are a consequence of hydraulic insulation of the strata within the basin from their recharge zones as compared to their discharge zones. The Dakota Sandstone and underlying hydrostratigraphic units are insulated from the overlying water table by low-permeability shales of Cretaceous age, and from their own high-elevation outcrops by a zone of low permeability coincident with the basin deep. Subnormal pressures in the area of Denver, Colorado, and southward are further enhanced by faulting along the Front Range that isolates the stra a within the basin from their outcrops. The results of this study show that (1) subnormal fluid pressures can be explained as a consequence of steady-state regional ground-water flow, (2) shale is an important factor in the regional flow system, and (3) depth is an important control on the distribution of hydraulic conductivity.
","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/703C999C-1707-11D7-8645000102C1865D","usgsCitation":"Belitz, K., and Bredehoeft, J.D., 1988, Hydrodynamics of Denver basin: Explanation of subnormal fluid pressures: American Association of Petroleum Geologists Bulletin, v. 72, no. 11, p. 1334-1359, https://doi.org/10.1306/703C999C-1707-11D7-8645000102C1865D.","productDescription":"26 p.","startPage":"1334","endPage":"1359","numberOfPages":"26","costCenters":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"links":[{"id":226136,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Iowa, Kansas, Nebraska, South Dakota, Wyoming","otherGeospatial":"Denver basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -104.40130307963295,\n 37.43273547761615\n ],\n [\n -94.90669024004416,\n 37.278349382185866\n ],\n [\n -95.73123888547872,\n 43.12625436891602\n ],\n [\n -105.46272051147162,\n 43.243836203561045\n ],\n [\n -104.40130307963295,\n 37.43273547761615\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"72","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a333fe4b0c8380cd5ee62","contributors":{"authors":[{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":367748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bredehoeft, John D.","contributorId":86747,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":367749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014362,"text":"70014362 - 1988 - Origin of metaluminous and alkaline volcanic rocks of the Latir volcanic field, northern Rio Grande rift, New Mexico","interactions":[],"lastModifiedDate":"2012-03-12T17:19:28","indexId":"70014362","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of metaluminous and alkaline volcanic rocks of the Latir volcanic field, northern Rio Grande rift, New Mexico","docAbstract":"Volcanic rocks of the Latir volcanic field evolved in an open system by crystal fractionation, magma mixing, and crustal assimilation. Early high-SiO2 rhyolites (28.5 Ma) fractionated from intermediate compositionmagmas that did not reach the surface. Most precaldera lavas have intermediate-compositions, from olivine basaltic-andesite (53% SiO2) to quartz latite (67% SiO2). The precaldera intermediate-composition lavas have anomalously high Ni and MgO contents and reversely zoned hornblende and augite phenocrysts, indicating mixing between primitive basalts and fractionated magmas. Isotopic data indicate that all of the intermediate-composition rocks studied contain large crustal components, although xenocrysts are found only in one unit. Inception of alkaline magmatism (alkalic dacite to high-SiO2 peralkaline rhyolite) correlates with, initiation of regional extension approximately 26 Ma ago. The Questa caldera formed 26.5 Ma ago upon eruption of the >500 km3 high-SiO2 peralkaline Amalia Tuff. Phenocryst compositions preserved in the cogenetic peralkaline granite suggest that the Amalia Tuff magma initially formed from a trace element-enriched, high-alkali metaluminous magma; isotopic data suggest that the parental magmas contain a large crustal component. Degassing of water- and halogen-rich alkali basalts may have provided sufficient volatile transport of alkalis and other elements into the overlying silicic magma chamber to drive the Amalia Tuff magma to peralkaline compositions. Trace element variations within the Amalia Tuff itself may be explained solely by 75% crystal fractionation of the observed phenocrysts. Crystal settling, however, is inconsistent with mineralogical variations in the tuff, and crystallization is thought to have occurred at a level below that tapped by the eruption. Spatially associated Miocene (15-11 Ma) lavas did not assimilate large amounts of crust or mix with primitive basaltic magmas. Both mixing and crustal assimilation processes appear to require development of relatively large magma chambers in the crust that are sustained by large basalt fluxes from the mantle. The lack of extensive crustal contamination and mixing in the Miocene lavas may be related to a decreased basalt flux or initiation of blockfaulting that prevented pooling of basaltic magma in the crust. ?? 1988 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00399442","issn":"00107999","usgsCitation":"Johnson, C., and Lipman, P.W., 1988, Origin of metaluminous and alkaline volcanic rocks of the Latir volcanic field, northern Rio Grande rift, New Mexico: Contributions to Mineralogy and Petrology, v. 100, no. 1, p. 107-128, https://doi.org/10.1007/BF00399442.","startPage":"107","endPage":"128","numberOfPages":"22","costCenters":[],"links":[{"id":205690,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00399442"},{"id":226218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"100","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a70e5e4b0c8380cd7630c","contributors":{"authors":[{"text":"Johnson, C.M.","contributorId":78707,"corporation":false,"usgs":true,"family":"Johnson","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":368218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lipman, P. W.","contributorId":93470,"corporation":false,"usgs":true,"family":"Lipman","given":"P.","middleInitial":"W.","affiliations":[],"preferred":false,"id":368219,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014426,"text":"70014426 - 1988 - Salton Sea Scientific Drilling Program","interactions":[],"lastModifiedDate":"2012-03-12T17:19:33","indexId":"70014426","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1437,"text":"Earthquakes & Volcanoes (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Salton Sea Scientific Drilling Program","docAbstract":"This article briefly describes the progress of drilling in the Salton Sea to depths exceeding 10 000 ft (3050 m) in the search for geothermal energy supplies. -A.Scarth","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquakes & Volcanoes (USGS)","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Sass, J., 1988, Salton Sea Scientific Drilling Program: Earthquakes & Volcanoes (USGS), v. 20, no. 4, p. 156-160.","startPage":"156","endPage":"160","numberOfPages":"5","costCenters":[],"links":[{"id":225314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ab038e4b0c8380cd879c5","contributors":{"authors":[{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":368374,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014161,"text":"70014161 - 1988 - Optical (diffuse reflectance) and Mossbauer spectroscopic study of nontronite and related Fe-bearing smectites","interactions":[],"lastModifiedDate":"2012-03-12T17:19:35","indexId":"70014161","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Optical (diffuse reflectance) and Mossbauer spectroscopic study of nontronite and related Fe-bearing smectites","docAbstract":"Near-ultraviolet to near-infrared optical (diffuse reflectance) spectra of several nontronites and related Fe-bearing smectites [(Fe2+,Fe3+)-bearing saponite and (Fe2+,Fe3+)-bearing montmorillonite] are presented and interpreted. Mossbauer spectra at 298 K are also presented to help interpret the optical spectra. The optical spectra of nontronites are dominated by the ligand field transitions of Fe3+ in octahedral coordination sites. In addition to the ligand field transitions of single Fe3+ cations, a broad absorption band centered near 22000 cm-1 is observed that may be due to the simultaneous excitation of two Fe3+ cations to the 4T1g (4G) state. Alternatively, this band may represent excitations to the 2A2g and 2T1g ligand field states. For most samples, the amount of tetrahedrally coordinated Fe3+ was below that detectable by Mossbauer spectroscopy (1-3% of total Fe). However, the optical spectra of all of the nontronites show an absorption band near 23000 cm-1. This band is assigned to the 6A1 ??? 4E,4A1 transition of tetrahedrally coordinated Fe3+. The optical spectra of mixed-valence Fe-bearing smectites show a broad absorption band at 14000-15000 cm-1 owing to Fe2+ ??? Fe3+ charge transfer. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0003004X","usgsCitation":"Sherman, D.M., and Vergo, N., 1988, Optical (diffuse reflectance) and Mossbauer spectroscopic study of nontronite and related Fe-bearing smectites: American Mineralogist, v. 73, no. 11-12, p. 1346-1354.","startPage":"1346","endPage":"1354","numberOfPages":"9","costCenters":[],"links":[{"id":226137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6ec5e4b0c8380cd757c6","contributors":{"authors":[{"text":"Sherman, David M.","contributorId":73218,"corporation":false,"usgs":true,"family":"Sherman","given":"David","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":367751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vergo, N.","contributorId":12627,"corporation":false,"usgs":true,"family":"Vergo","given":"N.","affiliations":[],"preferred":false,"id":367750,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66317,"text":"i1897H - 1988 - Hydraulic map of Crystal Rapids, Grand Canyon, Arizona","interactions":[],"lastModifiedDate":"2022-07-07T19:26:34.465163","indexId":"i1897H","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1897","chapter":"H","title":"Hydraulic map of Crystal Rapids, Grand Canyon, Arizona","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1897H","collaboration":"Prepared in cooperation with the Bureau of Reclamation and the National Park Service","usgsCitation":"Kieffer, S.W., 1988, Hydraulic map of Crystal Rapids, Grand Canyon, Arizona: U.S. Geological Survey IMAP 1897, 1 Plate: 56.76 × 38.28 inches, https://doi.org/10.3133/i1897H.","productDescription":"1 Plate: 56.76 × 38.28 inches","costCenters":[],"links":[{"id":187509,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1897h/plate-1-thumb.jpg"},{"id":91544,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1897h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400825,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9983.htm"}],"scale":"1000","country":"United States","state":"Arizona","otherGeospatial":"Crystal Rapids, Grand Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.2486,\n 36.1333\n ],\n [\n -112.2422,\n 36.1333\n ],\n [\n -112.2422,\n 36.1394\n ],\n [\n -112.2486,\n 36.1394\n ],\n [\n -112.2486,\n 36.1333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a25a","contributors":{"authors":[{"text":"Kieffer, Susan W.","contributorId":270732,"corporation":false,"usgs":false,"family":"Kieffer","given":"Susan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":274342,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70142175,"text":"70142175 - 1988 - Extracting topographic structure from digital elevation data for geographic information-system analysis","interactions":[],"lastModifiedDate":"2017-01-18T14:31:27","indexId":"70142175","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Extracting topographic structure from digital elevation data for geographic information-system analysis","docAbstract":"Software tools have been developed at the U.S. Geological Survey's EROS Data Center to extract topographic structure and to delineate watersheds and overland flow paths from digital elevation models. The tools are specialpurpose FORTRAN programs interfaced with general-purpose raster and vector spatial analysis and relational data base management packages.
