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  • 2020-2023  (11,250)
  • 1975-1979  (865,660)
  • 1960-1964  (438,949)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Needleman, Stanley M (1960): Soil science studies at Centrum Sø, northeast Greenland, 1960. Polarforschung, 30(1/2), 33-41, hdl:10013/epic.29211.d001
    Publication Date: 2024-06-10
    Description: During the period May to August 1960, an Air Force scientific field party conducted earth science studies and tested a raised sand terrace, located about 224 km south of Station Nord, Northeast Greenland. The operation staged from Thule Air Force Base was climaxed by successful test Iandings on the terrace by C-119 and C-130 aircraft. Significant data were obtained from related investigations on a typical arctic lake, ice-free soils, meteorology, engineering geology, geomorphology, and electrical resistivity of soils.
    Keywords: 20S-15N; California bearing ratio; Centrum Sø, notheast Greenland; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Geological profile sampling; GEOPRO; Profile ID; Temperature, soil; Thickness; Water content, dry mass
    Type: Dataset
    Format: text/tab-separated-values, 119 data points
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  • 2
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    PANGAEA
    In:  Supplement to: Seibold, Eugen; Dill, Robert F; Walger, Eckart (1961): Tauchbeobachtungen und petrographische Untersuchungen zur Sedimentumlagerung in der Kieler Außenförde. Meyniana, 11, 82-96, https://doi.org/10.2312/meyniana.1961.11.82
    Publication Date: 2024-06-10
    Description: Geological observations, using "free-diving" techniques (Figure I) were made in September, 1960 and March 1961 along two continuous profiles in the outer Kiel Harbor, Germany and at several other spot locations in the Western Baltic Sea. A distinct terrace, cut in Pleistocene glacial till, was found that was covered with varying amounts and types of recent deposits. Hand samples were taken of the sea-floor sediments and grainsize distribution determined for both the sediment as a whole and for its heavy mineral fraction. From the Laboratory and Field observations it was possible to recognize two distinct types of sand; Type I, Sand resulting from transportation over a long period of time and distance and Type 11, Sand resulting from little transportation and found today near to xvhere it was formed. Several criterea related to the agent of movement could be used to classify the nature of the sediment; (1) undisturbed (the sediment Cover of the Pleistocene Terrace is essentially undisturbed), (2) mixed by organisms, (3) transported by water movements (sediment found with ripple marks, etc., and (4) "Scoured" (the movement of individual particles of sediment from around larger boulders causes a slow downward movement or "Creeping" which is due to both the force of gravity and bottom currents. These observations and laboratory studies are discussed concerning their relationship to the formation of residual sediments, the direction of sand transportation, and the intensive erosion on the outer edge of the wave-cut platform found in this part of the Baltic Sea.
    Keywords: buelk; Calculated; Comment; Depth, bathymetric; DEPTH, sediment/rock; DIVER; ECHO; Echosounder; Heavy minerals; off Leuchtturm Bülk, Kieler Bucht, Baltic Sea; Profile ID; Sample ID; Sampling by diver; Sand; Size fraction, statistical value; Smear slide analysis
    Type: Dataset
    Format: text/tab-separated-values, 790 data points
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  • 3
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    PANGAEA
    In:  Scripps Institution of Oceanography, UC San Diego | Supplement to: SCRIPPS Institution of Oceanography (1962): PROA Expedition April-August 1962, list of core and dredge samples, R/V Spencer F. Baird. Scripps Institution of Oceanography, UC San Diego, unpublished, 64 pp, https://www.ngdc.noaa.gov/mgg/curator/data/spencer_f._baird/proa/15065003.pdf
    Publication Date: 2024-05-26
