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  • National Academy of Sciences  (2,741)
  • PANGAEA
  • 2025-2025
  • 2010-2014
  • 2005-2009
  • 1980-1984  (1,802)
  • 1975-1979  (1,189)
  • 1950-1954
  • 1981  (1,802)
  • 1976  (1,189)
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  • 2025-2025
  • 2010-2014
  • 2005-2009
  • 1980-1984  (1,802)
  • 1975-1979  (1,189)
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  • 1
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    PANGAEA
    In:  EPIC3Neue Ausgarbungen und Forschungen in Niedersachsen, Bremerhaven, PANGAEA, 10, pp. 197-224
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 2
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    PANGAEA
    In:  EPIC3Nauka, Moscow, Bremerhaven, PANGAEA, 296 p.
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 3
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    PANGAEA
    In:  EPIC3Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, Bremerhaven, PANGAEA, 80, 118 p.
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 4
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 5
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2015-07-15
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 6
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2016-02-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 7
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    PANGAEA
    In:  EPIC3"Meteor" Forschungs-Ergebnisse, C, Bremerhaven, PANGAEA, 35, pp. 23-59
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 8
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    PANGAEA
    In:  EPIC3Offa, Berichte und Mitteilungen zur Urgeschichte, Frühgeschichte und Mittelalterarchäologie, Bremerhaven, PANGAEA, 38, pp. 365-376
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
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  • 9
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 10
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 11
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 12
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    PANGAEA
    In:  EPIC3A rapid and sensitive method for the quantitation of microgram quantities of protein utilizing the principle of protein-dye binding. Analytical Biochemistry, 72(1-2), 248-254, doi:10.1016/0003-2697(76), Bremerhaven, PANGAEA, pp. 90527-3
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 13
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
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  • 14
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    PANGAEA
    In:  EPIC3Probleme der Küstenforschung im südlichen Nordseegebiet, Bremerhaven, PANGAEA, 11, pp. 101-118
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 15
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    PANGAEA
    In:  Supplement to: Seifert, Karl E; Vallier, Tracy L; Windom, Kenneth E; Morgan, S R (1981): Geochemistry and petrology of igneous rocks, Deep Sea Drilling Project Leg 62. In: Thiede, J; Vallier, TL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 62, 945-953, https://doi.org/10.2973/dsdp.proc.62.149.1981
    Publication Date: 2023-07-10
    Description: Igneous rocks were recovered from three sites on Hess Rise during Deep Sea Drilling Project Leg 62: altered basalt at Site 464, at the northern end of Hess Rise; and altered trachyte from Site 465, and rounded basalt pebbles in upper Albian to middle Miocene sediments from Site 466, both at the southern end of Hess Rise. Major-, minor-, and trace-element data for basalt from Hole 464 are consistent with these rocks being transitional tholeiites that have undergone low-temperature alteration by reaction with sea water. Trachyte from Hole 465A exhibits as many as three generations of plagioclase along with potash feldspar that are flow aligned in groundmasses alterted to smectites and random mixed-layer clays. Textural evidence indicates that these rocks were eruped subaerially. Chemical data show a range of values when plotted on two- and three-component variation diagrams. The observed variations may result in part from differentiation, but they also reflect the high degree of alteration. Several oxides and elements show strong correlation with H2O+: K2O, SiO2, Rb and Lu decrease and MgO increases with increasing H2O+. These trends, except for that of Lu, are consistent with experimentally determined changes in chemistry that accompany alteration. The trend for Lu has not been previously reported; it may result from a more-intense alteration of the HREE-rich mafic minerals than of the LREE-rich feldspars. Despite their alteration, the trachytes compare favorably with alkalic differentiates from oceanic islands. We interpret Hess Rise as a volcanic platform formed by eruption of off-ridge volcanic rocks onto MORB oceanic crust during the Aptian and Albian stages, after the basement had migrated away from the spreading center. By analogy with present oceanic islands, we propose that early tholeiitic basalts were followed by alkalic basalts and their differentiation products (trachytes), producing a volcanic archipelago of islands and seamounts. Subsequent tectonism and subsidence led to the present state of Hess Rise.
    Keywords: 62-464; 62-465A; Aluminium oxide; Barium; Calcium oxide; Carbon dioxide; Cerium; Cobalt; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Europium; Event label; Glomar Challenger; Hafnium; Instrumental neutron activation analysis (INAA); Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Leg62; Lutetium; Magnesium oxide; Manganese oxide; North Pacific/CONT RISE; Phosphorus pentoxide; Potassium oxide; Rubidium; Samarium; Sample code/label; Sample ID; Scandium; Silicon dioxide; Sodium oxide; Strontium; Tantalum; Terbium; Thorium; Titanium dioxide; Total; Water in rock; X-ray fluorescence (XRF); Ytterbium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 702 data points
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  • 16
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    PANGAEA
    In:  Supplement to: Seifert, Karl E (1981): Geochemistry of Nauru Basin basalts from the lower portion of Hole 462A, Deep Sea Drilling Project Leg 61. In: Larson, RL; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 61, 705-708, https://doi.org/10.2973/dsdp.proc.61.129.1981
    Publication Date: 2023-07-10
    Description: Atomic-absorption spectrophotometry and instrumental neutron activation analysis were used to determine concentrations of SiO2, Al2O3, FeOt, MgO, CaO, Na2O, K2O, MnO, La, Ce, Sm, Eu, Tb, Yb, Lu, Sc, Co, Cr, Th, Hf, and Ta for 14 basalt samples from the lower portion of Hole 462A in the Nauru Basin. The basalts are similar to normal midocean ridge basalt (MORB) for the elements analyzed, and light rare-earth elements (LREE) are depleted relative to heavy rare-earth elements (HREE). Two samples are extensively altered to smectites and show significant reductions in Al2O3, CaO, MnO, Na2O, REE, Sc, Co, and Hf and gains in MgO and FeOt relative to unaltered samples. The increase in MgO and decrease in CaO indicate that alteration was caused by hydrothermal solutions.
    Keywords: 61-462A; Aluminium oxide; Atomic absorption spectrometry (AAS); Calcium oxide; Cerium; Chromium; Cobalt; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Europium; Glomar Challenger; Hafnium; Instrumental neutron activation analysis (INAA); Iron oxide, FeO; Lanthanum; Leg61; Lutetium; Magnesium oxide; Manganese oxide; Potassium oxide; Samarium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; Tantalum; Terbium; Thorium; Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 317 data points
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  • 17
    Publication Date: 2023-07-10
    Keywords: A150/180; A180-73; Atlantic Ocean; Atlantische Kuppenfahrten 1967/1-3; BC; BCR; Box corer; Box corer (Reineck); Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; Elevation of event; Event label; GIK12309-2; GIK12310-4; GIK12328-5; GIK12329-6; GIK12331-4; GIK12345-5; GIK12347-2; GIK12379-3; GIK12392-1; GIK13207-3; GIK13209-2; GIK13289-1; Grain size, mean radius; KAL; Kasten corer; KOL; Latitude of event; Longitude of event; M12392-1; M25; M8; M8_017-1; M8/17-1; Meteor (1964); off NW Africa; PC; Piston corer; Piston corer (Kiel type); Size fraction 〉 0.006 mm, silt; South Atlantic Ocean; SP8-4; SPC; Sphincter corer; V10; V10-83; V16; V16-20; V19; V19-303; V22; V22-197; V23; V23-100; V23-91; V25; V25-44; V26; V26-41; V27; V27-178; V31; V31-2; V32; V32-31; VA-10/3; Valdivia (1961); Vema
    Type: Dataset
    Format: text/tab-separated-values, 103 data points
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  • 18
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    PANGAEA
    In:  Supplement to: Vinogradov, Mikhail E; Shushkina, Elvira A; Kukina, Irina N (1976): Functional characteristics of a planktonic community in an equatorial upwelling region. Oceanology, 16, 67-76
    Publication Date: 2023-07-09
    Description: An analysis was made of composition and content of nutrients, salts, particulate and dissolved organic matter, and various plankton groups in a series of samples collected by a 140-liter sampling bottle to depth up to 150 m at 4 equatorial stations between 97° and 154°W. Large and small phytoplankton, bacteria (aggregated and dispersed), heterotrophic flagellates, infusorians, radiolarians, foraminifers, fine filter-feeders, small and large, mostly herbivorous copepods, cyclopoids, predatory calanoids, and other predators were investigated separately. Trophic relations between these elements are established from personal and published data, and rate of their metabolism and some other physiological parameters are determined. Such functional characteristics as extent of satisfaction of food requirements of organisms belonging to various trophic groups, intensity of trophic relations, balance between production and consumption by individual elements of the community, ecological efficiency, and net and specific production of the groups distinguished, of individual trophic levels, of total zooplankton, and of the community as a whole are calculated. Variations of these characteristics along the equator with decreasing upwelling intensity are examined and their possible causes and mechanisms are discussed.
    Keywords: AK17-1454; AK17-1456; AK17-1458; AK17-1461; Archive of Ocean Data; ARCOD; Bacteria, biomass per area, as energy; Calanoides, biomass per area, as energy; Calculated; Carnivorous animals, biomass per area, as energy; Copepoda, biomass per area, as energy; Cyclopoida, biomass per area, as energy; Date/Time of event; Depth, bottom/max; Depth, top/min; DEPTH, water; Equatorial Pacific; Event label; Filter feeder, biomass per area, as energy; Flagellates, biomass per area, as energy; Infusorians, biomass per area, as energy; Latitude of event; Longitude of event; Nonpredatory animals, biomass per area, as energy; Phytoplankton, biomass per area, as energy; PLA; Plankton, biomass per area, as energy; Plankton net; Predators, biomass per area, as energy; Protozoa; Protozoa, biomass per area, as energy; Radiolarians, biomass per area, as energy; Zooplankton, biomass per area, as energy
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
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  • 19
    Publication Date: 2023-07-07
    Keywords: 52-418A; Aluminium oxide; Calcium oxide; Clinopyroxene; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron oxide, FeO; Leg52; Magnesium oxide; Matrix; North Atlantic/CONT RISE; Olivine; Plagioclase; Potassium oxide; Sample code/label; Sample method; Silicon dioxide; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 20
    Publication Date: 2023-07-07
    Keywords: 51-417D; Aluminium oxide; Calcium oxide; Clinopyroxene; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron oxide, FeO; Leg51; Magnesium oxide; Matrix; North Atlantic/CONT RISE; Olivine; Plagioclase; Potassium oxide; Sample code/label; Sample method; Silicon dioxide; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
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  • 21
    Publication Date: 2023-07-07
    Keywords: 53-418A; Aluminium oxide; Calcium oxide; Clinopyroxene; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron oxide, FeO; Leg53; Magnesium oxide; Matrix; Olivine; Plagioclase; Potassium oxide; Sample code/label; Sample method; Silicon dioxide; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 166 data points
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  • 22
    Publication Date: 2023-07-10
    Keywords: 61-462; 61-462A; Deep Sea Drilling Project; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Leg61; Sample code/label; Sand; Silt; Size fraction 〈 0.002 mm, clay; Wet sieve shaker
    Type: Dataset
    Format: text/tab-separated-values, 305 data points
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  • 23
    Publication Date: 2023-07-10
    Keywords: 62-463; Acaeniotyle diaphorogona; Acaeniotyle umbilicata; Acanthocircus carinatus; Acanthocircus dicranacanthos; Acanthocircus sp.; Acanthocircus trizonalis; Alievum antiguum; Alievum helenae; Amphibrachium hastatum; Amphipyndax mediocris; Archaeodictyomitra apiarium; Archaeodictyomitra brouweri alfa; Archaeodictyomitra lacrimula; Archaeodictyomitra nuda; Archaeodictyomitra pseudoscalaris; Archaeodictyomitra puga; Archaeodictyomitra vulgaris; Archaeospongoprunum cortinaensis; Archeospongoprunum tehamaensis; Archicapsa similis; Conosphaera tuberosa; Crolanium pythiae; Cromyodruppa concentrica; Crucella sp.; Cryptamphorella challengeri; Cryptamphorella conara; Cryptamphorella dumitricai; Cyclastrum infundibuliforme; Cyrtocalpis operosa; Cyrtocapsa asseni var. alpha; Cyrtocapsa grutterinki; Cyrtocapsa houwi; Deep Sea Drilling Project; Diacanthocapsa boersmae; Dibolachras tytthopora; Dicroa sp.; Dictyophimus gracilis; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Eucyrtidium thiensis; Eucyrtis columbaria; Eucyrtis elido; Eucyrtis molengraaffi; Eucyrtis sp.; Eucyrtis tenuis; Glomar Challenger; Gongylothorax baumgartneri; Gongylothorax verbeeki; Hagistrum euganeum; Hagistrum subacutum; Hemicryptocapsa sp.; Hemicryptocapsa vincentae; Hexalonche sp.; Hexastylus magnificus; Hexinastrum cretaceum; Higumastra sp.; Holocryptocanium barbui; Holocryptocapsa hindei; Homoeoparonaella tricuspidata; Hsuum sp.; Leg62; Lithocampe chenodes; Lithocampe pseudochrysalis var. alpha; Lithomitra pseudopinguis; Lophophaena sp.; Neosciadiocapsa sp.; North Pacific/SEAMOUNT; Paronaella diamphidia; Paronaella sp.; Parvicingula boesii; Parvicingula hsui; Parvicingula malleola; Parvicingula sp.; Pentasphaera longispina; Podobursa triacantha; Podobursa tricola; Pseudoaulophacus excavatus; Pseudoaulophacus sulcatus; Pseudodictyomitra blabla; Pseudodictyomitra carpatica; Pseudodictyomitra lanceloti; Pseudodictyomitra leptoconica; Pseudodictyomitra lilyae; Radiolarian preservation; Radiolarians abundance; Saitoum cepeki; Sample code/label; see reference(s); Sethocapsa orca; Sethocapsa trachyostraca; Sethocapsa uterculus; Siphocampium davidi; Siphocampium macropora; Siphocampium rutteni; Solenotryma sp.; Sphaeropyle thirencis; Sphaerostylus lanceola; Spongobrachium sp.; Spongocyclia trachodes; Spongodiscus misele; Spongopyle ecleptos; Spongosaturnalis horridus; Staurocyclia martini; Staurosphaera septemporata; Stephanastrum inflexum; Stichocapsa cribrata; Stichocapsa decora; Stichocapsa pseudodecora; Stichocapsa pseudopentacola; Stichocapsa sp.; Stichomitra asymbatos; Stylochlamyum sp.; Stylosphaera macrostyla; Thanaria pulchra; Thanarla karpoffae; Theocapsa laevis; Theocorys antiqua; Theocorys renzae; Triactoma hybum; Tripocalpis ellyae; Tripocyclia trigonum; Ultranapora durhami; Ultranapora spinifera; Williriedellum carpathicum; Williriedellum gilkeyi; Williriedellum petershmittae; Xitus alievi; Xitus sp.; Xitus sp. cf. X. spicularius; Xitus spicularius; Xitus vermiculatus