\nThe first phase of analysis is a conditioning phase that generates three data sets: the original OEM with depressions filled, a data set indicating the flow direction for each cell, and a flow accumulation data set in which each cell receives a value equal to the total number of cells that drain to it. The original OEM and these three derivative data sets can then be processed in a variety of ways to optionally delineate drainage networks, overland paths, watersheds for userspecified locations, sub-watersheds for the major tributaries of a drainage network, or pour point linkages between watersheds. The computer-generated drainage lines and watershed polygons and the pour point linkage information can be transferred to vector-based geographic information systems for futher analysis. Comparisons between these computergenerated features and their manually delineated counterparts generally show close agreement, indicating that these software tools will save analyst time spent in manual interpretation and digitizing.
","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Jenson, S.K., and Domingue, J.O., 1988, Extracting topographic structure from digital elevation data for geographic information-system analysis: Photogrammetric Engineering and Remote Sensing, v. 54, no. 11, p. 1593-1600.","productDescription":"8 p.","startPage":"1593","endPage":"1600","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":298224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54f597cae4b02419550d2f45","contributors":{"authors":[{"text":"Jenson, Susan K.","contributorId":66859,"corporation":false,"usgs":true,"family":"Jenson","given":"Susan","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":541674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Domingue, Julia O.","contributorId":91832,"corporation":false,"usgs":true,"family":"Domingue","given":"Julia","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":541675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014433,"text":"70014433 - 1988 - Erosional furrows formed during the lateral blast at Mount St. Helens, May 18, 1980","interactions":[],"lastModifiedDate":"2024-06-05T15:06:32.142714","indexId":"70014433","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Erosional furrows formed during the lateral blast at Mount St. Helens, May 18, 1980","docAbstract":"Nearly horizontal, quasi-periodic erosional features of 7-m average transverse wavelength and of order 100-m length occur in scattered locations from 3.5 to 9 km from the crater at Mount St. Helens under deposits of the lateral blast of May 18, 1980. We attribute the erosional features to scouring by longitudinal vortices resulting from flow instabilities induced by complex topography, namely, by streamline curvature in regions of reattachment downstream of sheltered regions, and by the cross-flow component of flow subparallel to ridge crests. The diameter of the vortices and their transverse spacing, inferred from the distance between furrows, are taken to be of the order of the boundary layer thickness. The inferred boundary layer thickness (≈14 m at 9 km from the source of the blast) is consistent with the running length from the mountain to the furrow locations. By using knowledge of ablation patterns on bodies and lofting of dust in high-speed flow, we are able to infer some features of the flow field within the blast. Within the furrows the erosion rate was of the order of 9 kg m−2 s−1, about 4 times greater than that expected from laboratory data obtained in flow free of longitudinal vortices. The orientation of furrows induced by the cross-flow instability can be used to measure the upwash angle and estimate the flow Mach number: at the central ridge of Spirit Lake the Mach number is inferred to have been about 2.5, and the flow velocity approximately 235 m/s. The similarities and differences between the furrows reported here and channels observed at other volcanoes are discussed.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB093iB12p14793","issn":"01480227","usgsCitation":"Kieffer, S.W., and Sturtevant, B., 1988, Erosional furrows formed during the lateral blast at Mount St. Helens, May 18, 1980: Journal of Geophysical Research Solid Earth, v. 93, no. B12, p. 14793-14816, https://doi.org/10.1029/JB093iB12p14793.","productDescription":"24 p.","startPage":"14793","endPage":"14816","costCenters":[],"links":[{"id":480038,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1029/jb093ib12p14793","text":"External Repository"},{"id":225446,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"B12","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a0a42e4b0c8380cd5228f","contributors":{"authors":[{"text":"Kieffer, S. W.","contributorId":19186,"corporation":false,"usgs":true,"family":"Kieffer","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":368388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sturtevant, B.","contributorId":48318,"corporation":false,"usgs":true,"family":"Sturtevant","given":"B.","email":"","affiliations":[],"preferred":false,"id":368389,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70182154,"text":"70182154 - 1988 - Seasonal occurrence of migrant whimbrels and bristle-thighed curlews on the Yukon-Kuskokwim Delta, Alaska","interactions":[],"lastModifiedDate":"2017-02-17T09:29:29","indexId":"70182154","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal occurrence of migrant whimbrels and bristle-thighed curlews on the Yukon-Kuskokwim Delta, Alaska","docAbstract":"Migrant Whimbrels (Numenius phaeopus) and Bristle-thighed Curlews (N. tahitiensis) were recorded during five summers along coastal tundra of the Yukon-Kuskokwim Delta, Alaska. From June to September, 1975-1979, 358 flocks totalling 1,265 curlews were observed; an additional 54 flocks were identified by vocalization alone. Among the 359 flocks identified to species, 52% were of Whimbrels, 47% were of Bristle-thighed Curlews, and 1% were of both species. Flocks as large as 48 Whimbrels and 33 Bristle-thighed Curlews were recorded, but 87% of