Structurally complex sequences of sedimentary, volcanic, and intrusive igneous rocks characterize a nearly continuous narrow band along the Pacific coast of North America from Baja California, Mexico to southern Alaska. They occur in two modes: (1) as complexly folded but coherent sequences of graywacke and argillite that locally exhibit blueschist-grade metamorphism, and (2) as melanges containing large blocks of graywacke, chert, volcanic and plutonic rocks, high-grade schist, and limestone in a highly sheared pelitic, cherty, or sandstone matrix. Fossils from the coherent graywacke sequences range in age from late Jurassic to Eocene; fossils from limestone blocks in the melanges range in age from mid-Paleozoic to middle Cretaceous. Fossils from the matrix surrounding the blocks, however, are of Jurassic, Cretaceous, and rarely, Tertiary age, indicating that fossils from the blocks cannot be used to date the time of formation of the melanges.
Both the deformation of the graywacke, with accompanying blueschist metamorphism, as well as the formation of the melanges, are believed to be the result of late Mesozoic and early Tertiary subduction. The origin of the melanges, particularly the emplacement of exotic tectonic blocks, is not understood.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(78)90031-8","issn":"00401951","usgsCitation":"Jones, D.L., Blake, M., Bailey, E.H., and McLaughlin, R.J., 1978, Distribution and character of upper Mesozoic subduction complexes along the west coast of North America: Tectonophysics, v. 47, no. 3-4, p. 207-222, https://doi.org/10.1016/0040-1951(78)90031-8.","productDescription":"16 p.","startPage":"207","endPage":"222","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":222209,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, Mexico, United States","state":"Alaska, California, Oregon, Washington","otherGeospatial":"Pacific coast of North America","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -154.41285894795098,\n 60.39101073090987\n ],\n [\n -139.43492469830107,\n 56.18442278816785\n ],\n [\n -127.41314296806209,\n 47.475629746329844\n ],\n [\n -124.45488000214503,\n 36.374566798936016\n ],\n [\n -110.61276212523683,\n 21.147885276292897\n ],\n [\n -108.04987973063052,\n 22.069396089742753\n ],\n [\n -119.6495023669611,\n 39.75914188879055\n ],\n [\n -122.86602155790652,\n 49.694221938084205\n ],\n [\n -134.69578953504842,\n 60.73706770472893\n ],\n [\n -145.72029861273748,\n 61.97887606686548\n ],\n [\n -154.41285894795098,\n 60.39101073090987\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"47","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a027ee4b0c8380cd50082","contributors":{"authors":[{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":363898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blake, M.C. Jr.","contributorId":27094,"corporation":false,"usgs":true,"family":"Blake","given":"M.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":363896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, E. H.","contributorId":44509,"corporation":false,"usgs":true,"family":"Bailey","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":363897,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McLaughlin, R. J. 0000-0002-4390-2288","orcid":"https://orcid.org/0000-0002-4390-2288","contributorId":107271,"corporation":false,"usgs":true,"family":"McLaughlin","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":363899,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70012862,"text":"70012862 - 1978 - Structures developed in fault gouge during stable sliding and stick-slip","interactions":[],"lastModifiedDate":"2025-09-02T16:26:13.097611","indexId":"70012862","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Structures developed in fault gouge during stable sliding and stick-slip","docAbstract":"We carried out a detailed study of the structural changes that occurred in a thin layer of quartz gouge sheared between saw cuts in granite cylinders at pressures of 2 and 4.7 kbar. At low pressure the material deformed stably, but at high pressure deformation was unstable. During deformation shear zones were developed oblique and parallel to the plane of the saw cuts. Our results suggest that shearing oblique to the strike of the fault zone precedes sudden slip, which is confined to the margin between the intact rock and gouge. If this is true in the natural situation, then it may be possible by studying the spacial distribution of the microseismic activity and creep in shear zones to determine whether sudden slip is imminent.