    Type: Dataset
    Format: text/tab-separated-values, 2901 data points
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  • 24
    Publication Date: 2023-07-10
    Keywords: 62-465A; Antimony; Antimony, standard deviation; Arsenic; Arsenic, standard deviation; Chromium; Chromium, standard deviation; Cobalt; Cobalt, standard deviation; Comment; Copper; Copper, standard deviation; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analysis, neutron activation (NAA); Glomar Challenger; Leg62; Molybdenum; Molybdenum, standard deviation; Nickel; Nickel, standard deviation; North Pacific/CONT RISE; Sample, optional label/labor no; Sample code/label; Sample ID; Tantalum; Tantalum, standard deviation; Zinc; Zinc, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 206 data points
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  • 25
    Publication Date: 2023-07-10
    Keywords: 62-464; Axopodorhabdus albianus; Biscutum constans; Chiastozygus litterarius; Cretarhabdus conicus; Cretarhabdus crenulatus; Cretarhabdus loriei; Cribrosphaerella ehrenbergii; Cruciellipsis chiastia; Cyclagelosphaera margerelii; Deep Sea Drilling Project; Discorhabdus ignotus; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Eiffellithus turriseiffelii; Etching index; Gaarderella cf. granulifera; Gephyrorhabdus coronadventis; Glomar Challenger; Leg62; Light microscope; Lithastrinus floralis; Lithraphidites carniolensis; Manivitella pemmatoidea; Nannofossils; Nannofossil zone; North Pacific/CONT RISE; Overgrowth index; Parhabdolithus angustus; Parhabdolithus asper; Parhabdolithus embergeri; Parhabdolithus splendens; Parhabdolithus swinnertonii; Prediscosphaera cretacea; Rucinolithus irregularis; Rucinolithus sp.; Sample code/label; Sollasites horticus; Stephanolithion laffittei; Tegumentum stradneri; Tranolithus orionatus; Vagalapilla compacta; Watznaueria barnesae; Watznaueria biporta; Watznaueria britannica; Watznaueria oblonga; Watznaueria ovata; Watznaueria supracretacea; Zygodiscus diplogrammus; Zygodiscus elegans; Zygodiscus erectus
    Type: Dataset
    Format: text/tab-separated-values, 215 data points
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  • 26
    Publication Date: 2023-07-10
    Keywords: 61-462; 61-462A; Calcium carbonate; Calculated, see reference(s); Carbon, organic, total; Carbon, total; Deep Sea Drilling Project; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO WR-12; Event label; Glomar Challenger; Leg61; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 325 data points
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  • 27
    Publication Date: 2023-07-10
    Keywords: 59-447A; 59-448; 59-448A; 59-449; 59-450; 59-451; Aluminium oxide; Barium; Caesium; Calcium oxide; Cerium; Chromium; Cobalt; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analysis, neutron activation (NAA); Elevation of event; Europium; Event label; Gallium; Glomar Challenger; Hafnium; Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Latitude of event; Leg59; Location; Longitude of event; Magnesium number; Magnesium oxide; Manganese oxide; Nickel; North Pacific/BASIN; North Pacific/Philippine Sea/BASIN; North Pacific/Philippine Sea/RIDGE; North Pacific/RIDGE; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample, optional label/labor no; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; Strontium; Tantalum; Terbium; Thorium; Titanium dioxide; Total; Uranium; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 623 data points
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  • 28
    Publication Date: 2023-07-07
    Keywords: 63-469; 63-470A; 63-472; 63-472A; 63-473; CIPW Norm; Clinopyroxene; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Groundmass; Latitude of event; Leg63; Longitude of event; North Pacific/ABYSSAL FLOOR; North Pacific/ESCARPMENT; North Pacific/Gulf of California/CONT RISE; North Pacific/PLATEAU; Olivine; Plagioclase; Sample code/label; Spinel
    Type: Dataset
    Format: text/tab-separated-values, 61 data points
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  • 29
    Publication Date: 2023-07-07
    Keywords: 59-448; 59-448A; Clinopyroxene; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Leg59; Lithologic unit/sequence; North Pacific/Philippine Sea/RIDGE; Number; Olivine; Orthopyroxene; Plagioclase; Texture; Thickness; Type
    Type: Dataset
    Format: text/tab-separated-values, 250 data points
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  • 30
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    PANGAEA
    In:  Supplement to: Boyce, Robert E (1981): Electrical resistivity, sound velocity, thermal conductivity, density-porosity, and temperature, obtained by laboratory techniques and Well Logs: Site 462 in the Nauru Basin of the Pacific Ocean. In: Larson, RL; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 61, 743-761, https://doi.org/10.2973/dsdp.proc.61.133.1981
    Publication Date: 2023-07-12
    Description: At Deep Sea Drilling Project (DSDP) Site 462, from mudline to 447 meters below the sea floor, Cenozoic nannofossil oozes and chalks have acoustic anisotropies such that horizontal sonic velocities are 0 to 2.5% faster than those in the vertical direction. In laminated chalk, anisotropy of 5% is typical, and in limestones, radiolarian oozes, porcellanites, and cherts, the anisotropies range from 4 to 13%. Middle Maestrichtian volcaniclastics from 447 meters to 560 meters below the sea floor have an acoustic anisotropy of 2 to 32%; 4 to 13% is typical. Basalt flows and sills occur between 560 meters and 1068 meters, and have no apparent anisotropy, but minor interbedded volcaniclastics have anisotropies from 0 to 20% (5% is typical). These volcaniclastics frequently have very small anisotropies, however, compared with the volcaniclastic sequence above the basalt section. Data in cross-plots of the laboratory-measured compressional sound velocity versus wet-bulk density, wet-water content, and porosity of sediments and sedimentary rock typically lie between the equations derived by Wyllie et al. (1956) and Wood (1941); the Wyllie et al. (1956) equation has a fair fit with similar basalt velocity cross-plots. Crossplots of thermal conductivity and sound velocity indicate only a fair correlation. Cross-plots of thermal conductivity versus porosity, wet-water content, and wet-bulk density correlate well with equations derived by Maxwell (1904), Ratcliff (1960), Parasnis (1960), and Bullard and Day (1961). Electrical formation factor versus porosity for sediments and sedimentary rock agrees with the Archie (1942) equation, with m values of 2.6; for basalt, an m of about 2.1 is typical. Basalt pore-water resistivities do not appear to be greatly different from sea water. Formation factors are greater than those derived from equations in Maxwell (1904), Winsauer et al. (1952), Boyce (1968), and Kermabon et al. (1969). An "apparent interstitial water resistivity" (Rwa) curve was derived from the density and induction logs. This Rwa curve indicated an anomaly, at 393.5 to 396.5 meters, which could be interpreted as (1) 76% hydrocarbons, (2) relatively fresh pore water (1.8 per mil salinity), or (3) low-grain-density (2.2 g/cm**3) semi-lithified porcellanite-chert. Porcellanite-chert is the most plausible interpretation. In situ temperatures measured by the Uyeda temperature probe were about 2 to 5°C (50%) higher than the equilibrium temperature (Lachenbruch and Brewer, 1959) extrapolated from two Gearhart-Owen continuous temperature logs; this discrepancy probably arises because the hole was washed out in this depth interval, so these extrapolated temperatures are probably not reliable. If one ignores all precautions as to temperature artifacts, then the equilibrium temperatures of the Gearhart-Owen temperature logs suggest that hydrothermal circulation is occurring in at least the upper 40 meters of the basalt section and heat is transferred by convection and not conduction. Hydrothermal circulation is probably not indicated, however, and the temperature anomalies probably result from excessive artificial cooling of the fractured basalt zones by circulation of water during drilling.
    Keywords: 61-462; Deep Sea Drilling Project; Density, wet bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Formation factor; Gamma ray; Gamma-ray attenuation porosity evaluator (GRAPE); Glomar Challenger; Hole Diameter; Leg61; Lithology/composition/facies; Porosity; Porosity, fractional; Pressure; Resistivity, electrical; Salinity; Sample ID; see reference(s); Temperature, in rock/sediment
    Type: Dataset
    Format: text/tab-separated-values, 200 data points
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  • 31
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    In:  Geological Institute, Russian Academy of Sciences, Moscow | Supplement to: Lisitzina, Nadezhda A; Butuzova, Galina Yu (1976): Zeolites in sediments of the lithological profile across the Pacific Ocean. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 11(2), 9-21
    Publication Date: 2023-07-11
    Description: Results of petrographic, chemical and X-ray studies of zeolites in sediments in the Transpacific lithological profile from the coast of Japan to the coast of Mexico are reported. For ocean phillipsites constancy of Si/Al ratio (2.44-2.87) and unstable cation composition in quantitative predominance of potassium over sodium are characteristic. Two groups of ocean phillipsites are distinguished: of deep-water basins and of submarine rises. The first spread over broad areas of the pelagic zone, and are formed by diagenetic transformation of fine dispersed pyroclastic material in minimum sedimentation rates, the latter occur locally - in areas of basaltic volcanism manifestations.
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Barium oxide; Calcium oxide; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM9; DM9-612; DM9-643; Dmitry Mendeleev; Elevation of event; Event label; GC; Gravity corer; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Northeast Pacific; Northwestern Basin, Pacific Ocean; Northwest Pacific; OKEAN; Okean Grab; Phosphorus pentoxide; Potassium oxide; Ratio; Silicon/Aluminium ratio; Silicon dioxide; Size fraction; Sodium oxide; Sum; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ4362-GR-1; VITYAZ6176-GC; VITYAZ6177-GR; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 32
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    PANGAEA
    In:  Supplement to: Meyer, Klaus-Dieter (1981): Die rote Gesteinsscholle von Schobüll bei Husum (Schleswig-Holstein) - Rotliegendes oder Old Red? Meyniana, 33, 1-7, https://doi.org/10.2312/meyniana.1981.33.1
    Publication Date: 2023-07-11
    Description: The stratigraphic position of the glacially transported 'Scholle' (large-size erratic block) at Schobüll near Husum (Schleswig-Holstein) is now considered to be Devonian rather than 'Rotliegendes'. The 'Scholle', consisting of red clay and dolomite, is overlain by red-colored till without any flint but with up to 90% carbonate clasts (containing 15% dolomite), which indicates an eastern Baltic origin. The relationship of the 'Scholle' with the glacial till also points to an eastern Baltic origin for it, with up to 1 000 km transport distance.
    Keywords: Area/locality; DEPTH, sediment/rock; Description; Dolomite; Event label; Flint; HAND; Hjelm-Moen1978; Limestone; Magmatites; Møn Island, Denmark; Ratio; Sample ID; Sampling by hand; Sandstone; Schleswig-Holstein, Germany; Schobuell1976; Sediments; Size fraction; Sum
    Type: Dataset
    Format: text/tab-separated-values, 122 data points
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  • 33
    Publication Date: 2023-07-11
    Keywords: 19-183; Chert; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Feldspar; Fragments; Glomar Challenger; Kalifeldspar; Leg19; North Pacific/PLAIN; Plagioclase; Quartz; Quartz, polycrystalline; Ratio; Rock fragments; Sample code/label; Size fraction
    Type: Dataset
    Format: text/tab-separated-values, 782 data points
    Location Call Number Expected Availability
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  • 34
    Publication Date: 2023-07-11
    Keywords: 19-183; Amphibole; Amphibole group minerals; Apatite; Clinopyroxene; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epidote; Garnet; Glomar Challenger; Hornblende, basaltic; Hornblende, common; Kyanite; Leg19; North Pacific/PLAIN; Orthopyroxene; Pumpellyite; Pyroxene group minerals; Sample code/label; Size fraction; Sphene; Staurolite; Tourmaline; Tremolite/Actinolite; Zircon; Zoisite
    Type: Dataset
    Format: text/tab-separated-values, 965 data points
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  • 35
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    PANGAEA
    In:  Supplement to: Bezrukov, Panteleimon L; Skornyakova, Nadezhda S; Murdmaa, Ivar O; Andrushchenko, Polina F; Zenkevich, Nikita L (1976): Ferromanganese Nodules of the Pacific Ocean. P.P. Shirshov Institute of Oceanology of the USSR Academy of Sciences, Transactions, vol. 109. Moscow, Nauka Publ. (P.L. Bezrukov, Ed.), 301 pp
    Publication Date: 2023-08-28
    Description: The monograph highlights extensive materials collected during expeditions of P.P. Shirshov Institute of Oceanology. We consider facial conditions of nodule formation, regularities of their distribution, stratigraphic position, petrography, mineral composition, textures, geochemistry of nodules and hosting sediments. Origin of iron-manganese nodules in the Pacific Ocean is considered as well.