the flocks contained five or fewer birds. During 2 years with early springs a few Whimbrels and Bristle-thighed Curlews were recorded on the delta in early June; these may have been late spring migrants, oversummering nonbreeders, or very early failed breeders. Whimbrel numbers peaked twice each summer, first in middle to late July and again in late August. These peaks probably consisted mainly of late failed breeders and of successful breeders with juveniles, respectively. The patterns of occurrence of Bristle-thighed Curlews were more complex, with up to three peaks in abundance each season, probably consisting of the following populational subclasses: (1) early failed breeders from late June to mid-July, (2) late failed breeders in late July, and (3) successful breeders and juveniles in early August. Most Bristle-thighed Curlews were gone by mid-August and Whimbrels, by early September. For both species the earliest juveniles were seen in late July in flocks with adults. The Yukon-Kuskokwim Delta is conservatively estimated to support several thousands of both Whimbrels and Bristle-thighed Curlews. This area is considered to be particularly important for Bristle-thighed Curlews because it is the primary of only two known areas used during migration between their nesting grounds in Alaska and the first known stop on their wintering grounds in the Hawaiian Island chain, a transoceanic distance of 3,800 km. Whimbrels are more ubiquitous in their distribution and use of habitats, and their migration strategy may provide more flexibility in choice of timing and routes.
","language":"English","publisher":"Cooper Ornithological Society","doi":"10.2307/1368835","usgsCitation":"Handel, C.M., and Dau, C.P., 1988, Seasonal occurrence of migrant whimbrels and bristle-thighed curlews on the Yukon-Kuskokwim Delta, Alaska: The Condor, v. 90, no. 4, p. 782-790, https://doi.org/10.2307/1368835.","productDescription":"9 p.","startPage":"782","endPage":"790","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":335800,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Yukon-Kuskokwim Delta","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -168.50830078125,\n 59.57885104663186\n ],\n [\n -159.521484375,\n 59.57885104663186\n ],\n [\n -159.521484375,\n 63.869714622204825\n ],\n [\n -168.50830078125,\n 63.869714622204825\n ],\n [\n -168.50830078125,\n 59.57885104663186\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"90","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a819bae4b025c46429aff5","contributors":{"authors":[{"text":"Handel, Colleen M. 0000-0002-0267-7408 cmhandel@usgs.gov","orcid":"https://orcid.org/0000-0002-0267-7408","contributorId":3067,"corporation":false,"usgs":true,"family":"Handel","given":"Colleen","email":"cmhandel@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":669820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dau, Christian P.","contributorId":26185,"corporation":false,"usgs":true,"family":"Dau","given":"Christian","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":669821,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70197190,"text":"70197190 - 1988 - Integrating spatial and frequency information in the search for kuroko deposits of the Hokuroku District, Japan","interactions":[],"lastModifiedDate":"2018-05-21T15:39:46","indexId":"70197190","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Integrating spatial and frequency information in the search for kuroko deposits of the Hokuroku District, Japan","docAbstract":"A new method (FINDER) that uses the area of influence and Bayesian statistics to aid in selection of target areas on the basis of one or more variables and multiple observations was tested with drill hole data. A previously defined bimodal distribution of Na 2 O with the low sodium group confined to a 1.5 X 3.0-km zone beneath the cluster of deposits at Fukazawa was used as a control area for one test of FINDER. Using the Na 2 O means and standard deviations for the control area and minimum Na 2 O values from 174 drill holes, a probability map of centers of sodium depletion is produced for the Hokuroku district. High probability areas correspond to the known deposits that should have been rediscovered and to several areas without known deposits.Use of X-ray data from 165 drill holes, some of which also have chemical analyses, led to the identification of two additional variables, sericite and gypsum plus anhydrite, that allow more drill holes to be used and that expand the areas of influence around drill holes. Sericite is enriched up to 2.15 km and gypsum plus anhydrite up to 3.5 km from the centroid of the control area Fukazawa deposits. For the deposit groups with X-ray data nearby, Fukazawa, Shakanai, and Furutobe, a pattern of sericite enrichment, kuroko deposits, and gypsum plus anhydrite enrichment over 4 or 5 km is shown.With sodium, sericite, and gypsum plus anhydrite, FINDER's high probability areas include each of the four groups of kuroko deposits that should have been rediscovered and only one known deposit that is much smaller than Fukazawa is missed. Several large areas that are favorable centers of undiscovered deposits and other areas that are unlikely centers of deposits are also identified.