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(78)90068-9","issn":"00401951","usgsCitation":"Byerlee, J., Mjachkin, V., Summers, R., and Voevoda, O., 1978, Structures developed in fault gouge during stable sliding and stick-slip: Tectonophysics, v. 44, no. 1-4, p. 161-171, https://doi.org/10.1016/0040-1951(78)90068-9.","productDescription":"11 p.","startPage":"161","endPage":"171","costCenters":[],"links":[{"id":222445,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9c7fe4b08c986b31d416","contributors":{"authors":[{"text":"Byerlee, J.","contributorId":105838,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.","affiliations":[],"preferred":false,"id":364699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mjachkin, V.","contributorId":80421,"corporation":false,"usgs":true,"family":"Mjachkin","given":"V.","affiliations":[],"preferred":false,"id":364697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Summers, R.","contributorId":65483,"corporation":false,"usgs":true,"family":"Summers","given":"R.","email":"","affiliations":[],"preferred":false,"id":364696,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Voevoda, O.","contributorId":101811,"corporation":false,"usgs":true,"family":"Voevoda","given":"O.","email":"","affiliations":[],"preferred":false,"id":364698,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5221448,"text":"5221448 - 1978 - Effects of No. 2 fuel oil on common eider eggs","interactions":[],"lastModifiedDate":"2025-05-12T16:33:39.262902","indexId":"5221448","displayToPublicDate":"2003-04-07T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2676,"text":"Marine Pollution Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Effects of No. 2 fuel oil on common eider eggs","docAbstract":"An oil spill near a breeding colony could result in the transfer of oil from the plumage and feet of incubating birds to their eggs. Microlitre amounts of No. 2 fuel oil were applied externally to common eider eggs in an island breeding colony in Maine. Clutches of eggs treated with 20 ?l of fuel oil had significantly greater embryonic mortality than the control clutches when they were examined 7 days after treatment. The results are similar to those of an earlier study of artificially incubated common eider eggs and indicate that nest site conditions do not affect embryotoxicity of No. 2 fuel oil.","language":"English","publisher":"Elsevier","doi":"10.1016/0025-326X(78)90590-8","usgsCitation":"Albers, P., and Szaro, R.C., 1978, Effects of No. 2 fuel oil on common eider eggs: Marine Pollution Bulletin, v. 9, no. 5, p. 138-139, https://doi.org/10.1016/0025-326X(78)90590-8.","productDescription":"2 p.","startPage":"138","endPage":"139","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197443,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","otherGeospatial":"Bangs Island, East Casco Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.18236357335988,\n 43.759784030767946\n ],\n [\n -70.18236357335988,\n 43.6761981129479\n ],\n [\n -70.0670930378678,\n 43.6761981129479\n ],\n [\n -70.0670930378678,\n 43.759784030767946\n ],\n [\n -70.18236357335988,\n 43.759784030767946\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"9","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624fc6","contributors":{"authors":[{"text":"Albers, P.H.","contributorId":26646,"corporation":false,"usgs":true,"family":"Albers","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":333871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szaro, Robert C.","contributorId":21240,"corporation":false,"usgs":false,"family":"Szaro","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":333870,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012473,"text":"70012473 - 1978 - Arctic continental shelf morphology related to sea-ice zonation, Beaufort Sea, Alaska","interactions":[],"lastModifiedDate":"2025-04-18T15:55:47.548736","indexId":"70012473","displayToPublicDate":"2003-04-04T00:00:00","publicationYear":"1978","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":"Arctic continental shelf morphology related to sea-ice zonation, Beaufort Sea, Alaska","docAbstract":"Landsat-1 and NOAA satellite imagery for the winter 1972–1973, and a variety of ice and sea-floor data were used to study sea-ice zonation and dynamics and their relation to bottom morphology and geology on the Beaufort Sea continental shelf of arctic Alaska.
In early winter the location of the boundary between undeformed fast ice and westward-drifting pack ice of the Pacific Gyre is controlled by major coastal promontories. Pronounced linear pressure- and shear-ridges, as well as hummock fields, form along this boundary and are stabilized by grounding, generally between the 10- and 20-m isobaths. Slippage along this boundary occurs intermittently at or seaward of the grounded ridges, forming new grounded ridges in a widening zone, the stamukhi zone, which by late winter extends out to the 40-m isobath. Between intermittent events along the stamukhi zone, pack-ice drift and slippage is continuous along the shelf edge, at average rates of 3–10 km/day. Whether slippage occurs along the stamukhi zone or along the shelf edge, it is restricted to a zone several hundred meters wide, and ice seaward of the slip face moves at uniform rates without discernible drag effects.