    Keywords: AK4-225-TR; AK4-227-PH; AK4-230-GR; AK4-231-GR; AK4-232-GR; AK4-232-PH; AK4-233-GR; AK4-233-TR; AK4-259-GR; AK4-259-PH; AK4-260-GR; AK4-261-GR; Akademik Kurchatov; AKU4; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Central Pacific Seamounts, Pacific Ocean; DM8; DM8-516-GR; DM8-518-GR; DM8-520-GR; DM8-521-TR; DM8-541-GR; DM8-554-GR; DM8-556-GR; DM8-568-GR; DM8-569-GR; DM8-598-GR; DM8-599-GR; DM8-600-GR; DM8-607-GR; DM8-608-GR; Dmitry Mendeleev; Dredge; DRG; Eastern Basin, Pacific Ocean; Eastern Mariana Basin, Pacific Ocean; Equatorial Pacific; GC; Grab; GRAB; Gravity corer; Manihiki Plateau, Pacific Ocean; Marcus-Necker Ridge; Mariana Basin, Pacific Ocean; MULT; Multiple investigations; Northwestern Basin, Pacific Ocean; OKEAN; Okean Grab; Photo/Video; PV; Southeast Pacific; Southern Basin, Pacific Ocean; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); Vityaz-20; Vityaz-25; Vityaz-29; VITYAZ3150-TR; VITYAZ3151-TR; VITYAZ3233-GC-2; Vityaz-34; VITYAZ3630-PH; VITYAZ3631-GR-1; VITYAZ3632-PH; VITYAZ3635-PH; VITYAZ3729-GC-1; VITYAZ3782-PH; VITYAZ3782-TR; VITYAZ3787-TR; VITYAZ3802-TR; VITYAZ3871-GR-1; VITYAZ3899-GR-1; VITYAZ3900-GR-1; VITYAZ3996-TR; VITYAZ4009-TR; VITYAZ4074-TR; VITYAZ4084-GR-1; VITYAZ4090-TR; VITYAZ4104-TR; VITYAZ4191-TR; VITYAZ4199-TR; VITYAZ4217-TR; VITYAZ4221-TR; VITYAZ4239-PH; VITYAZ4239-TR; VITYAZ4245-GR; VITYAZ4249-PH; VITYAZ4249-TR; VITYAZ4261-PH; VITYAZ4265-TR; VITYAZ4273-GR-1; VITYAZ4273-PH; VITYAZ4273-TR; VITYAZ4279-PH; VITYAZ4279-TR; VITYAZ4281-TR; VITYAZ4285-GR-1; VITYAZ4285-PH; VITYAZ4289-GR-1; VITYAZ4289-TR; Vityaz-43; VITYAZ4309-TR; VITYAZ4320-TR; VITYAZ4331-GR-1; VITYAZ4343-GR-1; VITYAZ4347-GR-1; VITYAZ4347-PH; VITYAZ4351-GR; VITYAZ4355-GR; VITYAZ4359-GR-1; VITYAZ4359-PH; VITYAZ4362-GR-1; VITYAZ4370-PH; VITYAZ4370-TR; Vityaz-48; VITYAZ5066-GR; VITYAZ5066-TR; VITYAZ5074-PH; VITYAZ5074-TR; VITYAZ5096-PH; VITYAZ5100-GR-1; VITYAZ5110-GR-1; VITYAZ5112-GR; VITYAZ5114-GR; VITYAZ5124-TR; VITYAZ5126-GR-1; VITYAZ5128-TR; VITYAZ5129-GR-1; VITYAZ5133-TR; VITYAZ5139-GR-1; VITYAZ5159-TR; VITYAZ5163-GR-1; VITYAZ5398-GR-1; VITYAZ5408-GR-1; VITYAZ5409-GR-1; VITYAZ5410-GR-1; VITYAZ5411-GR-1; VITYAZ5412-DR; VITYAZ5414-GR-1; VITYAZ5420-GR-1; VITYAZ5421-GR-1; VITYAZ5422-GR-1; VITYAZ5423-GR-1; VITYAZ5424-GR; VITYAZ5429-GR-1; VITYAZ5432-GR-1; VITYAZ5437-GR; VITYAZ5505-GR; VITYAZ5937A-GR; VITYAZ5937-GR; VITYAZ5955; VITYAZ5958-GR; VITYAZ5959-GR; VITYAZ5960-GR; VITYAZ5960-PH; VITYAZ5962-GR; VITYAZ5962-PH; VITYAZ5963-GC; VITYAZ5964-GR; VITYAZ5965-0-GR; VITYAZ5965-10-GR-1; VITYAZ5965-1-GR; VITYAZ5965-2-GC; VITYAZ5965-3-GR; VITYAZ5965-3-TR; VITYAZ5965-5-GR; VITYAZ5965-6-GC; VITYAZ5966-GR; VITYAZ5966-PH; VITYAZ5968-14-DR; VITYAZ5968-15-DR; VITYAZ5968-18-GC; VITYAZ5968-1-GR; VITYAZ5968-2-GC; VITYAZ5968-3-GR; VITYAZ5968-4-GR; VITYAZ5968-7-TR; VITYAZ5968-9-GR; VITYAZ5970-GR; VITYAZ5971-GR; VITYAZ5972-TR; VITYAZ5975-GR; VITYAZ5975-PH; VITYAZ5977-PH; VITYAZ5982-GR; VITYAZ5982-PH; VITYAZ5983-GR; VITYAZ5983-PH; VITYAZ5984-GR; VITYAZ5984-PH; VITYAZ5987-GR; VITYAZ5988-11-GR; VITYAZ5988-12-GR; VITYAZ5988-13-GR; VITYAZ5988-14-GC; VITYAZ5988-16-GR; VITYAZ5988-19-TR; VITYAZ5988-20-GR; VITYAZ5988-21-GR; VITYAZ5988-22-GR; VITYAZ5988-24-GR; VITYAZ5988-25-GR; VITYAZ5988-2-GC; VITYAZ5988-4-TR; VITYAZ5988-5-GR; VITYAZ5988-7-GR; VITYAZ5988-9-GR; VITYAZ5993-GR; VITYAZ5995-GR; VITYAZ5996-10-GR; VITYAZ5996-11-TR; VITYAZ5996-13-GR; VITYAZ5996-15-GR; VITYAZ5996-17-GR; VITYAZ5996-18-GR; VITYAZ5996-1-GR; VITYAZ5996-20-GR; VITYAZ5996-22-GR; VITYAZ5996-24-GC; VITYAZ5996-25-GR; VITYAZ5996-2-TR; VITYAZ5996-4-GR; VITYAZ5996-6-GR; VITYAZ6000-GC; VITYAZ6002-11-GC; VITYAZ6002-12-DR; VITYAZ6002-17-GC; VITYAZ6002-20-GC; VITYAZ6002-21-DR; VITYAZ6002-24; VITYAZ6004-GC; VITYAZ6005-GC; VITYAZ6005-GR; VITYAZ6006-GR; VITYAZ6008; VITYAZ6009-GR; VITYAZ6011-GR; VITYAZ6012-GR; VITYAZ6013-GR; VITYAZ6014-GR; VITYAZ6015-GR; VITYAZ6015-PH; VITYAZ6015-TR; VITYAZ6016-GR; VITYAZ6017-DR; VITYAZ6165-GR-1; VITYAZ6167-GR; VITYAZ6168-GR; VITYAZ6172-GR; VITYAZ6174-GR; VITYAZ6177-GR; VITYAZ6243-GR; VITYAZ6255-GR; VITYAZ6256-GR; VITYAZ6257-GR; VITYAZ6264-GR; VITYAZ6265-DR; VITYAZ6267-GR; VITYAZ6270-DR; VITYAZ6272-GR; VITYAZ6273-GR; VITYAZ6275-11-GR; VITYAZ6275-15-TR; VITYAZ6275-2-TR; VITYAZ6275-3-GR; VITYAZ6275-5-GC; VITYAZ6275-8-TR; VITYAZ6277-3-GC; VITYAZ6277-4-TR; VITYAZ6297-TR; VITYAZ6298-10-GC; VITYAZ6298-12-GR; VITYAZ6298-13-TR; VITYAZ6298-14-GC; VITYAZ6298-18-GR; VITYAZ6298-19-GC; VITYAZ6298-1-GC; VITYAZ6298-20-TR; VITYAZ6298-24-TR; VITYAZ6298-26-GR; VITYAZ6298-28-GC; VITYAZ6298-2-GR; VITYAZ6298-30-TR; VITYAZ6298-31-GC; VITYAZ6298-33-GC; VITYAZ6298-34-GR; VITYAZ6298-35-TR; VITYAZ6298-36-GR; VITYAZ6298-37-TR; VITYAZ6298-40-TR; VITYAZ6298-42-GC; VITYAZ6298-43-GR; VITYAZ6298-45-GC; VITYAZ6298-46-GR; VITYAZ6298-47-GC; VITYAZ6298-48-GR; VITYAZ6298-49-GC; VITYAZ6298-50-GR; VITYAZ6298-51-GC; VITYAZ6298-52A-TR; VITYAZ6298-53-TR; VITYAZ6298-56-TR; VITYAZ6298-57-GC; VITYAZ6298-58; VITYAZ6298-62-TR; VITYAZ6298-7-TR; VITYAZ6298-8-GR; VITYAZ6298-9-GR; VITYAZ6299-TR; VITYAZ6300-TR; VITYAZ6307-TR; VITYAZ6331; VITYAZ6332-GR; VITYAZ6333-10-TR; VITYAZ6333-11-GR; VITYAZ6333-13-TR; VITYAZ6333-20; VITYAZ6333-22-GC; VITYAZ6333-23-TR; VITYAZ6333-26-GC; VITYAZ6333-2-TR; VITYAZ6333-3-GC; VITYAZ6333-5-GC; VITYAZ6333-7-GC; VITYAZ6333-8-GC; VITYAZ6334-GR; VITYAZ6335-GC; VITYAZ6339-GC; VITYAZ6343-TR; VITYAZ6344-TR; VITYAZ6348-TR; VITYAZ6352-TR; VITYAZ6356-TR; VITYAZ6358-TR; VITYAZ6359-TR; VITYAZ6360-TR; VITYAZ6364-TR; VITYAZ6365-TR; VITYAZ6366-DR; VITYAZ6367-DR; VITYAZ6368-DR; VITYAZ6369-DR; VITYAZ6405-PH; VITYAZ6408-PH; VITYAZ6704-GC; VITYAZ6706-DR; VITYAZ6817-GR; VITYAZ6818-TR; VITYAZ6819-TR; VITYAZ6821-GR; VITYAZ6822-DR; VITYAZ6824-GR; VITYAZ6825-GR; VITYAZ6826-GR; Vityaz Trench, Pacific Ocean
    Type: Dataset
    Format: application/zip, 14 datasets
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  • 36
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    In:  Supplement to: Moore, Willard S (1981): Iron-manganese banding in Oneida Lake ferromanganese nodules. Nature, 292(5820), 233-235, https://doi.org/10.1038/292233a0
    Publication Date: 2023-08-28
    Description: Ferromanganese nodules in the deep-sea and in freshwater lakes usually accrete layers rich in manganese oxides alternating with layers rich in iron oxides. The mechanism producing these alternating layers is unknown; indeed, the mechanism producing the nodules themselves is unknown. In Oneida Lake, New York, precipitants from the lake water and the surfaces of nodules at the sediment-water interface are enriched in Mn, whereas nodules buried in lake sediments have surface layers enriched in Fe. It is hypothesized here, using field and laboratory evidence, that reduction and mobilization of Mn from the nodule surface during periods of anoxic sediment cover produce the high Fe layers observed in the nodules.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 37
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    In:  Supplement to: Moore, Willard S; Vogt, Peter R (1976): Hydrothermal manganese crusts from two sites near the Galapagos spreading axis. Earth and Planetary Science Letters, 29(2), 349-356, https://doi.org/10.1016/0012-821X(76)90139-4
    Publication Date: 2023-08-28
    Description: Manganese oxide crusts similar to those reported from the Mid-Atlantic Ridge rift valley by Scott et al., 1974 (https://doi.pangaea.de/10.1594/PANGAEA.848726) were dredged at two sites near the Galapagos spreading axis on ocean floor estimated from magnetic anomalies to be 2.4 and 0.3 m.y. old. Compared to the typical ocean-floor manganese deposits attributed to precipitation from seawater, the 2-6 cm thick manganese crusts reported here exhibit very low Fe/Mn and low 232Th/238U ratios, as well as lower transition metal and higher manganese concentrations. The manganese crusts were deposited several orders of magnitude faster than the more common hydrogenous nodules; this fact together with other geochemical characteristics and the geophysical environment suggests the manganese deposits reported here are of hydrothermal origin.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 38
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    In:  Supplement to: Farmer, H G; Dick, H (1981): Descriptions of WHOI rock dredge samples: volume 3. Woods Hole Oceanographic Institution, No. WHOI-81-48, 81-48, 324 pp, https://doi.org/10.1575/1912/1522
    Publication Date: 2023-08-28
    Description: This report is Volume 3 of Descriptions of WHOI rock dredge samples. This series represents a major effort to catalog the rock dredge samples in the WHOI Sea Floor samples collection, and to disseminate this information throughout the scientific community. Volume 3 contains sample descriptions and station data for the dredge stations from five cruises during the period September 1978 through December 1980. The material in this and subsequent volumes of rock descriptions was largely prepared onboard ship by the participating scientists. Volume 3 was printed prior to volumes 1 and 2 because of the excellent documentation of the samples represented in this volume.
    Keywords: A210706; A210707; AII70-06; AII70-07; AT-II-10706-1; AT-II-10706-10PC; AT-II-10706-22GCC; AT-II-10706-39; AT-II-10706-40; AT-II-10706-53; AT-II-10706-55; AT-II-10706-58; AT-II-10706-60; AT-II-10706-61; AT-II-10706-63; AT-II-10706-65; AT-II-10706-66; AT-II-10706-67; AT-II-10707-11; AT-II-10707-13; AT-II-10707-14; AT-II-10707-15; AT-II-10707-16; AT-II-10707-17; AT-II-10707-18; AT-II-10707-2; AT-II-10707-20; AT-II-10707-23; AT-II-10707-25; AT-II-10707-4; AT-II-10707-9; Atlantic Ocean; Atlantis II (1963); Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; G2-10401-17; G2-10401-19; G2-10401-20; G2-10401-29; G2-10401-35; G2-10401-37; G2-10401-40; GC; Gilliss; Gravity corer; GS210401; KN07902; Knorr; KNR-7902-25; KNR-7902-26; KNR-7902-27; KNR-7902-28; Latitude of event; Longitude of event; Melville; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; VLCN05MV; VULCAN_5; VULCAN-5-18; VULCAN-5-20; VULCAN-5-21; VULCAN-5-22; VULCAN-5-23; VULCAN-5-26; VULCAN-5-27; VULCAN-5-29; VULCAN-5-30; VULCAN-5-31; VULCAN-5-32; VULCAN-5-33; VULCAN-5-34; VULCAN-5-35; VULCAN-5-36; VULCAN-5-37; VULCAN-5-39; VULCAN-5-40; VULCAN-5-41; VULCAN-5-42; VULCAN-5-43
    Type: Dataset
    Format: text/tab-separated-values, 619 data points
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  • 39
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    PANGAEA
    In:  Supplement to: Piper, David Z; Williamson, M E (1981): Mineralogy and composition of concentric layers within a manganese nodule from the North Pacific Ocean. Marine Geology, 40(3-4), 255-268, https://doi.org/10.1016/0025-3227(81)90143-2
    Publication Date: 2023-08-28
    Description: The minor-element composition of concentric layers within a single ferromanganese nodule from the eastern North Pacific exhibits strong correlations with Fe and Mn contents but appears to be independent of pronounced mineralogic variations. On the basis of these correlations, the elemental composition of individual layers apparently is controlled by the relative contribution of two sources: seawater, and interstitial water of associated sediment. In contrast, the mineralogy of the nodule, consisting of birnessite in the outer few layers and todorokite in the inner layers, is considered to be a function of nodule diagenesis.
    Keywords: Atomic absorption spectrometry (AAS); Barium; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; DISTANCE; Dredge; DRG; Europium; Insoluble residue; Iron; Lanthanum; Lead; Lutetium; Manganese; Neutron activation analysis; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Samarium; Sample ID; SAN_JUAN_1963; Scandium; SNJ-DH9; Spencer F. Baird; Terbium; Thorium; Wet chemistry; Ytterbium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 399 data points
    Location Call Number Expected Availability
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  • 40
    Publication Date: 2023-08-28
    Description: Compositional data for coexisting manganese nodules, micronodules, sediments and pore waters from five areas in the equatorial and S.W. Pacific have been obtained. This represents the largest study of its type ever undertaken to establish the distribution of elements between the various phases within the sediment column. The composition of manganese nodules, micronodules and sediments (on a carbonate-free basis) shows marked differences between the equatorial high productivity zone and the low productivity region of the S.W. Pacific. In the case of the nodules, th is reflects an increased supply of transition elements (notably Ni, Cu and Zn) to the nodules as a result of the in situ dissolution of siliceous tests within the sediment column in the equatorial Pacific high productivity zone. Micronodules display similar, but somewhat different, compositions to those of the associated nodules in each area. Micronodule composition is therefore influenced by the same basic factors that control nodule composition, but is modified by dissolution of the micronodules in situ within the sediment column. Locally, as in the area immediately south of the Marquesas Fracture Zone, the micronodule population is contaminated by small, angular volcanic rock fragments; this leads to apparently anomalous micronodule compositions. Micronodules appear to be a transient feature in the sediment column, especially in the equatorial Pacific. Dissolution of micronodules in the sediment column therefore represents an important source of elements for the growth of manganese nodules in the equatorial Pacific. Sediment composition is markedly influenced by the carbonate content. On a carbonate-free basis, the sediments from the equatorial high productivity zone are quite distinct in composition from those in the S.W. Pacific. This reflects differences in the lithology of the sediments. In the Aitutaki Passage, the local influence of volcanoclastic material in sediment composition has been established. The major cations and anions in pore waters measured here show no major differences between equatorial and S.W. Pacific sediments. Silica is, however, higher in equatorial Pacific pore waters reflecting the dissolution of siliceous tests in these sediments.
