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  • Springer Nature  (5,607)
  • PANGAEA
  • 1960-1964  (5,617)
  • 1961  (5,617)
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  • 1960-1964  (5,617)
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  • 1
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    Figures of: Manganese pavements on the Blake Plateau (1961)
    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Details
    Publication Date: 2016-08-25
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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    PAPER (OA)
  • 2
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    PÓZNOGLACJALNA I HOLOCEŃSKA HISTORIA ROŚLINNOŚCI GÓR ŚWIĘTOKRZYSKICH (The History of the Late Glacial and Holocene Vegetation of the Holy Cross Mountains (1961)
    PANGAEA
    In:  EPIC3Polska Akdademia Nauk, Instytut Botaniki, II(2), Bremerhaven, PANGAEA, 56 p.
    Details
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 3
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    O vybore metodiki mineralogicheskogo analiza peschano-alevritovykh fraktsyj morskikh donnykh osadkov (On choice of a method for mineralogical analysis of sandy-aleuritic franctions of marine bottom sediments) (1961)
    PANGAEA
    In:  EPIC3Transactions (Trudy) of the P.P. Shirshov Institute of Oceanology USSR Acad. Sci., 1961. Vol. 50, p., Bremerhaven, PANGAEA, pp. 170-183
    Details
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 4
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    Observation of manganese deposits in the Blake Plateau during Atlantis Cruise 266 (1961)
    PANGAEA
    Details
    Publication Date: 2023-08-28
    Description: Since 1954 the Blake Plateau has interested the geophysical group at Woods HOle. Early cruises gathered data on this region incidental to other work. It became apparent that the area was worthy of more intense study. Questions about the bathymetry and underlying structure had been raised. This is a report of the most recent cruise undertaken to study the northern portion of the Plateau. It is intended to summarize the data collected and to be useful as art aid to investigators in preparation of manuscripts for publication.
    Keywords: A-266/D-2-2; A-266/D-40; A-266/D-41; A-266/D-42; A-266/D-5 (9-12); A-266/R-45; AT26601; AT266-02; AT266-09-12; AT266-11C; AT266-20; AT266-30; AT266-31; AT266-32; AT266-34; AT266-40; AT266-41; AT266-42; AT266-45; AT266-45B; AT266-46; AT266-47; AT266-48; AT266-49; AT266-50; ATL266/45/45; ATL266/46/46; Atlantic Ocean; Atlantis (1931); Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 138 data points
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    DATA PANGAEA
  • 5
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    Annotated record of the detailed examination of Mn deposits recovered from dredges and cores from VEMA 17 Expedition stations (1961)
    PANGAEA
    In:  Supplement to: Hekinian, Roger; Kravitz, J; Bauchelle, D (1961): Vema Cruise 17 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 307 pp
    Details
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the Vema 17 Expedition from December 1960 until October 1961 by the Lamont Geological Observatory, Columbia University from the R/V Vema. An approximate total of 210 cores, dredges and camera stations were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Carribean sea; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Drake Passage; Dredge; DRG; Event label; Gulf of Mexico; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Southern Ocean; Strait of Magellan, Chile; Substrate type; V17; V17-1; V17-10; V17-104; V17-11; V17-12; V17-124; V17-125; V17-126; V17-13; V17-131; V17-134; V17-136; V17-14; V17-144; V17-146; V17-147; V17-15; V17-150; V17-152; V17-153; V17-155; V17-156; V17-16; V17-160; V17-162; V17-163; V17-165; V17-166; V17-17; V17-18; V17-182; V17-186; V17-188; V17-19; V17-192; V17-2; V17-20; V17-21; V17-210; V17-211; V17-22; V17-23; V17-25; V17-26; V17-27; V17-29; V17-29RD; V17-30; V17-31; V17-34; V17-36; V17-37; V17-38; V17-39; V17-40; V17-40SBT; V17-41; V17-41SBT; V17-42SBT; V17-45; V17-46; V17-47; V17-48; V17-49; V17-5; V17-52; V17-54; V17-55; V17-56; V17-57SBT; V17-59SBT; V17-6; V17-61; V17-66; V17-70; V17-8; V17-81SBT; V17-82SBT; V17-83; V17-83SBT; V17-84; V17-84SBT; V17-85SBT; V17-88; V17-89; V17-9; V17-90; V17-92; V17-93; Vema
    Type: Dataset
    Format: text/tab-separated-values, 1884 data points
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    DATA PANGAEA
  • 6
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    Table I. Composition of till in north Greenland (1961)