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.83.1.18","usgsCitation":"Singer, D.A., and Kouda, R., 1988, Integrating spatial and frequency information in the search for kuroko deposits of the Hokuroku District, Japan: Economic Geology, v. 83, no. 1, p. 18-29, https://doi.org/10.2113/gsecongeo.83.1.18.","productDescription":"12 p.","startPage":"18","endPage":"29","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Hokuroku District","volume":"83","issue":"1","noUsgsAuthors":false,"publicationDate":"1988-02-01","publicationStatus":"PW","scienceBaseUri":"5b15af92e4b092d9651e2332","contributors":{"authors":[{"text":"Singer, Donald A. dsinger@usgs.gov","contributorId":5601,"corporation":false,"usgs":true,"family":"Singer","given":"Donald","email":"dsinger@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":735954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kouda, Ryoichi","contributorId":198036,"corporation":false,"usgs":false,"family":"Kouda","given":"Ryoichi","email":"","affiliations":[],"preferred":false,"id":735955,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014428,"text":"70014428 - 1988 - Magmatic heat and the El Nino cycle","interactions":[],"lastModifiedDate":"2023-12-19T00:31:25.62698","indexId":"70014428","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Magmatic heat and the El Nino cycle","docAbstract":"Large submarine lava flows with apparent volumes exceeding 10 km3 have recently been imaged on the deep ocean floor in various parts of the Pacific by means of GLORIA and SeaMarc side-looking sonar surveys. Such flows may produce thermal anomalies large enough to perturb the cyclic processes of the ocean and could be a factor in the genesis of El Niño phenomena. We find that known volume rates of mid-ocean magma production could generate repetitive thermal anomalies as large as 10% of the average El Niño sea surface anomaly at intervals of about 5 years (the mean interval of El Niño events between 1935 and 1984). Likewise, estimated rates of eruption, cooling of lava on the seafloor, and transfer of heat to the near-surface environment could reasonably produce a thermal anomaly comparable to that associated with El Niño. Larger magmatic events, associated with fluctuations in the total magmatic power and seismicity along the East Pacific Rise, are possible at longer intervals and may explain the extreme size of some El Niño events, such as that of 1982–1983.
U.S. Geological Survey Newberry 2 was drilled to a depth of 932 m within Newberry caldera. The bottom-hole temperature of 265°C is the highest reported temperature of any drill hole in the Cascades region of the United States. The upper part of the stratigraphic section penetrated by Newberry 2 consists of caldera fill below which are increasingly more mafic lavas ranging from rhyodacite at 501 m to basalt at 932 m. Measured temperatures shallower than 300 m are less than 35°C, and rock alteration consists of hydration of glass and local palagonitization of basaltic tuffs. Incipient zeolitization and partial smectite replacement of ash and pumice occurred throughout the pumiceous lithic tuffs from 300 to 500 m. Higher-temperature alteration of the tuffs to chlorite and mordenite occurs adjacent to a rhyodacite sill at 460–470 m; alteration minerals within the sill consist of pyrrhotite, pyrite, quartz, calcite, and siderite. Below 697 m the rocks are progressively more altered with depth mainly because of increased temperature along a conductive gradient from 100°C at 697 m to 265°C at 930 m. Fluid inclusions in quartz and calcite indicate that temperatures in the past have been higher than at present, most likely due to local confining pressures between impermeable lava flows. Flow breccias are more altered than the adjacent dense massive lava flows, regardless of composition, because of their much higher permeability. Hydrothermal minerals in this zone are mainly mixed-layer chlorite-smectite, quartz, calcite, and pyrite. Chlorite becomes more abundant than mixed-layer clays near the bottom of the hole. In the lowest two lava flows, epidote, anhydrite, and scarce hematite occur locally. Alteration and leaching in the basal 2 m are unique and have led to the postulation of a localized two-phase fluid zone consisting mainly of steam and CO2. The hydrothermal system of Newberry 2 is a simple evolving system associated with the evolution of Newberry Volcano. Only a few localized highly altered intervals where fracturing controlled fluid access occur in the core. There are no crosscutting fractures to indicate multiple hydrothermal systems. Chemical analyses of altered rocks and equivalent fresh rocks indicate that little chemical migration has taken place.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB093iB09p10174","issn":"01480227","usgsCitation":"Keith, T.E., and Bargar, K., 1988, Petrology and hydrothermal mineralogy of US Geological Survey Newberry: 2. Drill core from Newberry Caldera, Oregon: Journal of Geophysical Research Solid Earth, v. 93, no. B9, p. 10174-10190, https://doi.org/10.1029/JB093iB09p10174.","productDescription":"17 p.","startPage":"10174","endPage":"10190","numberOfPages":"17","costCenters":[],"links":[{"id":225381,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"B9","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a7822e4b0c8380cd78645","contributors":{"authors":[{"text":"Keith, T. E. C.","contributorId":11681,"corporation":false,"usgs":true,"family":"Keith","given":"T.","email":"","middleInitial":"E. C.","affiliations":[],"preferred":false,"id":368382,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bargar, K.E.","contributorId":44548,"corporation":false,"usgs":true,"family":"Bargar","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":368383,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70176046,"text":"70176046 - 1988 - Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1987, with 1934-87 summary","interactions":[],"lastModifiedDate":"2016-08-24T10:47:26","indexId":"70176046","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"47","title":"Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1987, with 1934-87 summary","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Nalley, G., and Rettman, P., 1988, Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1987, with 1934-87 summary: Edwards Underground Water District Bulletin 47, 154 p.","productDescription":"154 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327778,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6aef3e4b0f2f0cebe4637","contributors":{"authors":[{"text":"Nalley, G.M.","contributorId":23535,"corporation":false,"usgs":true,"family":"Nalley","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":646899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":646900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014429,"text":"70014429 - 1988 - Ocean plateau-seamount origin of basaltic rocks, Angayucham terrane, central Alaska","interactions":[],"lastModifiedDate":"2024-03-14T11:16:38.412331","indexId":"70014429","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2309,"text":"Journal of Geology","active":true,"publicationSubtype":{"id":10}},"title":"Ocean plateau-seamount origin of basaltic rocks, Angayucham terrane, central Alaska","docAbstract":"The Angayucham terrane of north-central Alaska (immediately S of the Brooks Range) is a large (ca. 500 km E-W), allochthonous complex of Devonian to Lower Jurassic pillow basalt, diabase sills, gabbro plutons, and chert. The mafic rocks are transitional normal-to-enriched, mid-ocean-ridge (MORB) type tholeiites (TiO2 1.2-3.4%, Nb 7-23 ppm, Ta 0.24-1.08 ppm, Zr 69-214 ppm, and light REE's slightly depleted to moderately enriched). Geologic and geochemical constraints indicate that Angayucham terrane is the upper \"skin' (ca. 3-4 km thick) of a long-lived (ca. 170-200 ma) oceanic plateau whose basaltic-gabbroic rocks are like those of seamounts of the East Pacific Rise. -Authors","language":"English","publisher":"University of Chicago Press","issn":"00221376","usgsCitation":"Barker, F., Jones, D.L., Budahn, J., and Coney, P., 1988, Ocean plateau-seamount origin of basaltic rocks, Angayucham terrane, central Alaska: Journal of Geology, v. 96, no. 3, p. 368-374.","productDescription":"7 p.","startPage":"368","endPage":"374","numberOfPages":"7","costCenters":[],"links":[{"id":225380,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6c94e4b0c8380cd74ccf","contributors":{"authors":[{"text":"Barker, F.","contributorId":101368,"corporation":false,"usgs":true,"family":"Barker","given":"F.","affiliations":[],"preferred":false,"id":368381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":368378,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Budahn, J. R. 0000-0001-9794-8882","orcid":"https://orcid.org/0000-0001-9794-8882","contributorId":83914,"corporation":false,"usgs":true,"family":"Budahn","given":"J. R.","affiliations":[],"preferred":false,"id":368380,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Coney, P.J.","contributorId":67065,"corporation":false,"usgs":true,"family":"Coney","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":368379,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70014402,"text":"70014402 - 1988 - MAGMIX: a basic program to calculate viscosities of interacting magmas of differing composition, temperature, and water content","interactions":[],"lastModifiedDate":"2013-01-21T15:34:37","indexId":"70014402","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"MAGMIX: a basic program to calculate viscosities of interacting magmas of differing composition, temperature, and water content","docAbstract":"MAGMIX is a BASIC program designed to predict viscosities at thermal equilibrium of interacting magmas of differing compositions, initial temperatures, crystallinities, crystal sizes, and water content for any mixing proportion between end members. From the viscosities of the end members at thermal equilibrium, it is possible to predict the styles of magma interaction expected for different initial conditions. The program is designed for modeling the type of magma interaction between hypersthenenormative magmas at upper crustal conditions. Utilization of the program to model magma interaction at pressures higher than 200 MPa would require modification of the program to account for the effects of pressure on heat of fusion and magma density. ?? 1988.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(88)90005-2","issn":"00983004","usgsCitation":"Frost, T.P., and Lindsay, J., 1988, MAGMIX: a basic program to calculate viscosities of interacting magmas of differing composition, temperature, and water content: Computers & Geosciences, v. 14, no. 2, p. 213-228, https://doi.org/10.1016/0098-3004(88)90005-2.","startPage":"213","endPage":"228","numberOfPages":"16","costCenters":[],"links":[{"id":266180,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(88)90005-2"},{"id":225953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4aade4b0c8380cd68f57","contributors":{"authors":[{"text":"Frost, T. P.","contributorId":49797,"corporation":false,"usgs":true,"family":"Frost","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":368326,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindsay, J.R.","contributorId":45452,"corporation":false,"usgs":true,"family":"Lindsay","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":368325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014465,"text":"70014465 - 1988 - Mechanistic characterization of chloride interferences in electrothermal atomization systems","interactions":[],"lastModifiedDate":"2020-01-12T14:22:27","indexId":"70014465","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Mechanistic characterization of chloride interferences in electrothermal atomization systems","docAbstract":"A computer-controlled spectrometer with a photodiode array detector has been used for wavelength and temperature resolved characterization of the vapor produced by an electrothermal atomizer. The system has been used to study the chloride matrix interference on the atomic absorption spectrometric determination of manganese and copper. The suppression of manganese and copper atom populations by matrix chlorides such as those of calcium and magnesium is due to the gas-phase formation of an analyte chloride species followed by the diffusion of significant fractions of these species from the atom cell prior to completion of the atomization process. The analyte chloride species cannot be formed when matrix chlorides with metal-chloride bond dissociation energies above those of the analyte chlorides are the principal entitles present. The results indicate that multiple wavelength spectrometry used to obtain temperature-resolved spectra is a viable tool in the mechanistic characterization of interference effects observed with electrothermal atomization systems.