    Keywords: Barium; BCR; Box corer (Reineck); Cobalt; Comment; Copper; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Iron; KAL; Kasten corer; Latitude of event; Longitude of event; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Sediment type; SO06; SO06_10KG; SO06_110KG; SO06_114KG; SO06_138KG; SO06_139KAL; SO06_162KG; SO06_179KG; SO06_184KG; SO06_198KG; SO06_210KG; SO06_214KG; SO06_215KG; SO06_218KAL; SO06_233KG; SO06_235KG; SO06_28KG; SO06_47KG; SO06_51KG; SO06_73KG; SO06_96KG; SO6/1-C-Loc2-10; SO6/1-C-Loc6-28; SO6/1-F-Loc12-73; SO6/1-F-Loc15-96; SO6/1-F-Loc9-47; SO6/1-F-Loc9-51; SO6/1-G-Loc16-110; SO6/1-G-Loc17-114; SO6/1-G-Loc20-138; SO6/1-G-Loc20-139; SO6/2-K-Loc24-162; SO6/2-K-Loc26-179; SO6/2-K-Loc27-184; SO6/2-K-Loc28-198; SO6/2-K-Loc31-210; SO6/2-K-Loc32-214; SO6/2-K-Loc32-215; SO6/2-K-Loc32-218; SO6/2-K-Loc35-233; SO6/2-K-Loc36-235; Sonne; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 419 data points
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  • 41
    Publication Date: 2023-08-28
    Keywords: Baker_B; Big-Adam_B; BLM-75; Deposit type; DEPTH, sediment/rock; Description; Dream_B; Dredge; DRG; Event label; Gulf of Mexico; Gyre; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Size; Small-Adam_B; South-Baker_B; Southern-Hospital_B; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 42
    Publication Date: 2023-08-28
    Description: During U.S. Department of Interior, Bureau of Land Management (BLM) public hearings held in 1973, 1974 and 1975 prior to Texas Outer Continental Shelf (OCS) oil and gas lease sales, concern was expressed by the National Marine Fisheries Service, scientists from Texas A&M and the University of Texas and private citizens over the possible environmental impact of oil and gas drilling and production operations on coral reefs and fishing banks in or adjacent to lease blocks to be sold. As a result, certain restrictive regulations concerning drilling operations in the vicinity of the well documented coral reefs and biostromal communities at the East and West Flower Gardens were established by BLM, and Signal Oil Company was required to provide a biological and geological baseline study of the less well known Stetson Bank before a drilling permit could be issued. Considering the almost total lack of knowledge of the geology and biotic communities associated with the South Texas OCS banks lying in or near lease blocks to be offered for sale in 1975, BLM contracted with Texas A&M University to provide the biological and geological baseline information required to facilitate judgments as to the extent and nature of restrictive regulations on drilling near these banks which might be required to insure their protection. In pursuit of this, scientists from Texas A&M University were to direct their attention toward assessments of ground fish populations, unique biological and geological features, substratum type and distribution, and the biotic and geologic relationships between these banks and those farther north.
    Keywords: Baker_B; Big-Adam_B; BLM-75; Deposit type; DEPTH, sediment/rock; Description; Dream_B; Dredge; DRG; Event label; Gulf of Mexico; Gyre; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Size; Small-Adam_B; South-Baker_B; Southern-Hospital_B; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 43
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    In:  Supplement to: Jenkyns, Hugh C (1976): Sediments and Sedimentary History, Manihiki Plateau, South Pacific Ocean. In: Schlanger, S.O.; Jackson, E.D.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXIII, 873-890, https://doi.org/10.2973/dsdp.proc.33.134.1976
    Publication Date: 2023-08-28
    Description: The Manihiki Plateau is an elevated area of shallow oceanic crust in the South Pacific; it was formed during Early Cretaceous time by profuse outpourings of basalt. DSDP Holes 317, 317A, and 317B, on which this account is based, are situated in a basinal area on the so called High Plateau, the shallowest part of the volcanic edifice, where depths range between 2000 and 3000 meters. The oldest sediments cored are Lower Cretaceous greenish-black volcaniclastics traversed by reddish-purple clay seams; these deposits commonly show evidence of redeposition, but the only possible shallow-water remains found are very rare bryozoan and echinoderm fragments.
    Keywords: 33-314; 33-315A; 33-317A; 33-318; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg33; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/FAN; North Pacific/TROUGH; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Pacific/PLATEAU; South Pacific/RIDGE; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 44
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    In:  Supplement to: Clague, David A (1976): Petrology of Basaltic and Gabbroic Rocks Dredged from the Danger Islands Troughs, Manihiki Plateau. In: Schlanger, S.O.; Jackson, E.D.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXIII, 891-911, https://doi.org/10.2973/dsdp.proc.33.135.1976
    Publication Date: 2023-08-28
    Description: Dredging in the Danger Island Troughs, which divide the High and Western parts of the Manihiki Plateau, recovered several fresh pebbles of olivine tholeiite and tholeiite, a single pebble of highly altered gabbroic cumulate, and several dozen pebbles of altered variolitic basalt. Troughs suggests that at one time the troughs were the site of active faulting. A tectonic model for the evolution of the plateau, consistent with a fracture zone origin for the Danger Island Troughs, requires the formation of the Manihiki Plateau at a triple junction of the Pacific, Farallon, and Antarctic plates.
    Keywords: Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; DSDP; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; SOTW11WT-068D; SOTW-68D; SOUTHTOW; Substrate type; Thomas Washington; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 11 data points
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  • 45
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    PANGAEA
    In:  Supplement to: Vallier, Tracy L; Salisbury, Matthew H; Sachs, H; Quilty, Patrick G; Hart, Roger A; Benson, William E; Bass, Manuel N; Ade-Hall, James M; Yeats, Robert S; Hart, Stanley R (1976): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXIV, 814 pp, https://doi.org/10.2973/dsdp.proc.34.1976
    Publication Date: 2023-08-28
    Description: The Bauer Deep is the depression between the active East Pacific Rise on the west and the extinct Galapagos Rise on the east. The selection of Site 319 was based on a detailed survey of the Bauer Basin during Yaloc-13, Leg 3. Leg 3. It is in a basin about 8 km wide (east-west) at 13°OO.8'S, which is part of a broadly faulted zone on the low western flank of the Galapagos Rise. Site 320 and 321 where located in order to survey the Nazca plate. The objectives for Site 320 were (1) to core basalt continuously as deep as possible, with one and possibly two re-entries; (2) to determine the history of the eastern Nazca plate for the last 30 to 40 m.y., (3) to determine the effectiveness of the Peru-Chile Trench as a barrier to turbidity current dispersal. Site 321 is located on the eastern edge of the Nazca plate immediately south of the Mendafia Fracture Zone. The objectives for Site 321 were similar as those for Site 320.
    Keywords: 34-319; 34-319A; 34-320; 34-320B; 34-321; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg34; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; South Pacific/BASIN; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 137 data points
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  • 46
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    In:  Supplement to: White, Stan; Warnke, Detlef A; Nilsen, T H; Müller, Carla; Morris, D A; Kharin, Gennady S; Faas, Richard W; Caston, V S D; Bjorklund, Kjell R; Talwani, Manik; Udintsev, Gleb B (1976): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXXVIII, 1256 pp, https://doi.org/10.2973/dsdp.proc.38.1976
    Publication Date: 2023-08-28
    Description: Because of its position between the North Atlantic and the Arctic oceans, its young age, small size, and diversity of geological structures, the Norwegian-Greenland Sea provided a unique target for deep drilling on Leg 38 of the Glomar Challenger. From studies of the sediments and basement rocks it was expected to gain insight particularly as to the following: 1) The tectonic framework and evolution of this area with special emphasis on the continental margins and on questions concerned with shifts of spreading axis and existence of foundered continental areas. 2) The youngest times of existence of land bridges between Eurasia and North America and the effect these land bridges had on water circulation and paleoclimates. 3) The date of the initiation of glaciation and dates of glacial advances and retreats. 4) Description of the Tertiary marine microfauna and microflora of the Norwegian-Greenland Sea, which are essentially unknown at present, and investigation of their similarity with microfauna and microflora from other areas.
    Keywords: 38-337; 38-345; 38-347; 38-349; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg38; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/Norwegian Sea/BASIN; North Atlantic/Norwegian Sea/RIDGE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 81 data points
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  • 47
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    In:  Supplement to: Heirtzler, James R (1976): Submersible studies of the Cayman Trough. In: Geodynamics Project U.S. Progress Report - 1976. National Academy of Sciences, Washington D.C., USA; https://catalog.hathitrust.org/Record/007158946, 11-17, https://store.pangaea.de/Projects/NOAA-MMS/Heirtzler_1976_Cayman.pdf
    Publication Date: 2023-08-28
    Description: Scientists from the Woods Hole Oceanographic Institution, the U.S. Navy, the State University of New York at Albany, Wesleyan University, Oregon State University, Dalhousie University, and the Scripps Institution of Oceanography participated in the Cayman Trough expedition durieng 15 ALVIN dives in January and February 1976. The survey focused on a spreading center is a 150-km section of the plate boundary running across the floor of the Cayman Trough, where two tectonic plates are actually moving apart.
    Keywords: AL61100; AL61200; AL61300; AL61500; AL61600; AL61700; AL61900; AL62000; AL62100; AL62200; AL62300; AL62400; AL62500; ALV611; ALV-611; ALV612; ALV-612; ALV613; ALV-613; ALV615; ALV-615; ALV616; ALV-616; ALV617; ALV-617; ALV619; ALV-619; ALV620; ALV-620; ALV621; ALV-621; ALV622; ALV-622; ALV623; ALV-623; ALV624; ALV-624; ALV625; ALV-625; Alvin; Comment; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Grab; GRAB; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 48
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    In:  Supplement to: Hollister, Charles D; Craddock, Campbell; Bogdanov, Yury A; Edgar, N Terry; Gieskes, Joris M; Haq, Bilal U; Lawrence, James R; Rögl, F; Schrader, Hans-Jürgen; Tucholke, Brian E; Weaver, Fred M; Zhivago, V N (1976): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXV, 999 pp, https://doi.org/10.2973/dsdp.proc.35.1976
    Publication Date: 2023-08-28
    Description: The sites drilled on Leg 35 were selected to study the tectonic relationships and interactions between the Antarctic plate and the Antarctic Peninsula, the Scotia Arc, the southern Andes, and the Chile Ridge. Site 322 was drilled on the eastern end of the Bellingshausen Abyssal Plain where it is bounded by the Hero Fracture Zone to the northeast and the continental rise of Antarctica to the south. Site 323 was centrally located on the abyssal plain, about 30 miles west of the Eltanin Fracture Zone and about 150 miles north of the Antarctic continental rise. Site 324 was located on the gently sloping lower continental rise of Antarctica about 160 miles north of Thurston Island, the closest exposed land.
    Keywords: 35-322; 35-323; 35-324; Antarctic Ocean/CONT RISE; Antarctic Ocean/PLAIN; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg35; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 75 data points
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  • 49
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    In:  Marine Institute, University of Texas, Galvestone
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Event label; Gulf of Mexico; Ida Green; Identification; IG19-3; IG19-3-13; IG19-3-15; IG19-3-41; IG19-3-42; IG19-3-45; IG19-3-46; IG19-3-47; IG19-3-48; IG19-4; IG19-4-54; IG19-4-55; IG19-4-56; IG19-4-57; IG19-4-58; IG19-4-68; IG19-4-72; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 240 data points
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  • 50
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    In:  Supplement to: Hariya, Yu; Tsutsumi, Makoto (1981): Hydrogen-isotopic composition of some hydrous manganese minerals. Chemical Geology, 34(1-2), 43-52, https://doi.org/10.1016/0009-2541(81)90070-X
    Publication Date: 2023-08-28
    Description: Initial data on the hydrogen-isotopic compositions in hydrous Mn minerals from various occurrences fall in a wide range from -298 to -84 per mil, relative to SMOW. DeltaD-values of todorokite and cryptomelane from Tertiary deposits show -89 and -150 per mil. 10 Angström-manganite and Delta-MnO2 from deep-sea nodules have relatively restricted DeltaD-values ranging from -96 to -84 per mil. The DeltaD-values for manganese bog ores from recent hot springs show almost -105 per mil. It is recognized that the isotopic values obtained for the deep-sea nodules and recent bog ores are slightly different ranged. Manganite and groutite are unique in their hydrogen-isotopic compositions, having the most depleted DeltaD-values ranging from -298 to -236 per mil. MnO(OH) minerals are more deuterium-depleted hydrous minerals than any other hydrothermal minerals from various ore deposits. Hydrogen-isotope fractionation factors between manganite and water were experimentally determined to be 0.7894, 0.7958 and 0.8078 at 150°, 200° and 250°C, respectively. the present experimental results indicate that if manganites were formed at temperatures below 250°C, under isotopic equilibrium conditions, most of the manganite mineralization in the Tertiary manganese deposits must have precipitated from meteoric hydrothermal solutions.
    Keywords: Core; CORE; Deposit type; DEPTH, sediment/rock; Dredge, box; DRG_B; Event label; FFGR; Free-fall grab; GH77-1; GH77-1-D212; GH77-1-FG40-1; GH77-1-G384; Hakuho-Maru; Hakurei-Maru (1974); Identification; Isotope ratio mass spectrometry; KH-73-4; KH73-4-2; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; O70; Ocean 70 grab; Pacific Ocean; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 51
    Publication Date: 2023-08-28
    Description: This report is Volume 1 in the series of reports entitled "Descriptions of W.H.O.I. rock dredge samples". This series represents a major effort to catalog and prepare initial descriptions for all rock dredge samples in the W.H.O.I. Sea Floor Samples Collection, and to distribute this information throughout the scientific community. Volume 1 contains sample descriptions from approximately 382 dredging stations executed during the period 1960 through 1977. It also represents a digitized listing of all dredge station data for the entire W.H.O.I. Dredge Collection through 1980. This data is sorted by Marsden Square and can serve as a regional index for all rock descriptions included in Volumes 1-3.