    PANGAEA
    In:  Supplement to: Davies, William E (1961): Glacial Geology of Northern Greenland. Polarforschung, 31(1/2), 94-103, hdl:10013/epic.29222.d001
    Details
    Publication Date: 2023-09-29
    Description: From 1950 through 1900 studies on the glacial geology of northern Greenland have been made in cooperation with the U.S. Air Force Cambridge Research Laboratories. As a result of these studies four distinct phases of the latest glaciation have been recognized. The last glaciation extended over most of the land and removed traces of previous anes. Retreat of the ice mass began some time previous to 6000 years ago. This was followed by a rtse in sea level which deposited clay-silt succeeded by karne gravels around stagnant ice lobes in the large valleys. Marine terraces, up to 129 meters above present sea level, developed as readjustment occurred in the land free of ice. About 3700 years ago an advance of glaciers down major fjords took place followed by retreat to approximately the present position of the ice. Till in Peary Land, north of Frederick E. Hyde Fjord, contains only locally derived matertals indicating that the central Greenland ice cap did not cover the area.
    Keywords: Andesite; Area/locality; Basalt; Diabase; Felsitic fragments; Gneiss; Granite; Greenstone; LATITUDE; Limestone; LONGITUDE; Marble; Phyllite; Quartz; Quartzite; Sandstone; Schist; Shale; Slate
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 7
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    (Table 3, page 264), Composition of a manganese micronodule found in a fossil red clay bed from Western Timor (1961)
    PANGAEA
    In:  Supplement to: El Wakeel, S K; Riley, J P (1961): Chemical and mineralogical studies of fossil red clays from Timor. Geochimica et Cosmochimica Acta, 24(3-4), 260-265, https://doi.org/10.1016/0016-7037(61)90021-7
    Details
    Publication Date: 2023-08-28
    Description: Chemical analyses are presented for two Cretaceous clays from Noil Tobee, Timor. Mineralogical examination has shown that they consist principally of quartz, feldspar, illite and chlorite, together with minor amounts of montmorillonite. Both chemically and mineralogically the clays are very similar to the recent argillaceous deep-sea sediments of the Pacific and Indian Oceans, which confirms Molengraaff's theory (1921) that they are of deep-sea origin. Further confirmation of this theory is provided by comparison of the composition of micromanganese nodules, separated from one of these clays, with that of manganese nodules from the Pacific Ocean.
    Keywords: Aluminium oxide; Barium oxide; Calcium oxide; Carbon dioxide; Cobalt oxide; Copper(II) oxide; DEPTH, sediment/rock; Description; Flame photometry; Gallium oxide; Identification; Iron oxide, Fe2O3; Lead oxide; Magnesium oxide; Manganese oxide; Molybdenum trioxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Noil_Tobee_M; Noni river, Timor; Oxygen, gas; Phosphorus pentoxide; Potassium oxide; Silicon dioxide; Sodium oxide; Spectrophotometric; Strontium oxide; Tin dioxide; Titanium dioxide; Vanadium oxide; Water in rock; Wet chemistry; Zinc oxide; Zirconium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
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  • 8
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    (Fig 1, page 350) A manganese nodule in the top part of the CHUBASCO station 17 core taken in the Pacific Ocean (1961)
    PANGAEA
    In:  Supplement to: Bramlette, M (1961): Pelagic sediments. in: Invited Lectures Presented at the International Oceanographic Congress Held in New York, 31 August-12 September 1959. Presented at the International Oceanographic Congress, 1959, American Association for the Advancement of Science, New York, U.S.A., 345-366, https://archive.org/details/oceanographyinvi00inte
    Details
    Publication Date: 2023-08-28
    Description: The vast extent of pelagic deposits, covering about 70 per cent of the ocean floor, thus about half of the earth, makes them of obvious importance to all Earth Science. All the pelagic (eupelagic) sediments, whether largely of plankton remains or fine inorganic particles, have certain distinctive characteristics to reflect their environment of accumulation. The great segregation of manganese in pelagic sediments presents many problems. It is hypothesized that in the formation of present day nodules a relatively slow accumulation in order to permit deposition of more of the manganese as large nodules, rather than as the disseminated micronodules that are in larger proportion in the Tertiary.