","language":"English","publisher":"ACS","doi":"10.1021/ac00174a010","issn":"00032700","usgsCitation":"Shekiro, J., Skogerboe, R., and Taylor, H.E., 1988, Mechanistic characterization of chloride interferences in electrothermal atomization systems: Analytical Chemistry, v. 60, no. 23, p. 2578-2582, https://doi.org/10.1021/ac00174a010.","productDescription":"5 p.","startPage":"2578","endPage":"2582","numberOfPages":"5","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":225958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"23","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5373e4b0c8380cd6cac4","contributors":{"authors":[{"text":"Shekiro, J.M. Jr.","contributorId":11773,"corporation":false,"usgs":true,"family":"Shekiro","given":"J.M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":368459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skogerboe, R.K.","contributorId":7348,"corporation":false,"usgs":true,"family":"Skogerboe","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":368458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":368460,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70014425,"text":"70014425 - 1988 - Icebergs rework shelf sediments to 500 m off Antarctica","interactions":[],"lastModifiedDate":"2024-01-24T12:32:57.237036","indexId":"70014425","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Icebergs rework shelf sediments to 500 m off Antarctica","docAbstract":"Icebergs and sea ice rework the sediments of high-latitude shelves, producing modern diamicts (ice-keel turbates) unrelated to glacial proximity. Off Antarctica, sidescan sonar data indicate the presence of ice-gouge features formed by the physical interaction between ice keels and the sea bed. These are recognized as incisions a few metres deep and tens of metres wide, in water depths up to 500 m. On the submarine bank tops and slopes off Wilkes Land and in the Weddell Sea, subcircular depressions 30 to 150 m in diameter, a washboard pattern, and hummocky bed features also represent iceberg-resting sites. The freshness of sea-bed morphology, nearby Holocene sediment ponding, and active hydraulic sedimentary processes indicate that the sea floor is being reworked by iceberg keels. Tabular iceberg drafts in excess of 330 m have been measured, and modeling studies suggest that nontabular iceberg drafts of 500 m are possible. We conclude that a modern ice-keel turbate deposit in the form of a poorly stratified diamicton is probably widespread on that part (54%) of the Antarctic shelf less than 500 m deep.
No abstract available
","language":"English","publisher":"Bonneville Power Administration","publisherLocation":"Portland, OR","usgsCitation":"Poe, T., and Rieman, B., 1988, Predation by resident fish on juvenile salmonids in John Day Reservoir.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"John Day reservoir ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.67176818847656,\n 45.74500616007653\n ],\n [\n -120.87570190429688,\n 45.682678322324904\n ],\n [\n -120.94642639160158,\n 45.67116404333791\n ],\n [\n -120.94917297363281,\n 45.63516665067313\n ],\n [\n -120.88874816894531,\n 45.62652383350405\n ],\n [\n -120.79399108886719,\n 45.67596194751415\n ],\n [\n -120.63400268554689,\n 45.73206686696598\n ],\n [\n -120.67176818847656,\n 45.74500616007653\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d5e4b0fa1e59bc1ea8","contributors":{"authors":[{"text":"Poe, T.P.","contributorId":51687,"corporation":false,"usgs":true,"family":"Poe","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":662448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rieman, B.E.","contributorId":67283,"corporation":false,"usgs":true,"family":"Rieman","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":662449,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014464,"text":"70014464 - 1988 - Tectonic significance of dikes of Westerly Granite, southeastern Connecticut and southwestern Rhode Island","interactions":[],"lastModifiedDate":"2012-03-12T17:19:30","indexId":"70014464","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2896,"text":"Northeastern Geology","active":true,"publicationSubtype":{"id":10}},"title":"Tectonic significance of dikes of Westerly Granite, southeastern Connecticut and southwestern Rhode Island","docAbstract":"Undeformed Early Permian Westerly Granite dikes cut gneisses of the southeastern New England Avalon zone along coastal southeastern Connecticut and adjacent Rhode Island. Most dikes dip southward at a low angle. The Westerly dikes were emplaced in relatively warm rock penecontemporaneously with the Narragansett Pier Granite during a narrow time interval shortly after cessation of pervasive Alleghanian ductile deformation but probably before final localized movement on major shear zones. The gentle dips indicate subhorizontal release at the end stage of the Alleghanian compressive event. Doming, intrusion of granite, and subsequent rapid uplift and cooling are attributed to the underplating of Avalonian crust by an African plate during the Alleghanian. -Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Northeastern Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Goldsmith, R., 1988, Tectonic significance of dikes of Westerly Granite, southeastern Connecticut and southwestern Rhode Island: Northeastern Geology, v. 10, no. 3, p. 