    Description: The cores and dredges described in this report were taken on the PROA Expedition in April 1962 until August 1962 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 180 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Comment; Core; CORE; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; GC; Gravity corer; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Photo/Video; Piston corer; Position; PROA; PROA-009D; PROA-011P; PROA-011PG; PROA-015D; PROA-029D; PROA-063PG; PROA-072D; PROA-079P; PROA-084P; PROA-099P; PROA-101P; PROA-102C1; PROA-102C2; PROA-103V; PROA-105G; PROA-108C; PROA-108P; PROA-108PG; PROA-112P; PROA-113P; PROA-113PG; PROA-113V; PROA-116P; PROA-123G; PROA-137G; PROA-139G; PROA-141G; PROA-147G; PROA-147V; PROA-148G; PROA-150G; PROA-151G; PROA-156G; PROA-157G; PROA-159G; PROA-160G; PROA-161G; PROA-162G; PROA-167G; PROA-168G; PROA-169G; PROA-175G; PROA-PC7; PV; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 467 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Schock, Hans Hartmut (1979): Distribution of rare-earth and other trace elements in magnetites. Chemical Geology, 26(1-2), 119-133, https://doi.org/10.1016/0009-2541(79)90034-2
    Publication Date: 2024-05-15
    Description: Titanomagnetites separated from 15 different rock samples (including ocean-floor basalts from DSDP Legs 37, 45 and 46) were analyzed together with whole-rock samples by instrumental neutron-activation analysis for Sc, Cr, Co, Zn, Hf, Ta, Th and the REE La, Ce, Nd, Sm, Eu, Gd, Tb, Dy, Tm, Yb and Lu. In titanomagnetities from ocean-floor basalts and some other rocks, REE are enriched with respect to the whole-rock composition by factors of between 1.5 and 3 for light REE and between 1.0 and 1.9 for heavy REE; that is, REE with larger ionic radii are preferentially incorporated into the magnetite lattice. Three magnetite samples are REE depleted. Their whole-rock samples contain P in appreciable amounts, so apatite, an important REE-accumulating mineral, could have captured REE to some extent. All titanomagnetites show a marked negative Eu anomaly, this is most probably caused by discrimination of Eu(2+) from the magnetite lattice. Co, Zn, Hf and Ta are significantly enriched in magnetites. The distribution behaviour of Sc and Cr is masked chiefly by the crystallization of clinopyroxene and therefore is not easy to estimate. Ulvöspinel contents of about 70% for the titanomagnetites from ocean-floor basalts were estimated from qualitative microprobe analysis. Ulvöspinel contents of all other samples varied in a wide range from 20% to about 90%. No correlation could be observed between this and the REE contents of the magnetites. Ilmenite exsolution lamellae could only be observed in titanomagnetites from a doleritic basalt from Leg 45.
    Keywords: 37-332A; 37-332B; 45-395A; 46-396B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg37; Leg45; Leg46; North Atlantic/VALLEY
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Hart, Stanley R; Staudigel, Hubert (1978): Oceanic Crust: Age of hydrothermal alteration. Geophysical Research Letters, 5(12), 1009-1012, https://doi.org/10.1029/GL005i012p01009
    Publication Date: 2024-05-15
    Description: Times of vein mineral deposition in the ocean crust have been determined both by Rb-Sr isochron ages of vein smectites and by comparison of 87Sr/86Sr ratios of vein calcites with the known variations of seawater 87Sr/86Sr ratio with time. Results from drilling sites 105, 332B and 418A, Atlantic Ocean, which have basement formation ages of 155 m.y., 3.5 m.y., and 110 m.y., respectively, show that vein deposition is essenrially complete within 5-10 m.y. after formation of the basaltic crust. This provids direct evidence that hydrothermal circulation of sea-water through the oceanic crust is an important process for only 5-10 m.y. after crust formation.
    Keywords: 11-105; 37-332B; 51-417A; 52-418A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg11; Leg37; Leg51; Leg52; North Atlantic/CONT RISE; North Atlantic/HILL; North Atlantic/VALLEY
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Dostal, J; Muecke, G K (1978): Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37. Earth and Planetary Science Letters, 40(3), 415-422, https://doi.org/10.1016/0012-821X(78)90164-4
    Publication Date: 2024-05-15
    Description: REE abundances in gabbros and peridotites from Site 334 of DSDP Leg 37 show that these rocks are cumulates produced by fractional crystallization of a primitive oceanic tholeiite magma. They may be part of a layered oceanic complex. The REE distributions in the residual liquids left after such a fractionation are similar to those of incompatible element-depleted oceanic tholeiites. The REE data indicate that the basalts which overlie the gabbro-peridotite complex, are not genetically related to plutonic rocks.