    Keywords: CHUB01BD; CHUB01BD-017G; CHUB-17; CHUBASCO; Comment; Core; CORE; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Spencer F. Baird; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 9
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    Annotated record of the detailed examination of Mn deposits from MONSOON Expedition stations (1961)
    PANGAEA
    Details
    Publication Date: 2023-08-28
    Keywords: Argo; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; Identification; Java Sea; Latitude of event; Longitude of event; Method/Device of event; MONS01AR-007P; MONS01AR-012G; MONS01AR-MONS08AR; MONS02AR-001D; MONS02AR-030D; MONS02AR-030G; MONS06AR-074D; MONS06AR-085G; MONS06AR-086SG; MONS06AR-091G; MONS06AR-098P; MONS07AR-110D; MONS07AR-116P; MONS07AR-121G; MONS07AR-123G; MONS07AR-125G; MONS08AR-139D; MONS08AR-143P; MONS08AR-150G; MONS08AR-151PG; MONS08AR-157G; MONSOON; MSN-01D; MSN-07G; MSN-07P; MSN-08G; MSN-10G; MSN-110D; MSN-116P; MSN-11G; MSN-121G; MSN-122G; MSN-123G; MSN-125G; MSN-126G; MSN-127G; MSN-128; MSN-128G; MSN-12G; MSN-132; MSN-135P; MSN-139D; MSN-140; MSN-143P; MSN-148G; MSN-148V; MSN-150G; MSN-151PG; MSN-152; MSN-153P; MSN-156V; MSN-157G; MSN-157V; MSN-16; MSN-17G; MSN-18G; MSN-19G; MSN-20; MSN-21G; MSN-30D; MSN-30G; MSN-47G; MSN 6-2; MSN 6-25; MSN-62G; MSN-68G; MSN-74D; MSN 8-1; MSN 8-11; MSN 8-19; MSN 8-24; MSN 8-29; MSN 8-31; MSN 8-5; MSN-85G; MSN-86SG; MSN-87; MSN-90G; MSN-91G; MSN-98P; MSN-98V; MSN G; MSN H; MSNK; MSN P; MSN Q; MSN S; MSN U; MSN W; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 576 data points
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  • 10
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    (Table 1, page 1376) Chemical analyses of manganese nodules and crusts from the Pacific Ocean (1961)
    PANGAEA
    In:  Supplement to: Mero, John L (1961): Sea floor manganese nodules. Unpublished report to the Daniel C. Jackling Award Fellowship Committee; American Institute of Mining, Metallurgical, and Petroleum Engineers (AIME), https://www.ngdc.noaa.gov/mgg/geology/data/1599/15995009/15995009.pdf
    Details
    Publication Date: 2023-08-28
    Description: A compilation of chemical analyses of Pacific Ocean nodules using an x-ray fluorescence technique. The equipment used was a General Electric XRD-5 with a tungsten tube. Lithium fluoride was used as the diffraction element in assaying for all elements above calcium in the atomic table and EDDT was used in conjunction with a helium path for all elements with an atomic number less than calcium. Flow counters were used in conjunction with a pulse height analyzer to eliminate x-ray lines of different but integral orders in gathering count data. The stability of the equipment was found to be excellent by the author. The equipment was calibrated by the use of standard ores made from pure oxide forms of the elements in the nodules and carefully mixed in proportion to the amounts of these elements generally found in the manganese nodules. Chemically analyzed standards of the nodules themselves were also used. As a final check, a known amount of the element in question was added to selected samples of the nodules and careful counts were taken on these samples before and after the addition of the extra amount of the element. The method involved the determination and subsequent use of absorption and activation factors for the lines of the various elements. All the absorption and activation factors were carefully determined using the standard ores. The chemically analyzed samples of the nodules by these methods yielded an accuracy to at least three significant figures.