    Keywords: A201102; A204201; A207301; A207702; A209306; A209603; AII-04-2RD; AII-11-10RD; AII-11-11RD; AII-11-8RD; AII-73-12RD; AII-73-2RD; AII-73-8RD; AII-73-9RD; AII-77-10RD; AII-77-11RD; AII-77-12RD; AII-77-13RD; AII-77-3RD; AII-77-4RD; AII-77-6RD; AII-77-7RD; AII-77-8RD; AII-77-9RD; AII-93-11RD; AII-93-13RD; AII-93-16RD; AII-96-10RD; AII-96-14RD; AII-96-15RD; AII-96-16RD; AII-96-17RD; AII-96-1RD; AII-96-2RD; AII-96-3RD; AII-96-4RD; AII-96-6RD; AII-96-7RD; AII-96-8RD; AII-96-9RD; AT26601; AT266-03; AT28001; AT280-06; AT29600; AT296-01; AT296-03; Atlantic Ocean; Atlantis (1931); Atlantis II (1963); Caribbean Sea; CH00703; CH00709; CH00906; CH00907; CH01302; CH02101; CH03401; CH03601; CH04301; CH04601; CH05201; CH05801; CH07501; CH07502; CH08207; CH08208; CH10006; CH-100-5RD; CH11504; CH11506; CH115-3RD; CH115-9RD; CH13-7RD; CH21-2RD; CH21-6RD; CH35-3RD; CH35-4RD; CH36-5RD; CH36-6RD; CH43-16RD; CH43-23RD; CH43-33RD; CH43-40RD; CH43-41RD; CH43-7RD; CH46-1RD; CH46-6RD; CH46-7RD; CH52-3RD; CH52-6RD; CH58-9RD; CH7-28RD; CH-75-1RD; CH-75-2RD; CH-75-3RD; CH-75-7RD; CH-75-8RD; CH7-6RD; CH-82-2RD; CH-82-6RD; CH9-2RD; CH9-5RD; Chain; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GO07301; GOS73-7RD; Gosnold; Identification; Indian Ocean; KN04202; KN04203; KN04204; KN04205; KN05402; KN05403; Knorr; KNR-42-11RD; KNR-42-12RD; KNR-42-17RD; KNR-42-18RD; KNR-42-20RD; KNR-42-21RD; KNR-42-22RD; KNR-42-24RD; KNR-42-25RD; KNR-42-26RD; KNR-42-27RD; KNR-42-29RD; KNR-42-30RD; KNR-42-31RD; KNR-42-33RD; KNR-42-34RD; KNR-42-36RD; KNR-42-37RD; KNR-42-39RD; KNR-42-3RD; KNR-42-40RD; KNR-42-41RD; KNR-42-42RD; KNR-42-45RD; KNR-42-4RD; KNR-42-8RD; KNR-42-9RD; KNR-54-20RD; KNR-54-22RD; KNR-54-38RD; KNR-54-39RD; KNR-54-42RD; KNR-54-45RD; KNR-54-4RD; KNR-54-9RD; Latitude of event; Longitude of event; Mediterranean Sea; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optional event label; Position; Quantity of deposit; Sediment type; Size; Southern Ocean; Sta 100; Sta 108; Sta 10 - Dr 2; Sta 110; Sta 112-Dr RD40; Sta 113-Dr RD41; Sta 117; Sta 121; Sta 122; Sta 129; Sta 12 - Dr 11; Sta 12-Dr 4; Sta 130; Sta 131; Sta 137; Sta 145; Sta 146; Sta 146-Dr 9; Sta 14 - Dr 13; Sta 15; Sta 156-Dr 31; Sta 161-Dr 33; Sta 162-Dr 34; Sta 166-Dr 36; Sta 168-Dr 37; Sta 171-Dr 39; Sta 174-Dr 40; Sta 177-Dr 41; Sta 178-Dr 42; Sta 17-Dr 5; Sta 18; Sta 182-Dr 45; Sta 18 - Dr 16; Sta 19 - Dr 2; Sta 2; Sta 21-Dr 3; Sta 23 - Dr 3; Sta 24 - Dr 8; Sta 24-Dr 9; Sta 25-Dr 3; Sta 25-Dr 7; Sta 26 - Dr 4; Sta 26-Dr 8; Sta 28-Dr 4; Sta 30 - Dr 8; Sta 32 - Dr 10; Sta 33 - Dr 11; Sta 34-Dr 2; Sta 37 - Dr 6; Sta 38-Dr 3; Sta 38 - Dr 7; Sta 38 - Dr 9; Sta 3-Dr 1; Sta 42-Dr 20; Sta 44-Dr 22; Sta 44-Dr RD16; Sta 45 - Dr 8; Sta 47 - Dr 12; Sta 48-Dr 6; Sta 48 - Dr 9; Sta 5; Sta 51-Dr 8; Sta 52 - Dr 10; Sta 58 - Dr 11; Sta 5-Dr 2; Sta 60; Sta 62 - Dr 12; Sta 63; Sta 63 - Dr 13; Sta 68; Sta 73; Sta 74; Sta 77-Dr 11; Sta 86-Dr 12; Sta 88-Dr RD33; Sta 9; Sta 91; Sta 98; Sta D-2-Dr 2; Sta D-3-Dr 3; Sta D-4-Dr 4; Sta D-5-Dr 6; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1091 data points
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  • 52
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    In:  Supplement to: Lonsdale, Peter (1976): Abyssal circulation of the southeastern Pacific and some geological implications. Journal of Geophysical Research, 81(6), 1163-1176, https://doi.org/10.1029/JC081i006p01163
    Publication Date: 2023-08-28
    Description: The abyssal circulation of the Pacific Ocean east of the East Pacific Rise is deduced from hydrographic data, supported by a few direct current measurements. Two main flow paths are recognized: across the Chile Rise into the Chile Basin, and thence northward into the Peru Basin and Panama Basin; and eastward across the East Pacific Rise into the Guatemala Basin and into Bauer Basin. Transform fault troughs are important passages allowing flow across the rises, and the Peru-Chile Trench is the principal channel for inflow to the Peru and Panama basins. The deep water that flows across the East Pacific Rise near the equator has a similar temperature structure to that in the southern Chile Basin, but it is less saline and has lower oxygen concentrations. Along both flow paths the bottom waters become warmer, less saline, and less oxygenated as a result of vertical mixing (intensified near sills), geothermal heating (concentrated at active spreading centers) and in situ decay of organic matter (especially beneath productive surface waters). The regional pattern of abyssal circulation may partly control the distribution of metalliferous pelagic sediments (including both fine-grained precipitates and manganese nodules) and the rates of dissolution of calcareous sediments. Where the deep thermohaline flow is accelerated in narrow passages between basins it has deeply eroded the sea floor and transports sediment as bed load. Steady currents measured in one of these passages exceeded 30 cm/s.
    Keywords: CCTW-03D; COCOTOW; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; East Pacific Ocean; File name; Identification; Melville; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 11 data points
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  • 53
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    PANGAEA
    In:  Supplement to: Cyamex Scientific Team; Francheteau, Jean; Needham, H D; Choukroune, P; Juteau, Thierry; Séguret, Marie J M; Ballard, R D; Fox, P J; Normark, William R; Carranza, A; Cordoba, D; Guerrero, Gerardo; Rangin, Claude (1981): First manned submersible dives on the East Pacific Rise at 21�N (project RITA): General results. Marine Geophysical Research, 4(4), 345-379, https://doi.org/10.1007/BF00286034
    Publication Date: 2023-08-28
    Description: A submersible study has been conducted in February - March 1978 at the axis of the East Pacific Rise near 21°N. The expedition CYAMEX, the first submersible program to be conducted on the East Pacific Rise, is part of the French-American-Mexican project RITA (Rivera - Tamayo), a 3-year study devoted to detailed geological and geophysical investigations of the East Pacific Rise Crest. On the basis of the 15 dives made by CYANA in the axial area of the Rise, a morphological and tectonic zonation can be established for this moderately-fast spreading center. A narrow, 0.6 to 1.2 km wide zone of extrusion (zone 1), dominated by young lava flows, is flanked by a highly fissured and faulted zone of extension (zone 2) with a width of 1 to 2 km. Further out, zone 3 is dominated by outward tilted blocks bounded by inward-facing fault scarps. Active or recent faults extend up to 12 km from the axis of extrusion of the East Pacific Rise. This represents the first determination from direct field evidence of the width of active tectonism associated with an accreting plate boundary. Massive sulfide deposits, made principally of zinc, copper and iron, were found close to the axis of the Rise. Other signs of the intense hydrothermal activity included the discovery of benthic fauna of giant size similar to that found at the axis of the Galapagos Rift. We emphasize the cyclic character of the volcanicity. The main characteristics of the geology of this segment of the East Pacific Rise can be explained by the thermal structure at depth below this moderately-fast spreading center. The geological observations are compatible with the existence of a shallow magma reservoir centered at the axis of the Rise with a half-width of the order of 10 km.
    Keywords: CY78-16DF; CY78-17V; CY78-18V; CYAMEX; Cyana (Submersible); Deposit type; DEPTH, sediment/rock; Description; East Pacific Rise; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; OBSE; Observation; Position; Quantity of deposit; Sediment sample; Sediment type; SES; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 21 data points
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  • 54
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    In:  Supplement to: Zakariadze, Guram S; Usher, John L; Theyer, Fritz; Sartori, Renzo; Rodolfo, Kelvin S; Mattey, David P; Martini, Erlend; Keating, Barbara; Ishii, Teruaki; Heiman, M E; Chotin, Pierre; Brassell, Simon C; Balshaw, K M; Kroenke, Loren W; Scott, R (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LIX, 1020 pp, https://doi.org/10.2973/dsdp.proc.59.1981
    Publication Date: 2023-08-28
    Description: Of numerous island-arc systems in the western Pacific, the Mariana arc-trench system and the basins and submerged ridges lying west of them in the Philippine Sea seemed to be best suited to answer questions regarding arc-trench and back-arc basin formation. Three years of planning by the JOIDES Active Margin Panel, Ocean Crust Panel, and Planning Committee resulted in a proposed transect of drill sites aligned more or less along the 18th parallel. This South Philippine Sea transect was designed to investigate each major basin and ridge between the central part of the West Philippine Sea and the Mariana Trench and the Pacific Ocean plate immediately to the east.
    Keywords: 59-447; 59-447A; 59-448; 59-449; 59-450; 59-451; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; Glomar Challenger; Identification; Latitude of event; Leg59; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; North Pacific/Philippine Sea/BASIN; North Pacific/Philippine Sea/RIDGE; North Pacific/RIDGE; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 366 data points
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  • 55
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    In:  Supplement to: Windom, Ken; Vallier, Tracy L; Tokuyama, Hidekazu; Thierstein, Hans R; Thiede, Jörn; Steiner, Maureen B; Sliter, William V; Shcheka, S A; Seifert, Karl E; Sayer, William O; Riech, Volkher; Rea, David K; Premoli Silva, Isabella; Moberly, Ralph; Koporulin, V I; Jenkyns, Hugh C; Fujii, Naoyuki; de Wever, Patrick; Cepek, Pavel; Boyce, Robert E; Batiza, Rodey; Larson, Roger L; Schlanger, Seymour O (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXI, 885 pp, https://doi.org/10.2973/dsdp.proc.61.1981
    Publication Date: 2023-08-28
    Description: The goal of Site 462 was to study the paleontologic, sedimentary, petrologic, tectonic, and magnetic histories of that area through Recent to Late Jurassic time by drilling a deep re-entry site into the Nauru Basin west of the Ralik Chain of the Marshall Islands. This area formed at a fast-spreading Pacific Plate boundary 145 to 155 m.y. ago, in the Late Jurassic. Cores from this area allow to better understand the biostratigraphic evolution and sedimentary processes in a Mesozoic open-ocean environment, the petrologic nature of fast-spreading oceanic crust, the tectonic history of the Late Jurassic Pacific Plate, and the nature of the Jurassic magnetic quiet zone.
    Keywords: 61-462; 61-462A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg61; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 71 data points
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  • 56
    Publication Date: 2023-08-28
    Description: The four sites drilled during Leg 62 were needed to establish better regional coverage of the North Pacific Ocean. Although paleoenvironments were to be stressed on Leg 62, studies of igneous rocks from acoustic basement were planned, to determine ages, petrogenesis, alteration effects, rock magnetism, and Paleomagnetism of old parts of the Pacific crust. These studies were emphasized in order to establish the early history of oceanic plateaus and whether they are the result of midocean-ridge or intraplate volcanism.
    Keywords: 62-463; 62-464; 62-465A; 62-466; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg62; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/CONT RISE; North Pacific/SEAMOUNT; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 157 data points
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  • 57
    Publication Date: 2023-08-28
    Description: A primary objective of Leg 63 was to investigate the fluctuations of this eastern boundary current along a north-south transect off the Gulf of California. This information would aid in biostratigraphically correlating open-ocean planktonic zones with local California zonations. Spanning the last 30 m.y., the complicated tectonic history of the continental margin off California and Baja California comprises changes from a subduction zone to a transform boundary and then to an inactive margin. A second objective of Leg 63 was to define and clarify this history using information on sedimentation, unconformities, basement ages, and paleomagnetic reconstructions gained from drilling, in conjunction with geophysical data and pre-existing bottom samples.
    Keywords: 63-468B; 63-469; 63-470; 63-470A; 63-471; 63-472; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg63; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/ABYSSAL FLOOR; North Pacific/ESCARPMENT; North Pacific/FAN; North Pacific/PLATEAU; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 82 data points
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  • 58
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    In:  Supplement to: Burnett, B R; Nealson, K H (1981): Organic films and microorganisms associated with manganese nodules. Deep Sea Research Part A. Oceanographic Research Papers, 28(6), 637-645, https://doi.org/10.1016/0198-0149(81)90124-2
    Publication Date: 2023-08-28
    Description: Undamaged deep-sea manganese nodules were retrieved from a box core from the central North Pacific and quickly preserved in formaldehyde solution. Light and scanning electron microscope studies of the nodule surface reveal the presence of a variety of fragile filamentous and coccoid bacterial morphotypes, associated with an organic film that covers the botryoid surface.
    Keywords: Argo; BC; Box corer; CLIMAX_II; Deposit type; DEPTH, sediment/rock; Description; H-233; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Size; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 59
    Publication Date: 2023-08-28
    Description: This report presents megascopic descriptions of deep-sea sediment cores obtained by personnel of the Hawaii Institute of Geophysics on cruises of the R/V Kana Keoki in the eastern and western Pacific Ocean during the year 1972.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; FFGR; File name; Free-fall grab; GC; Gravity corer; Identification; Kana Keoki; KK72; KK72MN-FFG-001; KK72MN-FFG-002; KK72MN-FFG-003; KK72MN-FFG-004; KK72MN-FFG-007; KK72MN-FFG-008; KK72MN-FFG-009; KK72MN-FFG-010; KK72MN-FFG-011; KK72MN-LDC-001; KK72MN-LDC-004; KK72MW-RD19; KK72MW-RD20; KK72MW-RD23; KK72MW-RD24; KK72MW-RD25; KK72MW-RD32; KK72MW-RD33; KK72MW-RD34; KK72MW-RD36; KK72MW-RD40; KK72MW-RD43; KK72MW-RD44; KK72MW-RD47; KK72MW-RD49; KK72-PC-3; KK72-PC-7; KK72-PCOD-32; KK72-PCOD-41; KK72-PCOD-50; KK72-PCOD-51; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 284 data points
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  • 60
    Publication Date: 2023-08-28
    Description: Submarine photography and box cores described in this report were taken during the R/V Oceanographer Cruise RP-6-OC-75 in June 1975 over Area C of the DOMES project (Deep Ocean Mining Environmental Study). This Phase I of the DOMES project was conducted by the U.S. Geological Survey under the auspices of the National Oceanic and Atmospheric Administration (NOAA). The purpose of DOMES project was to acquire the information necessary to provide both a timely and an independent assessment of the impact of deep ocean manganese nodule mining on the marine ecosystem before commercial mining operations begin. It was formulated in cooperation with the academic community and the mining industry. It consisted of a two-phase study, first to obtain basic information on the deep ocean environment and then to assess the impact of prototype mining operations on that environment.
    Keywords: Age, comment; BC; Box corer; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DOMES Site C, Pacific Ocean; Elevation of event; Event label; File name; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Photo/Video; Position; PV; Quantity of deposit; RP6OC75; RP6OC75-10-8C; RP6OC75-11-53; RP6OC75-14-38; RP6OC75-14-39; RP6OC75-14-40; RP6OC75-14-41; RP6OC75-14-42; RP6OC75-15B-50; RP6OC75-16B-1; RP6OC75-16B-4; RP6OC75-16B-43; RP6OC75-16B-44; RP6OC75-16B-45; RP6OC75-16B-46; RP6OC75-16B-47; RP6OC75-16B-48; RP6OC75-16B-49; RP6OC75-1-7C; RP6OC75-18A-31; RP6OC75-18A-32; RP6OC75-18A-33; RP6OC75-18A-34; RP6OC75-18A-36; RP6OC75-18B-37; RP6OC75-20-27; RP6OC75-2-1C; RP6OC75-23B-30; RP6OC75-24B-28; RP6OC75-24B-29; RP6OC75-25-51; RP6OC75-27-52; RP6OC75-3-5; RP6OC75-4-2C; RP6OC75-5-10; RP6OC75-5-2; RP6OC75-5-3C; RP6OC75-6-18; RP6OC75-6-6C; RP6OC75-8-4C; RP6OC75-9-21; RP6OC75-9-5C; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 654 data points
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  • 61
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    In:  Supplement to: Hein, James R; Gutmacher, Christina; Miller, Jacquelyn (1976): DOMES Area C, General statement about mineralogy, diagenesis and sediment classification. in: Deep Ocean Mining Environmental Study, N.E. Pacific Nodule Province, Site C, Geology and Geochemistry, U.S. Geological Survey Open File Report. U.S. Geological Survey, 63-80, https://store.pangaea.de/Projects/NOAA-MMS/DOMES_Hein_1976.pdf
    Publication Date: 2023-08-28
    Description: DOMES area C sediment is quite heterogeneous, but most commonly is classified as mud (clay minerals, quartz, and feldspar) or siliceous ooze. However, in several samples Fe-Mn micronodules, globules and aggreqates are the major sediment components. Calcareous nannofossil ooze characterized only one sample, core 18A-1-8 and calcite (reworked limestone?) is present in several other cores, but never as a major compoment. Volcanic ash (glassy mud) is the major sediment type in several cores.