    Keywords: 37-334; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg37; North Atlantic/BASIN
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: O'Nions, R K; Hamilton, P J; Evensen, N M (1977): Variations in 143Nd/144Nd and 87Sr/86Sr ratios in oceanic basalts. Earth and Planetary Science Letters, 34(1), 13-22, https://doi.org/10.1016/0012-821X(77)90100-5
    Publication Date: 2024-05-15
    Description: 143Nd/144Nd ratios have been determined on 37 samples of oceanic basalt, with a typical precision of +/- 2-3 * 10**-5 (2 sigma). Ocean island and dredged and cored submarine basalts are included for which reliable measurements of 87Sr/86Sr ratios exist in the literature or have been measured as part of this study. A strong negative correlation exists between 143Nd/144Nd and 87Sr/86Sr ratios in basalts from Iceland and the Reykjanes Ridge, but such a clear correlation does not exist for samples from the Hawaiian Islands. However, when other ocean island basalts from the Atlantic are included there is an overall correlation between these two parameters. Increases and decreases in Rb/Sr in oceanic basalt source regions have in general been accompanied by decreases and increases respectively in Sm/Nd ratios. The compatibility of the data with single-stage models is assessed and it is concluded that enrichment and depletion events, which are consistent with transfer of silicate melts, are responsible for the observed variation.
    Keywords: 37-332A; 37-332B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg37; North Atlantic/VALLEY
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Müller, Peter J; Suess, Erwin (1979): Productivity, sedimentation rate, and sedimentary organic matter in the oceans. I.- Organic matter preservation. Deep-Sea Research Part A. Oceanographic Research Papers, 26(12), 1347-1362, https://doi.org/10.1016/0198-0149(79)90003-7
    Publication Date: 2024-05-15
    Description: Comparison of rates of accumulation of organic carbon in surface marine sediments from the central North Pacific, the continental margins off northwest Africa, northwest and southwest America, the Argentine Basin, and the western Baltic Sea with primary production rates suggests that the fraction of primary produced organic carbon preserved in the sediments is universally related to the bulk sedimentation rate. Accordingly, less than 0.01% of the primary production becomes fossilized in slowly accumulating pelagic sediments [(2 to 6 mm (1000 y)**-1] of the Central Pacific, 0.1 to 2% in moderately rapidly accumulating [2 to 13 cm (1000 y)**-1] hemipelagic sediments off northwest Africa, northwest America (Oregon) and southeast America (Argentina), and 11 to 18% in rapidly accumulating [66 to 140 cm (1000 y)**-1] hemipelagic sediments off southwest America (Peru) and in the Baltic Sea. The emiprical expression: %Org-C = (0.0030*R*S**0.30)/(ps(1-Theta)) implies that the sedimentary organic carbon content (% Org-C) doubles with each 10-fold increase in sedimentation rate (S), assuming that other factors remain constant; i.e., primary production (R), porosity and sediment density (ps). This expression also predicts the sedimentary organic carbon content from the primary production rate, sedimentation rate, dry density of solids, and their porosity; it may be used to estimate paleoproductivity as well. Applying this relationship to a sediment core from the continental rise off northwest Africa (Spanish Sahara) suggests that productivity there during interglacial oxygen isotope stages 1 and 5 was about the same as today but was higher by a factor of 2 to 3 during glacial stages 2, 3, and 6.