    Keywords: 248; Acapulco Trench, Pacific ocean; ALB-13; ALB-173; ALB-2; ALB-31; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; Albatross IV (1963); ALBTR-13; ALBTR-173; ALBTR-2; ALBTR-31; ALBTR-4622; ALBTR-4656; ALBTR-4658; ALBTR-4660; ALBTR-4662; ALBTR-4676; ALBTR-4681; ALBTR-4685; ALBTR-4701; ALBTR-4711; ALBTR-4721; Aluminium; Argo; B1 VS-78; Barium; Calcium; Calculated from weight loss after ignition at 450 °C; CAP-50BG-1; CAPB01BD-050BG-01; CAPRICORN-B; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; CHA-248; CHA-252; CHA-276; CHA-285; CHA-289; CHA-299; CHA-302; Challenger1872; CHUB01BD; CHUB01BD-001G; CHUB01BD-002G; CHUB01BD-003G; CHUB01BD-009G; CHUB01BD-017G; CHUB01BD-019G; CHUB01BD-039G; CHUB-1; CHUB-11G; CHUB-17; CHUB-19; CHUB-2; CHUB-3; CHUB-39; CHUB5; CHUB-7G; CHUB-9; CHUBASCO; Cobalt; Copper; Core; CORE; core_48; CRU9121; CUSP1954; CUSP8P; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0ABD-017G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-048G; DNWB0BBD-054G; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-004H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B4; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD1; DWBD2; DWBD4; DWBD7; DWBG147B; DWBG17; DWBG19; DWBG37; DWBG40; DWBG43; DWBG48; DWBG54; DWBG78; DWHD15; DWHD16; DWHD47; DWHD55; DWHD72; DWHH4; Epce; Event label; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Henderson Seamount, Pacific Ocean; Horizon; Identification; Iron; Lead; Loss on ignition; Manganese; MDPC01HO-005-02; MDPC02HO-032; MDPC02HO-MP-025F-2; MDPC02HO-MP-026A-3; MDPC02HO-MP-033K; MDPC02HO-MP-037A; MDPC03HO-MP-043D; MIDPAC; Molybdenum; Monegasque Trawl; MONS01AR-MONS08AR; MONS08AR-139D; MONSOON; MPC-25F-2; MPC-26A-3; MPC-32; MPC-33K; MPC-37A; MPC-43D; MPC-5-2; MSN-07G; MSN-10G; MSN-11G; MSN-139D; MSN-17G; MSN-18G; MSN G; MSNK; MSN Q; MSN S; MTRW; NEL-HEND; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NODC-0418; North-East Pacific Ocean; Northern_Holiday; North Pacific Ocean; Northwest Pacific Ocean; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Page(s); PAS-19121; Phosphorus; Potassium; Sample code/label; SDSE_073; Sediment type; Silicon; Size; SOB; SOB-005D; SOB-010D; SOB-013D; SOB-020D; SOB-022D; SOB-025D; SOB-027D; SOBO03BD-005D; SOBO03BD-010D; SOBO03BD-013D; SOBO04BD-020D; SOBO04BD-022D; SOBO04BD-025D; SOBO04BD-027D; Southern Borderland; Specific gravity; Spencer F. Baird; Strontium; SwedishDeepSeaExpedition; Titanium; TRANS_14C; TRANS_14D; TRAWL; Trawl net; UNK_BH2; UNK_MS; VERMILION_SEA; Vermilion Sea, Pacific Ocean; Vityaz (ex-Mars); Vityaz-29; VITYAZ4191-TR; VITYAZ4199-TR; VITYAZ4217-TR; VITYAZ4221-TR; VS BII-35; VSS35D; VSS78D; Water in rock; WIG-6; WIGWAM; Wired profile sonde; WP; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 2243 data points
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