A causal relationship is seen between the spatial distribution of major ice-ridge systems and offshore shoals downdrift of major coastal promontories. The shoals appear to have migrated shoreward under the influence of ice up to 400 m in the last 25 years. The sea floor seaward of these shoals within the stamukhi zone shows high ice-gouge density, large incision depths, and a high degree of disruption of internal sedimentary structures. The concentration of large ice ridges and our sea floor data in the stamukhi zone indicate that much of the available marine energy is expended here, while the inner shelf and coast, where the relatively undeformed fast ice grows, are sheltered. There is evidence that anomalies in the overall arctic shelf profile are related to sea-ice zonation, ice dynamics, and bottom processes. A proposed ice zonation, including zones of (1) bottom-fast ice, (2) floating fast ice, (3) stamukhi, and (4) seasonal pack ice, emphasizes ice interaction with the shelf surface and differs from previous zonation.
Certain aspects of the results reported here are directly applicable to planned offshore developments in the Prudhoe Bay oil field. Properly placed artificial structures similar to offshore shoals should be able to withstand the forces of the ice, serve to modify the observed ice zonation, and might be used to make the environment less hostile to human activities.
","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(78)90018-X","issn":"00253227","usgsCitation":"Reimnitz, E., Toimil, L., and Barnes, P., 1978, Arctic continental shelf morphology related to sea-ice zonation, Beaufort Sea, Alaska: Marine Geology, v. 28, no. 3-4, p. 179-210, https://doi.org/10.1016/0025-3227(78)90018-X.","productDescription":"29 p.","startPage":"179","endPage":"210","costCenters":[],"links":[{"id":221949,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -167.95988350415863,\n 71.13296067931378\n ],\n [\n -167.95988350415863,\n 68.37053168683431\n ],\n [\n -157.50512865265642,\n 68.37053168683431\n ],\n [\n -157.50512865265642,\n 71.13296067931378\n ],\n [\n -167.95988350415863,\n 71.13296067931378\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"28","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ed53e4b0c8380cd49736","contributors":{"authors":[{"text":"Reimnitz, E.","contributorId":61557,"corporation":false,"usgs":true,"family":"Reimnitz","given":"E.","affiliations":[],"preferred":false,"id":363693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toimil, L.","contributorId":65603,"corporation":false,"usgs":true,"family":"Toimil","given":"L.","email":"","affiliations":[],"preferred":false,"id":363694,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnes, P.","contributorId":73331,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","affiliations":[],"preferred":false,"id":363695,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70012599,"text":"70012599 - 1978 - Correlation and zonation of miocene strata along the atlantic margin of North America using diatoms and silicoflagellates","interactions":[],"lastModifiedDate":"2025-05-12T15:59:59.708361","indexId":"70012599","displayToPublicDate":"2003-04-02T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Correlation and zonation of miocene strata along the atlantic margin of North America using diatoms and silicoflagellates","docAbstract":"Six Atlantic Miocene siliceous microfossil zones are proposed based on onshore and offshore samples from the United States Atlantic Margin. Diatoms and silicoflagellates are used to establish the zones. These zones are from oldest to youngest:
1. Zone I Actinoptychus heliopelta Concurrent Range Zone - Early Miocene
2. Zone II Delphineis ovata Partial Range Zone - late Early to early Middle Miocene
3. Zone III Delphineis ovata/Delphineis penelliptica Concurrent Range Zone - early Middle Miocene
4. Zone IV Delphineis penelliptica Partial Range Zone - Middle Miocene
5. Zone V Delphineis penelliptica/Coscinodiscus plicatus Concurrent Range Zone - Middle Miocene
6. Zone VI Coscinodiscus plicatus Partial Range Zone - Middle Miocene.
The six zones are easily traced along the Southern and Middle Atlantic Seaboard, but the older three are found for the most part between Cape Hatteras and New Jersey. There is some suggestion of sea-level change during Zone IV. Using rare planktonic diatoms that are index species from other regions and the zonal markers established in this study, correlation can be made with the Standard Foraminiferal Zones, the North Pacific Diatom Zones and with DSDP core 391A in the Blake-Bahama Basin.