195-201.","startPage":"195","endPage":"201","numberOfPages":"7","costCenters":[],"links":[{"id":225957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba47de4b08c986b32038f","contributors":{"authors":[{"text":"Goldsmith, R.","contributorId":49809,"corporation":false,"usgs":true,"family":"Goldsmith","given":"R.","email":"","affiliations":[],"preferred":false,"id":368457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1804,"text":"wsp2329 - 1988 - Effects of highway runoff on streamflow and water quality in the Sevenmile Creek basin, a rural area in the Piedmont Province of North Carolina, July 1981 to July 1982","interactions":[],"lastModifiedDate":"2023-04-07T20:35:42.292711","indexId":"wsp2329","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2329","title":"Effects of highway runoff on streamflow and water quality in the Sevenmile Creek basin, a rural area in the Piedmont Province of North Carolina, July 1981 to July 1982","docAbstract":"An evaluation of water-quality data from streams that receive stormwater runoff from a segment of Interstate Highway 85 in North Carolina indicated increased levels of many constituents compared to levels in nearby undeveloped basins. Additional data collected from a network of dry and wet atmospheric deposition collectors, lysimeter samples, soil surveys, wind measurements, and road sweepings helped define the general sources and migration of chemical substances near the highway. The eight study basins, located in a rural area in the Piedmont of North Carolina, had a combined area of 17.5 square miles and drained a 4.8-mile-long segment of the interstate. The average traffic flow along this section was 25,000 vehicles per day.\r\n\r\nDuring storm runoff, streamflow in basins traversed by the highway rose and fell more rapidly than that in the undeveloped basins. This more rapid response is due to the impervious, paved area of the basins and the manmade drainage systems designed to rapidly move water off the highway.\r\n\r\nAlkalinity, specific conductance, and concentrations of calcium, sodium, and chloride were greater at the highway stations than in the undeveloped basins as a result of highway salting for control of ice. Specific conductance and concentrations of dissolved and total nitrogen peaked at the beginning of each storm event. The data indicated that, for the study basins, highway runoff had little or no effect on suspended sediment, water temperature, dissolved oxygen, and pH. However, the pH at all stations decreased during stormflow because the rainfall drained off by the streams had pH values less than 5.7.\r\n\r\nHigh metals concentrations were found in the soils within 100 feet of the highway and in the soil water infiltrating the soil zone. Chromium, copper, nickel, and zinc concentrations in the streams near the highway generally were above the maximum levels recommended by the U.S. Environmental Protection Agency (EPA) for the protection of aquatic life. Lead and cadmium concentrations frequently exceeded the maximum levels recommended by the EPA for drinking water.\r\n\r\n\r\nThe highway is a source of contaminants to surrounding areas. Particulate and metal loads in dustfall and chemical-constituent concentrations in soils decrease exponentially with distance from the highway. The highest concentrations of contaminants were found on the downwind side. Increased concentrations of metals (cadmium, chromium, iron, lead, nickel, and zinc) in rainfall were observed in samples collected near the highway and in samples collected approximately one-half mile away. Material loading due to dustfall was greater than loading due to rainfall. Loading due to saltated particles, those heavier particles bounced along the highway surface, was higher than loading due to dustfall. Saltation loads were greatest during the winter months because of highway deicing and sanding, which supplied an estimated two-thirds of the saltated materials. The remaining one-third of the saltated load came primarily from the deposition of particles from vehicles. Some of the greatest constituent concentrations were measured in the soil water sampled from the lysimeters located adjacent to the highway.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2329","usgsCitation":"Harned, D., 1988, Effects of highway runoff on streamflow and water quality in the Sevenmile Creek basin, a rural area in the Piedmont Province of North Carolina, July 1981 to July 1982: U.S. Geological Survey Water Supply Paper 2329, vi, 33 p., https://doi.org/10.3133/wsp2329.","productDescription":"vi, 33 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":415468,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25311.htm","linkFileType":{"id":5,"text":"html"}},{"id":26958,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2329/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137031,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2329/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Piedmont Province, Sevenmile Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.223,\n 36.019\n ],\n [\n -79.125,\n 36.019\n ],\n [\n -79.125,\n 36.083\n ],\n [\n -79.223,\n 36.083\n ],\n [\n -79.223,\n 36.019\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aea2c","contributors":{"authors":[{"text":"Harned, Douglas","contributorId":11195,"corporation":false,"usgs":true,"family":"Harned","given":"Douglas","affiliations":[],"preferred":false,"id":144184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}