    Keywords: BC; Box corer; Chlorite; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DOMES Site C, Pacific Ocean; Elevation of event; Event label; Illite; Kaolinite; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Position; RP6OC75; RP6OC75-11-53; RP6OC75-15B-50; RP6OC75-16B-49; RP6OC75-18A-36; RP6OC75-18B-37; RP6OC75-20-27; RP6OC75-24B-29; RP6OC75-25-51; RP6OC75-27-52; Sample ID; Sediment type; Smectite
    Type: Dataset
    Format: text/tab-separated-values, 678 data points
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  • 62
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    PANGAEA
    In:  Supplement to: Bischoff, James L; Piper, David Z (1976): Chemical composition of marine sediments of DOMES Site C. in: Deep Ocean Mining Environmental Study, N.E. Pacific Nodule Province, Site C, Geology and Geochemistry, U.S. Geological Survey Open File Report. U.S. Geological Survey, 113-130, https://store.pangaea.de/Projects/NOAA-MMS/bischoff2_DomesC_Analyses.pdf
    Publication Date: 2023-08-28
    Description: The study of the chemical composition of DOMES Site C sediment was undertaken in order to establish important baseline parameters in the overall characterization of the sediment. Such general characterization and information concerning heterogeneity and local variation of this and related parameters such as mineralogy, sediment age, and pore water chemistry, are essential in formulating predictive models concerning environmental perturbations caused by resuspension of sediments during deep sea mining.
    Keywords: Aluminium oxide; Atomic absorption spectrometry (AAS); Barium; BC; Beryllium; Boron; Box corer; Calcium oxide; Carbon, organic, total; Carbon analyser, LECO; Carbon dioxide; Chromium; Cobalt; Copper; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DOMES Site C, Pacific Ocean; Elevation of event; Event label; Iron oxide, Fe2O3; Latitude of event; Lead; Longitude of event; Magnesium oxide; Manganese oxide; Method/Device of event; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Optical emission spectrochemical analysis (OEP); Phosphorus pentoxide; Potassium oxide; RP6OC75; RP6OC75-11-53; RP6OC75-15B-50; RP6OC75-16B-49; RP6OC75-18A-36; RP6OC75-18B-37; RP6OC75-20-27; RP6OC75-24B-29; RP6OC75-25-51; RP6OC75-27-52; Sample ID; Scandium; Silicon dioxide; Sodium oxide; Strontium; Titanium dioxide; Vanadium; X-ray fluorescence (XRF); Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 1703 data points
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  • 63
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    PANGAEA
    In:  Supplement to: van der Weijden, Cornelis H (1976): Some geochemical controls on Ni and Co concentrations in marine ferromanganese deposits. Chemical Geology, 18(1), 65-80, https://doi.org/10.1016/0009-2541(76)90062-0
    Publication Date: 2023-08-28
    Description: The uptake of Ni and Co in the hydrous Mn oxide or the amorphous Fe-oxide phases of ferromanganese deposits in the oceans was studied by electron-microprobe analyses of 17 natural manganese nodules and by experiments on desorption-dissolution of these metals from synthetic Fe oxide or Mn oxides and natural nodule material. Ni was found to occur nearly always in the Mn-oxide phases of natural nodules, while Co occurs both in the Mn-oxide and Fe-oxide phases, with a slight preference for the latter. The solubility of Ni and Co (from coprecipitates of these metals with Fe hydroxides after aging) in seawater was found to depend strongly on the crystallinity of the host phase. The adsorption of Co by the synthetic Mn oxides from seawater was higher than that of Ni. The experimentally determined solubility of Ni and Co in seawater from natural nodule material is extremely low and matches the concentration range of these metals in ocean water.
    Keywords: Atlantic Ocean; Atomic absorption spectrometry (AAS); Cobalt; Copper; Deposit type; DEPTH, sediment/rock; DK_KMY30 (Location 15); DK_KMY35 (Location 9); DK_KMY5 (Location 11); DOWNWIND-H; Dredge; Dredge, chain bag; Dredge, rock; DRG; DRG_C; DRG_R; DWHD16; EASTW; EASTW-11068; Eastward; ELT17; ELT17.009-RD; ELT17.035-BT; ELT17.036-PH; ELT19; ELT19.006-PC; ELT20; ELT20.004-BT; ELT20.005-BT; ELT21; ELT21.004-BT; ELT21.005-BT; ELT25; ELT25.005-BT; ELT25.051-RD; ELT27; Eltanin; Event label; FANB01BD; FANBD-20D; FANFARE-B; GC; Gravity corer; Horizon; Identification; Insoluble residue; Iron; Lead; Manganese; Mineral name; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Southern Ocean; Spencer F. Baird; SYLT 82; TRAWL; Trawl net; V19; V19-11RD; VA05; VA05/1_465; VA05/1_48; VA05/1_515; Valdivia (1961); Vema; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 206 data points
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  • 64
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    In:  Supplement to: Mielke, James E (1976): Ocean manganese nodules. 94th U.S. Congress, 2nd Session, 2nd Edition. U.S. Government Printing Office, Washington; http://www.archive.org/details/oceaeseno00libr, 163 pp, https://store.pangaea.de/Projects/NOAA-MMS/mielke_1976.pdf
    Publication Date: 2023-08-28
    Description: Analysis of manganese nodules recovered from the Blake Plateau by Deepsea Ventures Inc.
    Keywords: Blake Plateau, Atlantic Ocean; Deposit type; DEPTH, sediment/rock; Description; Dredge, chain bag; DRG_C; DSV-70; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; PROS-6A-1; PROS-7A-20; PROS-7A-20F; PROS-7A-20I; PROS-8A-20; PROS-8A-20A; PROS-8A-20B; PROS-8A-20C; PROS-8A-20CB; PROS-8A-20H; PROS-8A-20HB; PROS-8A-20I; PROS-8A-20J; PROS-8A-20M; PROS-8A-20O; PROS-8A-20P; PROS-8A-20PB; PROS-8A-20PC; PROS-8A-20PF; PROS-8A-20PI; PROS-8A-20T; PROS-8A-20V; PROS-8A-20VB; Prospector; Prospector-70; Quantity of deposit; USGS-NOD-A1; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 65
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    In:  Supplement to: Byerly, Gary R; Melson, William G; Vogt, Peter R (1976): Rhyodacites, andesites, ferro-basalts and ocean tholeiites from the galapagos spreading center. Earth and Planetary Science Letters, 30(2), 215-221, https://doi.org/10.1016/0012-821X(76)90248-X
    Publication Date: 2023-08-28
    Description: Volcanic rocks, dredged from depths greater than 1000 m on the Galapagos spreading center, show extreme chemical diversity, including rhyodacites, andesite, ferro-basalts, and low-K oceanic tholeiite. All samples have fresh glassy margins. The ferro-basalts contain up to 18.5% total iron as FeO and up to 3.75% TiO2, while the oceanic tholeiites are as low as 0.02% K2O. The ferro-basalts correlate with the previously proposed zone of high magnetic anomaly amplitudes which flank the Galapagos hot spot, and are consistent with a genesis by shallow fractional crystallization.
    Keywords: Cruise_41; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; DSTGR74-D1; DSTGR74-D7; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Substrate type; USNS De Steiguer (T-AGOR-12); Visual description
    Type: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 66
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    In:  Supplement to: Christie, David M; Sinton, John M (1981): Evolution of abyssal lavas along propagating segments of the Galapagos spreading center. Earth and Planetary Science Letters, 56, 321-335, https://doi.org/10.1016/0012-821X(81)90137-0
    Publication Date: 2023-08-28
    Description: The unusual petrological diversity of abyssal lavas erupted along some segments of the Galapagos spreading center is a direct consequence of the propagation (elongation) of these segments into older oceanic crust. With increasing distance behind propagating rift tips, relatively unfractionated MORB erupted close to the tips are joined first by FeTi basalts (bimodal assemblage) and then by a wide range of basaltic and siliceous lavas. Further behind propagating rift tips, this broad range diminishes again, approaching the narrow compositional range of adjacent normal ridge segments. These compositional variations reflect the evolution of the subaxial magmatic system beneath the newly forming spreading center as it propagates through a pre-existing plate. We envisage this evolution as proceeding from small, isolated, ephemeral magma chambers through increasing numbers of larger, increasingly interconnected chambers to the steady-state buffered system of a normal ridge. Throughout this evolution, magma supply rates gradually increase and cooling rates of crustal magma bodies decrease. High degrees of crystal fractionation are favored only when a delicate balance between cooling rate and resupply rate of primitive magma is achieved. At other propagating and non-propagating ridge-transform intersections the degree to which the balance is achieved and the length of ridge over which it evolves control the distribution of fractionated lavas. These effects may be evaluated provided a number of tectonic variables including transform length, spreading and propagation rates are taken into account.
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Identification; Kana Keoki; KK781230; KK78-12-RD10; KK78-12-RD12; KK78-12-RD12B; KK78-12-RD14; KK78-12-RD16; KK78-12-RD17; KK78-12-RD2; KK78-12-RD20; KK78-12-RD21; KK78-12-RD24; KK78-12-RD25; KK78-12-RD26; KK78-12-RD27; KK78-12-RD29; KK78-12-RD32; KK78-12-RD4; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Station 107; Station 109; Station 8; Station 80; Station 83; Station 85; Station 86; Station 88; Station 89; Station 91; Station 93; Station 94; Station 95; Station 96; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 138 data points
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  • 67
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    In:  Supplement to: Stanley, Daniel Jean; Taylor, P T; Sheng, Harrison; Stuckenrath, Robert Jr (1981): Sohm Abyssal Plain: Evaluating Proximal Sediment Provenance. Smithsonian Contributions to the Marine Sciences, 11, 1-48, https://doi.org/10.5479/si.01960768.11
    Publication Date: 2023-08-28
    Description: The southernmost part of the Sohm Abyssal Plain in the Northwest Atlantic Basin is geographically distal with respect to the major source of Quaternary terrigenous material transported from the Canadian Maritime Provinces. An assessment of the proportion of more locally introduced sediment relative to that derived from distal sources is based largely on size and compositional analyses of Quaternary piston core samples. These data are supplemented by radiocarbon dating of selected core samples, bottom photographs, conductivity-temperature-depth profiles, and seismic records. The premises of the study are that (a) locally derived sediment should be most abundant near high-relief bathymetric features such as seamounts and abyssal hills, and (b) such material should contain enhanced proportions of reworked volcanic debris and alteration products. Core analyses reveal that the amounts of these are directly related to proximity of volcanic ocean-bottom features, and that a significant, although not total, amount of such volcanic materials recovered from cores are derived from submarine weathering of basalt. Associated with this assemblage are nannofossils, dating from the Quaternary to the Upper Cretaceous, reworked from older strata. This increased proportion of volcanic and related products and reworked faunas near seamounts and basement rises strongly implies that such topographic features continue to serve as major source terrains. Locally derived volcanic materials, however, are usually disseminated and masked on the Sohm Abyssal Plain, particularly in sectors receiving large amounts of terrigenous turbidites and biogenic suspensates, and/or undergoing reworking by bottom currents. We propose that the volcanic fraction can serve as a useful index, or "yardstick," to interpret the role of locally derived material in abyssal plain sedimentation. A sedimentation model is developed to illustrate the premise that as access to land-derived sources diminishes, the proportion of terrigenous components is reduced while pelagic and volcanic fractions are enhanced. Thus, sediment accumulating in abyssal plains almost totally isolated from terrigenous sources would comprise significant amounts of pelagic (including wind-blown) and volcanic components.
    Keywords: AT153; AT153-149CC; Atlantic Ocean; Atlantis (1931); Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; File name; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Substrate type; Uniform resource locator/link to image; V22; V22-231; V26; V26-6; V26-9; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 87 data points
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  • 68
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    In:  Supplement to: Fewkes, Ronald H (1976): Electron probe microanalysis of manganese nodules. Washington State University, 71 pp, https://store.pangaea.de/Projects/NOAA-MMS/Fewkes_1976.pdf
    Publication Date: 2023-08-28
    Description: Analyses of small samples extracted from different parts of a single manganese nodule have been reported by several investigators, clearly documenting the belief that a nodule is not homogeneous chemically, as a rule. The same sort of evidence has been gathered by use of the X-ray macroprobe and electron microprobe analyses. The X-ray probe work has shown clearly that chemical variations within a nodule can be correlated with optically recognizable mineral,and therefore optical study can tell much about chemical variations and obviate much probe analysis. As we have reported many times, optically anisotropic crystalline todorokite and birnessite contain the bulk of the Mn, Ni, and Cu in any nodule whereas optically isotropic and X-ray amorphous oxides contain most of the Fe and Co in the same nodule.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 69
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    In:  Supplement to: Bischoff, James L; Piper, David Z; Leong, Kam (1981): The aluminosilicate fraction of North Pacific manganese nodules. Geochimica et Cosmochimica Acta, 45(11), 2047-2063, https://doi.org/10.1016/0016-7037(81)90059-4
    Publication Date: 2023-08-28
    Description: Nine nodules collected from throughout the deep North Pacific were analyzed for their mineralogy and major-element composition before and after leaching with Chester-Hughes solution. Data indicate that the mineral phillipsite accounts for the major part (〉 75%) of the aluminosilicate fraction of all nodules. It is suggested that formation of phillipsite takes place on growing nodule surfaces coupled with the oxidation of absorbed manganous ion. All the nodules could be described as ternary mixtures of amorphous iron fraction (Fe-Ti-P), manganese oxide fraction (Mn-Mg Cu-Ni), and phillipsite fraction (Al-Si-K-Na), these fractions accounting for 96% of the variability of the chemical composition.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 70
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    In:  Supplement to: Meylan, Maurice A; Goodell, H G (1976): Chemical composition of manganese nodules from the Pacific-Antarctic Ocean, Drake Passage and Scotia Sea - Relation to ferromanganese oxide mineralogy and nucleus type. in: Glasby, G.P., Katz, H.R. (Eds.), Marine Geological Investigations in the Southwest Pacific and Adjacent Areas - Papers Presented at the IDOE Workshop, Suva, Fiji, 1-6 September 1975, Technical Bulletin. CCOP-SOPAC (Committee for Co-Ordination of Joint Prospecting for Mineral Resources in South Pacific Offshore Areas), 99-117, https://store.pangaea.de/Projects/NOAA-MMS/Meylan-Goodell_1976.pdf
    Publication Date: 2023-08-28
    Description: Manganese nodules from the Scotia Sea and Pacific Ocean sectors of the Southern Ocean display regional differences in chemical and mineralogical composition. Mn/Fe and todorokite/delta-MnO2 ratios decrease southeasterly from the Southwestern Pacific Basin to the Drake passage-Scotia Sea. Relative to Mn, the greatest enrichments of Co, Ti, V, Zn, Mo and Sn occur in Drake Passage-Scotia Sea nodules, while Ni and Cu are most enriched in the Southwestern Pacific Basin. Manganese mineralogy is directly related to the Mn/Fe ratio, so that todorokite rather than delta-MnO2 predominates when high manganese vs iron contents are found. Trace metal contents are also related to mineralogy, with high values of Ni, Cu, Zn and Sn, and low values of Co, Ti, V and Mo associated with high todorokite contents. Nodules having indistinct zeolitits/vesiculite nuclei tend to have Mn/Fe and todorokite/delta-MnO2 ratios significantly higher than average for the region in which they are found, whereas ferromanganese oxide fragments dredged from submarine rock surfaces usually have Mn/Fe and todorokite/delta-MnO2 ratios lower than regional average.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 71
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    In:  Supplement to: Heimendahl, M; Hubred, Gale Lee; Fuerstenau, D W; Thomas, G (1976): A transmission electron microscope study of deep-sea manganese nodules. Deep Sea Research and Oceanographic Abstracts, 23(1), 69-79, https://doi.org/10.1016/0011-7471(76)90809-3
    Publication Date: 2023-08-28
    Description: Two Pacific Ocean manganese nodules, one from the ocean basin and one from a sea-mount, were examined in transmission electron microscopes at 100 and 650 kV. Of the many specimens examined, ten electron diffraction crystal spot patterns were identified. Sodium birnessite was observed six times and todorokite, Giavanoli's synthetic birnessite, hydrohausmanite and -Fe2O3 one time each. Ferric hydroxide was synthesized in the laboratory and shown to be the same as the primary iron mineral observed in the manganese nodules. The ferric hydroxide had a particle size range from 30 to around 450. Manganese oxide particles were frequently embedded in a mass of smaller ferric hydroxide particles.