","language":"English","publisher":"Elsevier","doi":"10.1016/0377-8398(78)90009-9","issn":"03778398","usgsCitation":"Abbott, W., 1978, Correlation and zonation of miocene strata along the atlantic margin of North America using diatoms and silicoflagellates: Marine Micropaleontology, v. 3, no. 1, p. 15-34, https://doi.org/10.1016/0377-8398(78)90009-9.","productDescription":"20 p.","startPage":"15","endPage":"34","costCenters":[],"links":[{"id":222212,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc28e4b0c8380cd4e152","contributors":{"authors":[{"text":"Abbott, W.H.","contributorId":20076,"corporation":false,"usgs":true,"family":"Abbott","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":364017,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010324,"text":"70010324 - 1978 - Characterization of high-frequency strong ground motion","interactions":[],"lastModifiedDate":"2025-08-29T16:58:00.726754","indexId":"70010324","displayToPublicDate":"2003-04-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of high-frequency strong ground motion","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(78)90187-7","issn":"00401951","usgsCitation":"Hanks, T.C., 1978, Characterization of high-frequency strong ground motion: Tectonophysics, v. 49, no. 3-4, p. 263-263, https://doi.org/10.1016/0040-1951(78)90187-7.","productDescription":"1 p.","startPage":"263","endPage":"263","costCenters":[],"links":[{"id":218642,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f4cbe4b0c8380cd4bf06","contributors":{"authors":[{"text":"Hanks, Thomas C.","contributorId":35763,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","middleInitial":"C.","affiliations":[],"preferred":false,"id":358643,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012493,"text":"70012493 - 1978 - An inverse method for earthquake source mechanisms","interactions":[],"lastModifiedDate":"2025-09-02T15:54:01.168945","indexId":"70012493","displayToPublicDate":"2003-04-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"An inverse method for earthquake source mechanisms","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(78)90181-6","issn":"00401951","usgsCitation":"Julian, B.R., 1978, An inverse method for earthquake source mechanisms: Tectonophysics, v. 49, no. 3-4, p. 223-223, https://doi.org/10.1016/0040-1951(78)90181-6.","productDescription":"1 p.","startPage":"223","endPage":"223","costCenters":[],"links":[{"id":222257,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea8ee4b0c8380cd48939","contributors":{"authors":[{"text":"Julian, Bruce R.","contributorId":50063,"corporation":false,"usgs":true,"family":"Julian","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363747,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012632,"text":"70012632 - 1978 - Matrix effects on the determination of manganese in geological materials by atomic-absorption spectrophotometry under different flame conditions","interactions":[],"lastModifiedDate":"2025-08-13T16:14:26.209682","indexId":"70012632","displayToPublicDate":"2002-01-22T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Matrix effects on the determination of manganese in geological materials by atomic-absorption spectrophotometry under different flame conditions","docAbstract":"Suppression caused by five of the seven matrix elements studied (Si, Al, Fe, Ca and Mg) was observed in the atomic-absorption determination of manganese in geological materials, when synthetic solutions and the recommended oxidizing air—acetylene flame were used. The magnitude of the suppression effects depends on (1) the kind and concentration of the interfering elements, (2) the type of acid medium, and (3) the concentration of manganese to be determined. All interferences noted are removed or alleviated by using a reducing nitrous oxide—acetylene flame. The atomic-absorption method using this flame can be applied to the determination of total and extractable manganese in a wide range of geological materials without interferences. Analyses of six U.S. Geological Survey rock standards for manganese gave results in agreement with the reported values.
","language":"English","publisher":"Elsevier","doi":"10.1016/0039-9140(78)80058-7","issn":"00399140","usgsCitation":"Sanzolone, R.F., and Chao, T.T., 1978, Matrix effects on the determination of manganese in geological materials by atomic-absorption spectrophotometry under different flame conditions: Talanta, v. 25, no. 5, p. 287-290, https://doi.org/10.1016/0039-9140(78)80058-7.","productDescription":"4 p.","startPage":"287","endPage":"290","costCenters":[],"links":[{"id":222669,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a528ee4b0c8380cd6c4d6","contributors":{"authors":[{"text":"Sanzolone, R. F.","contributorId":64199,"corporation":false,"usgs":true,"family":"Sanzolone","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":364101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chao, T. T.","contributorId":31900,"corporation":false,"usgs":true,"family":"Chao","given":"T.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":364100,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012630,"text":"70012630 - 1978 - Atomic-absorption determination of beryllium in geological materials by use of electrothermal atomization","interactions":[],"lastModifiedDate":"2025-08-13T16:07:52.082569","indexId":"70012630","displayToPublicDate":"2002-01-22T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Atomic-absorption determination of beryllium in geological materials by use of electrothermal atomization","docAbstract":"A method is described for the atomic-absorption determination of beryllium in geological materials, that utilizes electrothermal atomization after a separation by solvent extraction. Samples are decomposed with hydrofluoric acid and nitric acid in Teflon-lined pressure decomposition vessels. Beryllium is isolated by its extraction as beryllium acetylacetonate at pH 8 into xylene and back-extraction in 3M hydrochloric acid. The method has been successfully applied to the determination of beryllium in 14 U.S. Geological Survey standard rocks. Four subsamples from four bottles of each standard sample were analysed in random order. The mean beryllium contents (ppm) are: AGV-1, 1.98; PCC-1, 0.024; MAG-1, 2.84; BHVO-1, 0.90; DTS-1, 0.026; SCo-1, 1.74; SDC-1, 2.52; BCR-1, 1.44; GSP-1, 1.22; SGR-1, 0.86; QLO-1, 1.83; RGM-1, 2.21; STM-1, 8.75; G-2, 2.29. An analysis of variance shows that all the samples may be considered homogeneous at F0.95 except AGV-1 and DTS-1 which may be considered homogeneous at F0.99.
