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  • Data  (3)
  • 1955-1959  (3)
Collection
Keywords
Publisher
Years
Year
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Tatsumoto, M; Goldberg, Edward D (1959): Some aspects of the marine geochemistry of uranium. Geochimica et Cosmochimica Acta, 17(3-4), 201-208, https://doi.org/10.1016/0016-7037(59)90094-8
    Publication Date: 2023-08-28
    Description: The uranium concentrations in marine calcareous material of a biological origin varied between 0.0X and 0.X p.p.m. with the exception of corals which had concentrations of several p.p.m. The aragonitic oolites and aragonite precipitated from sea-water had values similar to those of the corals. A geochronology based on the growth of ionium (thorium-230) from uranium is applicable not only to corals, as previous investigators have pointed out, but also to oolites. Several examples of "oolite ages" are given. The uranium content of ferromanganese minerals from pelagic deposits is of the order of from 4 to 5 p.p.m.
    Keywords: Atlantic Ocean; DEPTH, sediment/rock; DNWB0BBD; DNWB0BBD-047G; DNWB0BBD-052G; DOWNWIND-B2; DOWNWIND-H; Dredge; DRG; DWBG47; DWBG52; DWHD55; Event label; GC; Gravity corer; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Spencer F. Baird; TH1; TH1-TR4; Theta; Uranium; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
    Location Call Number Expected Availability
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bramlette, M; Faughn, James L; Hurley, RJ (1959): Anomalous sediment deposition on the flank of Eniwetok Atoll. Geological Society of America Bulletin, 70(12), 1549-1552, https://doi.org/10.1130/0016-7606(1959)70%5B1549:ASDOTF%5D2.0.CO;2
    Publication Date: 2023-08-28
    Description: Some short cores from the shelf at about 800-1000 fathoms on the southwest flank of Eniwetok Atoll penetrated Pliocene deposits with little to no later sediment cover. The Quaternary deposits include much coarse reef debris, particularly the fragments of algae such as Halimeda and other shallow-water material up to several millimeters in grain size, mixed with varying amounts of pelagic Foraminifera. The Pliocene sediments (one may be upper Miocene) are pure pelagic deposits of much finer grain size, consisting of coccoliths and pelagic Foraminifera with no admixture of reef material. Bottom photographs show areas of well-developed ripple marks in coarse sediment (C. J. Shipek, manuscript) apparently formed only in the areas with the veneer of post-Tertiary coarse sediments. A brown impregnation at the top and extending down as mottling for a few centimeters is also usual in the Tertiary sediment of the cores. This seems to consist of iron and manganese oxides and adds somewhat to the induration.
    Keywords: 10-J1268; 10-J1269; 10-J1270; 10-J1271; 10-J1272; 10-J1273; 10-J1274; 10-J1275; 11-J1276; 3-J1225; 3-J1226; 3-J1227; 3-J1228; 4-J1230; 4-J1231; 4-J1232; 4-J1233; 4-J1234; 4-J1235; 6-J1237; 6-J1238; 6-J1239; 6-J1240; 6-J1241; 6-J1242; 6-J1243; 6-J1244; 8-J1260; 8-J1261; 8-J1262; 8-J1263; 8-J1264; 8-J1265; 8-J1266; Comment; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; ENIW10PH-1268; ENIW10PH-1269; ENIW10PH-1270; ENIW10PH-1271; ENIW10PH-1272; ENIW10PH-1273; ENIW10PH-1274; ENIW10PH-1275; ENIW11PH-1276; ENIW20C; ENIW27C; ENIW3PH-1225; ENIW3PH-1226; ENIW3PH-1227; ENIW3PH-1228; ENIW4C; ENIW4PH-1230; ENIW4PH-1231; ENIW4PH-1232; ENIW4PH-1233; ENIW4PH-1234; ENIW4PH-1235; ENIW6PH-1237; ENIW6PH-1238; ENIW6PH-1239; ENIW6PH-1240; ENIW6PH-1241; ENIW6PH-1242; ENIW6PH-1243; ENIW6PH-1244; ENIW8PH-1260; ENIW8PH-1261; ENIW8PH-1262; ENIW8PH-1263; ENIW8PH-1264; ENIW8PH-1265; ENIW8PH-1266; ENIWETOK_Operation; Eniwetok Atoll, Central Pacific; Event label; H.M. Smith; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 341 data points
    Location Call Number Expected Availability
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Ericson, D; Morgenstein, M; Grinnell, R (1956): Vema Cruise 10 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 145 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 10 Expedition from June until September 1956 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 95 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; V10; V10-1; V10-11; V10-19; V10-20; V10-21; V10-32; V10-42; V10-50; V10-6; V10-65; V10-72; V10-77; V10-78; V10-80; V10-82; V10-83; V10-88; V10-95; V10-97; V10-99; Vema
    Type: Dataset
    Format: text/tab-separated-values, 254 data points
    Location Call Number Expected Availability
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