    Keywords: 2P-51; Atomic absorption spectrometry (AAS); Cobalt; Copper; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; DRG; DWHD16; Event label; Horizon; Identification; Iron; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Prospector; Prospector-63
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 72
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    PANGAEA
    In:  Supplement to: Friedrich, G; Schmitz-Wiechowski, A (1976): Mikroskopische und mikroanalytische Untersuchungen an metallischen Kügelchen aus Tiefseesedimenten des Zentralen Pazifik. Marine Geology, 20(3), 239-250, https://doi.org/10.1016/0025-3227(76)90118-3
    Publication Date: 2023-08-28
    Description: Metallic spherules from Central Pacific Ocean sediments (“Valdivia” expedition VA-05/1, 1973) were studied by means of microscopy and by electron microprobe analysis. The data suggest that most of the spherules are of meteoritic origin, i.e. ablation drops from meteorites as suggested in former studies on spherules from marine environment by Schmidt and Keil (1966), Finkelmann (1970, 1972) and others. The metallic spherules contain up to about 60% Ni, 37% Fe and 3% Co. Unusually high contents of Cr (up to 12%) were noted in some spherules. Some specimen being coated with Fe oxide could be mistaken for manganese micronodules always abundant in the sediments of the Central Pacific Ocean.
    Keywords: Dredge; DRG; Location 20; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; VA-05/1; VA-05/1_20; Valdivia (1961)
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 73
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    PANGAEA
    In:  Supplement to: Grill, E V; Chase, R L; MacDonald, Richard Drummond; Murray, John W (1981): A hydrothermal deposit from explorer ridge in the northeast Pacific Ocean. Earth and Planetary Science Letters, 52(1), 142-150, https://doi.org/10.1016/0012-821X(81)90216-8
    Publication Date: 2023-08-28
    Description: Crusts composed of nontronite and ferromanganese oxides were recovered from Explorer Ridge, a spreading ridge segment in the northeastern Pacific Ocean located off the west coast of Canada. The chemical and mineralogical composition of the crusts closely resembles that of the mound-like hydrothermal deposits recently discovered at the FAMOUS site on the Mid-Atlantic Ridge and on the Galapagos spreading centre. Compositional anomalies suggest that the crusts are precipitates of hydrothermal vent solutions which were ejected discontinuously and subsequently mixed with seawater.
    Keywords: Dredge; DRG; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; PZ69-11
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 74
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    In:  Supplement to: Février, M (1981): Hydrothermalisme et minéralisations sur la dorsale Est-Pacifique à 21° N. Ph. D. Dissertation, Université de Bretagne Occidentale, Brest, France, pdf 11 MB, 270 pp, https://archimer.ifremer.fr/doc/00034/14498/
    Publication Date: 2023-08-28
    Description: Submersible exploration on the eastern Pacific Ridge near 21 ° N has revealed an active hydrothermal system. It is manifested by the emission in the marine environment of hot and Highly mineralized fluids (370 ° C maximum). These fluids precipitate on contact with seawater and deposits of massive sulphides are built at the outlet of their sources. The mineralogical and geochemical study of the products associated with the emissions of hot fluids provides an initial evaluation of this type of deposit and leads to a comparison between the hydrothermalism responsible for the formation of sulphides and the hydrothermalism responsible for the formation of metal rich crusts formed of iron smectites and manganese oxides. This study is carried out with conventional mineralogical and geochemical investigations (optical and electronic microscopy, X-ray diffraction, X-ray fluorescence spectrometry, electron microprobe, neutron activation and mass spectrometry).
    Keywords: CY-74-26-14; CY-78-06-11; CY-78-12-41; CYAMEX; Cyana (Submersible); East Pacific Rise; FAMOUS 06-74; FAMOUS74; Grab; GRAB; GRAB_subCyana; Grab, on Cyana [Submersible]; Le Noroit; Mid Atlantic Ridge; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 75
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1976): SOUTHTOW Expedition, July 1972 - January 1973, R/V Thomas Washington, List of cores and dredge hauls. Scripps Institution of Oceanography, UC San Diego, unpublished, 18 pp, https://www.ngdc.noaa.gov/mgg/curator/data/thomas_washington/southtow/15045002.pdf
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken on the SOUTHTOW Expedition in June 1972 to January 1973 by the Scripps Institution of Oceanography from the R/V Thomas Washington. A total of 105 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; FFC; Free fall corer; GC; Gravity corer; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; SOTW07WT-008D; SOTW07WT-009D; SOTW07WT-022D; SOTW08WT-027D; SOTW08WT-032D; SOTW08WT-034D; SOTW08WT-036D; SOTW09WT-039D; SOTW09WT-040D; SOTW09WT-046G; SOTW09WT-048D; SOTW09WT-051D; SOTW09WT-052D; SOTW-10-1G; SOTW-104P; SOTW-10PG; SOTW10WT-001FFA; SOTW10WT-001G; SOTW10WT-002FFD; SOTW10WT-003FFA; SOTW10WT-004FFA; SOTW10WT-004FFB; SOTW10WT-004FFC; SOTW10WT-005FFA; SOTW10WT-005FFB; SOTW11WT-068D; SOTW11WT-070D; SOTW-14PV; SOTW-1FFA; SOTW-1G; SOTW-22D; SOTW-27D; SOTW-2FFD; SOTW-32D; SOTW-34D; SOTW-36D; SOTW-38G; SOTW-39D; SOTW-3FFA; SOTW-40D; SOTW-42PG; SOTW-45G; SOTW-46G; SOTW-48D; SOTW-4FFA; SOTW-4FFB; SOTW-4FFC; SOTW-51D; SOTW-52D; SOTW-5FFA; SOTW-5FFB; SOTW-68D; SOTW-6P; SOTW-70D; SOTW-8D; SOTW-9D; SOUTHTOW; Substrate type; Thomas Washington; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 335 data points
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  • 76
    Publication Date: 2023-08-28
    Description: The cores and dredges described at this site were taken on the SESAM cruise from 30 April until 10 June 1976 by the Muséum National d'Histoire Naturelle from the R/V Marion Dufresne. A total of 55 cores, dredges and camera stations were recovered and are available at MNHN for sampling and study.
    Keywords: AT760004; AT760005; AT760007; AT760008; AT760009; AT760010; AT760011; Comment; CS760001; CS760002; CS760003; CS760004; CS760005; CS760006; CS760007; CS760008; CS760009; CS760010; CS760011; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DR760013; DR760014; DR760015; Dredge; DRG; Event label; Identification; Indian Ocean; Marion Dufresne (1972); MD09; MD09-02; MD09-03; MD09-04; MD09-06A; MD09-06B; MD09-11; MD09-12A; MD09-12B; MD09-13; MD09-14; MD09-15CC; MD09-17; MD09-19; MD09-21A; MD09-21B; MD09-22; MD09-23A; MD09-23B; MD09-25A; MD09-25CC; MD09-26; MD09-27; MD09-28; MD09-30A; MD09-30C; MD09-30CC; MD09-31; MD09-32; MD09-33; MD09-34A; MD09-34B; MD09-34C; MD09-34D; MD09-35; MD09-36A; MD09-36B; MD09-37; MD09-38; MD09-40B; MD09-40CC; MD09-41A; MD09-41B; MD09-41C; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PS760089; PS760090; PS760091; PS760093; PS760098; PS760099; PS760100; PS760101; PS760102; PS760104; PS760106; PS760107; PS760108; PS760108CC; PS760109; PS760110; PS760111; PS760111CC; PS760112; PS760113; PS760116; PS760117; PV; Quantity of deposit; Sediment type; SESAM; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 850 data points
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  • 77
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    In:  Supplement to: Pautot, Guy; Renard, V; Auffret, Gérard A; Pastouret, L; De Charpal, O (1976): A granite cliff deep in the North Atlantic. Nature, 263(5579), 669-672, https://doi.org/10.1038/263669a0
    Publication Date: 2023-08-28
    Description: We report here preliminary results from the detailed sampling of granitic basement at a depth of 4.000 m at the lower edge of the Armorican continental margin near 48°N and 12°W. We consider that we have sampled here the extreme lateral limit of the continental crust where local exposures emerge from under a cover of Cainozoic,Mesozoic and probable Palaeozoic sediments.
    Keywords: Atlantic Ocean; CH75; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; GEOMANCHE75/1; Identification; Le Suroît; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Size; SU01-DR12; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 78
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    In:  Supplement to: Usui, Akira; Takenouchi, Sukune; Shoji, Tetsuya (1976): Distribution of metal elements in manganese nodules and formation mechanism of constituent minerals, with special reference to nodules from the Komahashi-Daini Seamount. Mining Geology, Society of Mining Geologists of Japan, 26(6), 371-384, https://doi.org/10.11456/shigenchishitsu1951.26.371
    Publication Date: 2023-08-28
    Description: Petrological, mineralogical and chemical investigations of marine manganese nodules from the West Pacific revealed the intimate relation between the chemical and mineral compositions and the remarkable preferential partitioning of metal elements in the ferromanganese minerals. The microscopic observations of textures of manganese nodules tell the growth history of manganese nodules and the formation conditions of ferromanganese minerals. Chemical compositions of nodules from Komahashi-Daini Seamount are very similar to those of the nodules from marginal banks and seamounts. Compositional variations in the bulk composition of nodules collected from the same dredge haul are considerably small, suggesting the similarity of the growth history of individual nodules, although the contents of metal elements vary remarkably from layer to layer in a single nodule.
    Keywords: Atomic absorption spectrometry (AAS); Bosei Maru; Cobalt; Copper; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GDP-8; GDP-8-12; GDP-8-7; Iron; Latitude of event; Longitude of event; Manganese; Mass; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Philippine Sea; Sample code/label; Sample ID; Size; Substrate type; Thickness; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 130 data points
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  • 79
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    In:  Supplement to: Nohara, Masato (1976): Geochemical characteristics in Pacific Ocean manganese nodules and its controlling factors. Marine Science Monthly (Tokyo), 8(11), 745-750
    Publication Date: 2023-08-28
    Description: Data comes from the NGDC database, https://www.ngdc.noaa.gov/.
    Keywords: Aluminium; Atomic absorption spectrometry (AAS); Calcium; Cobalt; Copper; Date/Time of event; Deposit type; DEPTH, sediment/rock; Dredge, box; DRG_B; Elevation of event; GH74-5; GH74-5-D55; Hakurei-Maru (1974); Iron; Latitude of event; Longitude of event; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Phosphorus; Sample ID; Silicon; Size; Station 128; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
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  • 80
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    In:  Supplement to: Mizuno, Atsuyuki; Moritani, Tomoyuki (1976): Some results of surveys for manganese nodule deposits in the Pacific Ocean by the Geological Survey of Japan. In: Marine Geological Investigations in the Southwest Pacific and Adjacent Areas - Papers Presented at the IDOE Workshop, Suva, Fiji, 1-6 September 1975, Technical Bulletin. CCOP-SOPAC (Committee for Co-Ordination of Joint Prospecting for Mineral Resources in South Pacific Offshore Areas), 62-79
    Publication Date: 2023-08-28
    Description: In 1974, the Geological Survey of Japan began its systematic investigation of manganese nodules in the Central Pacific Basin on the new geological research vessel Hakurei Maru. The first cruise (GH 74-5) was carried out over an eastern part area of the Basin (6°-10°30'N, 164°30'-171°30'W), and the authors report here the preliminary results on the occurrence of manganese nodule deposits, paying particular consideration to their relationship to submarine topography and surficial and sub-bottom sedimentary facies. The surveyed area comprises a deep-sea basin at 5,000-5,400 m, defined to the north and east by the chain of seamounts and guyots of the Christmas Ridge. The deep-sea basin is divided roughly into 2 contrasting topographic features. The eastern part is characterised by flattened topography resulting from continuous deposition of turbidities; the meridian and western parts are characterised by gently rolling topography and the existence of a large number of deep-sea hills. Manganese nodules are almost lacking in the former flattened eastern area, whereas they are widely distributed in the latter rolling meridian and western parts. The population density of nodules varies from less than 1 Kg/m² to 26 kg/m² and the higher density is found in the siliceous-calcareous ooze zone of rather small, flat basins surrounded by deep-sea hills. The density is closely related to the thickness of the transparent layer obtained by 3.5 kHz PDR profiling over the whole area. Considering the various data of grab sampling, 3.5 kHz PDR profiling and to a lesser extent of deep-sea television and camera observations, the most promising manganese field in the present area seems to be confined to the north of the western sector of the area.
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Dredge; DRG; Elevation of event; Event label; GH74-7; GH74-7-150-1; GH74-7-150-2; GH74-7-155; GH74-7-159; GH74-7-160; GH74-7-175; GH74-7-177; GH74-7-179; GH74-7-180; GH74-7-182; GH74-7-183; GH74-7-184; GSJ-71106; GSJ-71107; GSJ-71111; GSJ-71203; GSJ-71208; GSJ-73101; GSJ-73104; GSJ-73109; GSJ-73113; GSJ-73116; Hakurei-Maru (1974); Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 102 data points
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  • 81
    Publication Date: 2023-08-28
    Keywords: 9-77B; Aluminium; Atomic absorption spectrometry (AAS), Perkin-Elmer; Calcium carbonate; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron; Iron, fractionated; Leg9; Magnesium; Manganese; Manganese, fractionated; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/HILL; Phosphorus; Sample code/label; Silicon; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 70 data points
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  • 82
    Publication Date: 2023-08-28
    Keywords: 9-81; Aluminium; Atomic absorption spectrometry (AAS), Perkin-Elmer; Calcium carbonate; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron; Iron, fractionated; Leg9; Magnesium; Manganese; Manganese, fractionated; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/HILL; Sample code/label; Silicon; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 22 data points
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  • 83
    Publication Date: 2023-08-28
    Description: The sulfide deposit at Site 471 occurs between overlying pelagic sediment and underlying basalt. The deposit is vertically zoned and consists, from top to bottom, of the following mineral assemblages: (1) pyrite, chalcopyrite, and Zn-sulfide in chert and calcite gangue (~ 35 cm thick); (2) a 5-cm-thick metalliferous sediment layer and (3) a 4-cm-thick chert layer. The calcite gangue appears at a later stage than chert gangue in the sequence of deposition, also filling in voids and fractures. The manganese content of calcite is particularly high and varies systematically, reaching a maximum at the top of the massive sulfide portion of the deposit.