","language":"English","publisher":"Elsevier","doi":"10.1016/0039-9140(78)80050-2","issn":"00399140","usgsCitation":"Campbell, E., and Simon, F., 1978, Atomic-absorption determination of beryllium in geological materials by use of electrothermal atomization: Talanta, v. 25, no. 5, p. 251-255, https://doi.org/10.1016/0039-9140(78)80050-2.","productDescription":"5 p.","startPage":"251","endPage":"255","costCenters":[],"links":[{"id":222667,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eec9e4b0c8380cd49f6c","contributors":{"authors":[{"text":"Campbell, E.Y.","contributorId":59803,"corporation":false,"usgs":true,"family":"Campbell","given":"E.Y.","email":"","affiliations":[],"preferred":false,"id":364097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simon, F.O.","contributorId":41808,"corporation":false,"usgs":true,"family":"Simon","given":"F.O.","email":"","affiliations":[],"preferred":false,"id":364096,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66425,"text":"i1088 - 1978 - Geologic map of the Crater section of Haleakala National Park, Maui, Hawaii","interactions":[],"lastModifiedDate":"2022-09-07T21:26:36.636547","indexId":"i1088","displayToPublicDate":"1996-02-01T00:00:00","publicationYear":"1978","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":"1088","title":"Geologic map of the Crater section of Haleakala National Park, Maui, Hawaii","docAbstract":"No abstract available.
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It is the highest yielding aquifer in Mississippi with individual well yields as high as 5,000 gal/min. Major wells producing from the aquifer range in depth from 60 to 260 ft and are commonly screened in the coarse gravel at the base of the aquifer. Water levels in wells are generally between 5 and 30 feet below land surface, except near points of heavy pumping. Water from the alluvial aquifer is a hard, calcium bicarbonate type containing excessive iron in most places. In 1975, 745 Mgal/d, mostly for irrigation, were withdrawn from the alluvial aquifer. In the 7,000 sq mi area in northwestern Mississippi, the alluvial aquifer has been estimated to be capable of yielding over 1,700 Mgal/d, not including the 500 sq mi area in southwestern Mississippi. 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The data are presented in graphs and tables. Surface-water data include streamflow measurements and analyses of water collected at 58 sites; ground-water data include descriptions of 360 wells and core holes, analyses of water and hydrographs of selected wells, lithologic logs of 131 wells and test borings, and natural-gamma logs of selected wells ranging in depth from 110 to 1,346 feet. Rainfall and municipal pumpage data also are compiled. Maps show the location of the data-collection sites within the area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7897","collaboration":"Prepared in cooperation with Gadsden County and Northwest Florida Water Management District","usgsCitation":"Pascale, C.A., Wagner, J.R., and Sohm, J.E., 1978, Hydrologic, geologic, and water-quality data, Ochlockonee River basin area, Florida: U.S. Geological Survey Water-Resources Investigations Report 78-97, Report: vi, 5l5 p.; 2 Figures: 17.08 x 19.88 inches and 16.87 x 19.90 inches, https://doi.org/10.3133/wri7897.","productDescription":"Report: vi, 5l5 p.; 2 Figures: 17.08 x 19.88 inches and 16.87 x 19.90 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