    Keywords: 12897; 13939; 13947; Accumulation rate, total organic carbon; Atlantic Ocean; Baltic Sea; BC; BCR; Box corer; Box corer (Reineck); Calculated; Calculated, see reference(s); Calculated from mass/volume; Carbon, organic, total; Density, dry bulk; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; Elevation of event; Event label; GIK10127-2; GIK10132-1; GIK10140-1; GIK10141-1; GIK10145-1; GIK10147-1; GIK10175-1; GIK12310-3; GIK12327-4; GIK12328-4; GIK12329-4; GIK12336-1; GIK12337-4; GIK12344-3; GIK12345-4; GIK12347-1; GIK12392-1; GIK13209-2; KAL; KAL15; Kasten corer; Kasten corer 15 cm; Latitude of event; Longitude of event; M12392-1; M25; Meteor (1964); Pacific; PC; Percentage; Peru Continental Margin; Piston corer; Porosity, fractional; Primary production of carbon per area, yearly; Sedimentation rate; V15; V15-141; V15-142; VA-05/4; VA-08/1; VA-10/3; Valdivia (1961); Vema; W7610B-08; W7706; W7706-36; W7706-39; Wecoma
    Type: Dataset
    Format: text/tab-separated-values, 234 data points
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  • 9
    Publication Date: 2024-05-15
    Keywords: ALB-13; ALB-173; ALB-31; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-31; ALBTR-4660; ALBTR-4662; ALBTR-4676; ALBTR-4681; ALBTR-4685; ALBTR-4701; ALBTR-4711; ALBTR-4721; Aluminium; Atomic emission spectroscopy (AES); Barium; Bismuth; Boron; Cadmium; Calcium; Calculated from mass/volume; Calculated from weight loss after ignition at 450 °C; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; CHA-299; CHA-302; Challenger1872; CHIN02BD; CHIN02BD-016G; CHINOOK; CHNK-16G; Chromium; CHUB01BD; CHUB01BD-002G; CHUB01BD-034G; CHUB-2; CHUB-34; CHUB5; CHUBASCO; Cobalt; Copper; Core; CORE; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0ABD-016G; DNWB0ABD-017G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-048G; DNWB0BBD-052G; DNWB0BBD-054G; DNWB0BBD-055G; DNWB0BBD-056G; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-004H; DNWH0BHO-034G; DNWH0DHO-092H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B4; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD1; DWBD2; DWBD4; DWBD5; DWBD7; DWBG147B; DWBG16; DWBG17; DWBG19; DWBG37; DWBG40; DWBG43; DWBG48; DWBG52; DWBG54; DWBG55; DWBG56; DWBG78; DWHD15; DWHD16; DWHD47; DWHD55; DWHD72; DWHG34; DWHH4; DWHH92; Eastern Basin, Pacific Ocean; Epce; Event label; Gallium; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Horizon; Identification; Iron; Lanthanum; Lead; Loss on ignition; Magnesium; Manganese; MDPC02HO-MP-025F-1; MDPC02HO-MP-033D; MDPC03HO-MP-043A; MIDPAC; Molybdenum; MPC-25F-1; MPC-33D; MPC-43A; NAGA; NAGA8C; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; Page(s); Phosphorus; Potassium; Sample code/label; Scandium; Sediment type; Shape; Silicon; Silver; SIO-DX-1; Size; Sodium; Spencer F. Baird; Stranger; Strontium; Thallium; Thorium; Titanium; TRAWL; Trawl net; Uranium; Vanadium; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; VITYAZ4289-TR; Water content, wet mass; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 1930 data points
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  • 10
    Publication Date: 2024-05-15
    Keywords: ALB-31; Albatross (1882-1921); Albatross1899-1900; ALBTR-31; Aluminium; Barium; Boron; Calcium; Calculated from mass/volume; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; Chromium; Cobalt; Copper; Core; CORE; DEPTH, sediment/rock; Description; DNWB0BBD; DNWB0BBD-037G; DNWH0AHO-004H; DOWNWIND-B2; DOWNWIND-H; Dredge; DRG; DWBG37; DWBG78; DWHD55; DWHH4; Epce; Event label; Gallium; GC; Gravity corer; Horizon; Identification; Iron; Lead; Magnesium; Manganese; Molybdenum; NAGA; NAGA8C; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; Phosphorus; Potassium; Sediment type; Shape; Silicon; SIO-DX-1; Size; Sodium; Spencer F. Baird; Stranger; Strontium; Sulfur, total; Thallium; Tin; Titanium; TRAWL; Trawl net; V15; V15-126; Vanadium; Vema; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; Water content, wet mass; X-ray fluorescence (XRF); Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 257 data points
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