    Keywords: 63-471; Aluminium oxide; Aluminium oxide, standard deviation; Calcium oxide; Calcium oxide, standard deviation; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Glomar Challenger; Iron oxide, FeO; Iron oxide, FeO, standard deviation; Leg63; Magnesium oxide; Magnesium oxide, standard deviation; Manganese oxide; Manganese oxide, standard deviation; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/FAN; Potassium oxide; Potassium oxide, standard deviation; Replicates; Sample code/label; Silicon dioxide; Sodium oxide; Sodium oxide, standard deviation; Standard deviation; Titanium dioxide; Total
    Type: Dataset
    Format: text/tab-separated-values, 102 data points
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  • 84
    Publication Date: 2023-08-28
    Keywords: Coral Sea; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; ECO; Event label; GEORSTOM_III_CENTRE; GO329D; GO330D; GO331D; GO336D; GO3C-329D; GO3C-330D; GO3C-331D; GO3C-336D; Identification; Le Noroit; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 85
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Calcium oxide; Coral Sea; DEPTH, sediment/rock; Dredge; DRG; ECO; GEORSTOM_III_CENTRE; GO329D; GO3C-329D; Identification; Iron oxide, Fe2O3; Le Noroit; Magnesium oxide; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus pentoxide; Potassium oxide; Silicon dioxide; Sodium oxide; Titanium dioxide; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 86
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Shape; Size; Substrate type; VA-04/1; VA04-26; VA04-28; VA04-45; VA04-50; VA04-54; VA04-58; VA04-62; VA04-64; VA04-71; VA04-75; VA04-79; VA04-83; Valdivia (1961); Visual description
    Type: Dataset
    Format: text/tab-separated-values, 217 data points
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  • 87
    Publication Date: 2023-08-28
    Keywords: Atomic absorption spectrometry (AAS); Barium; Carbon dioxide; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Identification; Iron; Lead; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Phosphorus; Piston corer; Potassium; Shape; Silicon dioxide; Sodium; Substrate type; Surface description; Titanium; VA-04/1; VA04-26; VA04-28; VA04-45; VA04-50; VA04-54; VA04-58; VA04-62; VA04-64; VA04-71; VA04-75; VA04-79; VA04-83; Valdivia (1961); Volume; Water in rock; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 1056 data points
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  • 88
    Publication Date: 2023-08-28
    Keywords: Atomic absorption spectrometry (AAS); Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Gravimetric analysis; Identification; Iron; Lead; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Silicon dioxide; VA-04/1; VA04-54; VA04-58; VA04-62; Valdivia (1961); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 270 data points
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  • 89
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Identification; Location 20; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; VA-05/1; VA-05/1_20; Valdivia (1961); Visual description
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 90
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Atomic absorption spectrometry (AAS); Barium; Calcium oxide; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; Dredge; DRG; Identification; Iron oxide, Fe2O3; Lead; Magnesium oxide; Manganese oxide; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Opal-CT; Potassium oxide; PZ69-11; Silicon dioxide; Sodium oxide; Titanium dioxide; Vanadium; Water in rock; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 145 data points
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  • 91
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Atomic absorption spectrometry (AAS); BC; Box corer; Calcium oxide; Cobalt oxide; Copper(II) oxide; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DOMES Site A, Pacific Ocean; DOMES Site B, Pacific Ocean; DOMES Site C, Pacific Ocean; Dredge, bucket; DRG_BU; Elevation of event; Event label; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Method/Device of event; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Pacific Ocean; Potassium oxide; RP-8-OC-75; RP8OC7503; RP8OC75-47-12; RP8OC75-54-47; RP8OC76; RP-8-OC-76; RP8OC76-14-20; Sample ID; Seascope Expedition; Silicon dioxide; Sodium oxide; SS72/2; SS72/3; SS72/5; SS72/6; SS72-148DB; SS72-149DB; SS72-152DB; SS72-24DB; SS72-52DB; SS72-96DB; Titanium dioxide; Zinc oxide
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 92
    Publication Date: 2023-08-28
    Keywords: Cruise_41; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; DSTGR74-D6; DSTGR74-D9; Event label; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; USNS De Steiguer (T-AGOR-12); Visual description
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 93
    Publication Date: 2023-08-28
    Keywords: BC; Box corer; Color description; Core; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DOMES Site C, Pacific Ocean; Dry mass; Elevation of event; Event label; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Position; Quantity of deposit; RP6OC75; RP6OC75-11-53; RP6OC75-15B-50; RP6OC75-16B-49; RP6OC75-23B-30; RP6OC75-25-51; Sample code/label; Sample ID; Shape; Size; Texture; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 136 data points
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  • 94
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Rea, David K; Janecek, Thomas R (1981): Mass-accumulation rates of the non-authigenic inorganic crystalline (Eolian) component of deep-sea sediments from the western Mid-Pacific Mountains, Deep Sea Drilling Project Site 463. In: Thiede, J; Vallier, TL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 62, 653-659, https://doi.org/10.2973/dsdp.proc.62.125.1981
    Publication Date: 2023-10-19
    Description: Elevated regions in the central parts of ocean basins are excellent for study of accumulation of eolian material. The mass-accumulation rates of this sediment component appear to reflect changes in the influx of volcanic materials through the Early Cretaceous to Recent history of Deep Sea Drilling Project Site 463, on the Mid-Pacific Mountains. Four distinct episodes of eolian accumulation occurred during the Cretaceous: two periods of moderate accumulation, averaging about 0.2 to 0.3 g/cm**2/10**3 yr, 67 to 70.5 m.y. ago and 91 to 108 m.y. ago; a period of low accumulation, approximately 0.03 g/cm**2/10**3 yr, 70.5 to 90 m.y. ago; and a period of high accumulation, about 0.9 g/cm**2/10**3 yr, 109 to 117 m.y. ago (bottom of the hole). Much of the Cenozoic section is missing from Site 463. Upper Miocene to Recent sediments record an upward increase in accumulation rates, from less than 0.01 to about 0.044 g/cm**2/10**3 yr. The late Pliocene-Pleistocene peak may reflect the change to glacial-wind regimes, as well as an increase in volcanic source materials.
    Keywords: 62-463; Accumulation rate, dust; Accumulation rate, mass; AGE; Calculated, see reference(s); Comment; Deep Sea Drilling Project; Density, dry bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Dust, aeolian; Glomar Challenger; Leg62; North Pacific/SEAMOUNT; Porosity; Sample code/label; Sedimentation rate; see reference(s)
    Type: Dataset
    Format: text/tab-separated-values, 707 data points
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  • 95
    Publication Date: 2023-07-10
    Keywords: 18-173; Actinocyclus ingens; Actinocyclus tsugaruensis; Actinoptychus minutus; Actinoptychus vulgaris monicae; Asteromphalus darwinii; Brunia mirabilis; Coscinodiscus lineatus; Coscinodiscus symbolophorus; Deep Sea Drilling Project; Denticula hustedtii; Denticula kamtschatica; Denticula seminae fossilis; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Hemiaulus polymorphus; Leg18; Lithodesmium asketogonium; Lithodesmium californicum; Lithodesmium cornigerum; Nitzschia cf. jouseana; Nitzschia fossilis; Nitzschia praereinholdii; Nitzschia reinholdii; North Pacific/SLOPE; ORDINAL NUMBER; Rouxia californica; Sample code/label; Syendra jouseana; Thalassiosira antiqua; Thalassiosira cf. decipiens; Thalassiosira convexa; Thalassiosira nativa; Thalassiosira oestrupii
    Type: Dataset
    Format: text/tab-separated-values, 243 data points
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  • 96
    Publication Date: 2023-07-10
    Keywords: Actinocyclus ehrenbergii; Actinocyclus ingens; Actinoptychus gruendleri; Actinoptychus minutus; Actinoptychus vulgaris monicae; Asteromphalus darwinii; Brunia mirabilis; California, USA; Cladogramma dubium; Coscinodiscus endoi; Coscinodiscus lineatus; Coscinodiscus plicatus; Coscinodiscus symbolophorus; Cosmiodiscus elegans; Denticula dimorpha; Denticula hustedtii; Denticula hyalina; Denticula kamtschatica; Denticula lauta; Diatom zone; Eupodiscus californicus; HAND; Hemiaulus polymorphus; Hemidiscus cuneiformis; Lithodesmium asketogonium; Lithodesmium californicum; Lithodesmium cornigerum; Lithodesmium minusculum; Lithodesmium reynoldsii; Nitzschia cf. granulata; Nitzschia cf. rolandii; Nitzschia fossilis; Nitzschia marina; Nitzschia praereinholdii; Nitzschia reinholdii; POINT DISTANCE from start; Pterotheca subulata; Rhizosolenia barboi; Rhizosolenia miocenica; Rhizosolenia praebarboi; Rouxia californica; Sample code/label; Sampling by hand; Stephanopyxis schenckii; Stephanopyxis spinosissima; Synedra jouseana; Thalassiosira antiqua; Thalassiosira cf. decipiens; Thalassiosira cf. hyalinopsis; Thalassiosira convexa; Thalassiosira eccentrica; Thalassiosira lineata; Thalassiosira nativa; Thalassiosira oestrupii; Thalassiosira sp.; Triceratium condecorum; Upper-Newport-Bay
    Type: Dataset
    Format: text/tab-separated-values, 1612 data points
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  • 97
    Publication Date: 2023-07-10
    Keywords: Actinocyclus ingens; Actinoptychus gruendleri; Actinoptychus minutus; Actinoptychus vulgaris monicae; Asteromphalus darwinii; Brunia mirabilis; California, USA; Cladogramma dubium; Coscinodiscus cf. confusus; Coscinodiscus cf. temperi; Coscinodiscus endoi; Coscinodiscus lewisianus; Coscinodiscus lineatus; Coscinodiscus plicatus; Coscinodiscus praeyabei; Coscinodiscus symbolophorus; Coscinodiscus yabei; Cosmiodiscus elegans; Craspedodiscus coscinodiscus; Craspedodiscus rhombicus; Cymatogonia amblyoceras; Denticula dimorpha; Denticula hustedtii; Denticula lauta; Denticula nicobarica; Denticula punctata; Diatom zone; Eupodiscus californicus; HAND; Hemiaulus bipons; Hemiaulus polymorphus; Hemidiscus cuneiformis; Lithodesmium californicum; Lithodesmium minusculum; Lithodesmium reynoldsii; Mediaria splendida; Nitzschia cf. invisa; Nitzschia cf. rolandii; Nitzschia praereinholdii; POINT DISTANCE from start; Pterotheca subulata; Raphidodiscus marylandicus; Rhabdonema biquadratum; Rhaphoneis cf. parilis; Rhaphoneis miocenica; Rhizosolenia barboi; Rhizosolenia miocenica; Rhizosolenia praebarboi; Rouxia californica; Rouxia diploneides; Rouxia fusiformis; Rouxia naviculoides; Rouxia peragalli; Rouxia yabei; Sample code/label; Sampling by hand; Sceptroneis caducea; Stephanopyxis corona; Stephanopyxis lineatus; Stephanopyxis schenckii; Stephanopyxis spinosissima; Synedra jouseana; Thalassiosira eccentrica; Thalassiosira lineata; Thalassiosira sp.; Thalassiothrix miocenica; Trachyspheria sp.; Triceratium condecorum; Upper-Newport-Bay
    Type: Dataset
    Format: text/tab-separated-values, 2176 data points
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  • 98
    Publication Date: 2023-07-10
    Keywords: Atlantic Ocean; Atlantische Kuppenfahrten 1967/1-3; BC; BCR; Box corer; Box corer (Reineck); Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East Atlantic; Elevation of event; Event label; FGGE-Equator 79 - First GARP Global Experiment; GC; GIK12309-2; GIK12310-4; GIK12326-4; GIK12328-4; GIK12329-4; GIK12329-6; GIK12330-1; GIK12331-1; GIK12336-1; GIK12337-4; GIK12344-3; GIK12345-5; GIK12347-1; GIK12379-3; GIK12392-1; GIK13207-3; GIK13209-2; GIK13211-3; GIK13218-1; GIK13219-1; GIK13236-1; GIK13238-1; GIK13255-2; GIK13289-1; GIK13291-1; GIK13312-1; GIK13530-1; GIK13533-3; GIK13534-1; Grain size, mean radius; Gravity corer; Gravity corer (Kiel type); KAL; Kasten corer; KOL; Latitude of event; Longitude of event; M12392-1; M25; M30; M30_183; M30_185; M30_208; M30_209; M30_230; M51; M8; M8_017-1; M8/17-1; Meteor (1964); PC; Piston corer; Piston corer (Kiel type); Size fraction 〉 0.006 mm, silt; SL; South Atlantic Ocean; SPC; Sphincter corer; V10; V10-83; V10-84; V10-90; V16; V16-25; V17; V17-159; V19; V19-304; V22; V22-195; V22-196; V22-213; V22-25; V23; V23-100; V23-106; V23-93; V23-99; V25; V25-44; V27; V27-166; V27-167; V27-178; V27-253; V27-260; V27-262; V29; V29-169; V29-170; V30; V30-229; V30-233; V30-243; V30-49; V30-52; V30-56; V30-58; V30-74; V31; V31-2; V32; V32-18; V32-21TW; V32-24TW; V32-27TW; V32-30; V32-31TW; V32-33; V32-35TW; V32-37; V32-40TW; V32-52TW; V32-63TW; V32-9; VA-10/3; Valdivia (1961); van Veen Grab; Vema; VGRAB; Westafrika 1973
    Type: Dataset
    Format: text/tab-separated-values, 340 data points
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  • 99
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    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad
    Publication Date: 2023-07-11
    Keywords: AK15-1363; Akademik Kurchatov; AKU15; Amphibole; Archive of Ocean Data; ARCOD; Calculated; Carbonates; Chamosite; Counting, Stereo Microscope; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoms; Epidote; Feldspar; Foraminifera; Garnet; GC; Glauconite; Gravity corer; Iron hydroxides; Manganese; Mica; North Atlantic; Palagonite; Pyroxene, monoclinic; Pyroxene, rhombic; Quartz; Radiolarians; Rock fragments; Rock fragments and aggregates of clay minerals; Rutile; Size fraction; Spiculae; Sum; Volcanic glass, brown; Volcanic glass, clear; Zeolite; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 1080 data points
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  • 100
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    Unknown
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad
    Publication Date: 2023-07-11
    Keywords: Aggregates; AK15-1364; Akademik Kurchatov; AKU15; Archive of Ocean Data; ARCOD; Carbonate, authigenic; Chlorite; Clayey aggregates; Counting, Stereo Microscope; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Feldspar; Foraminifera; GC; Gravity corer; Minerals, other; North Atlantic; Quartz; Size fraction; Sulfides
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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