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  • Aluminium; Arsenic; Barium; Cadmium; Calcium; Carbon dioxide; Cerium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Dysprosium; Elevation of event; Erbium; Europium; Event label; Gadolinium; Geochemistry; HalbachD36; Holmium; Identification; Induction-coupled plasma technique; Iron; Lanthanum; Latitude of event; Lead; Lithology/composition/facies; Longitude of event; Lutetium; Magnesium; Manganese; manganese micronodule; manganese nodule; Marianas; Molybdenum; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; Pacific Ocean; Palladium; Phosphorus; Platinum; Potassium; Praseodymium; Rhodium; Samarium; Sample code/label; sediment; Silicon; Sodium; Strontium; Terbium; Thomas G. Thompson (1964); Thulium; Titanium; TT192; TT192-D11; TT192-D12; TT192-D13; TT192-D15; TT192-D20; TT192-D21; TT192-D27B; TT192-D28; TT192-D3; TT192-D33; TT192-D36; TT192-D37; TT192-D41; TT192-D42; TT192-D44; TT192-D51; TT192-D52; TT192-D54; TT192-D55; TT192-D56; TT192-D57; TT192-D58; TT192-D59; TT192-D71; TT192-D73; TT192-D8; Vanadium; Water in rock; Wet chemistry; Ytterbium; Yttrium; Zinc  (1)
  • granites  (1)
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  • 1
    Publication Date: 2023-11-23
    Description: During R/V T. Thompson cruise TT-192 around the the Mariana and Volcano Volcanic Arcs 60% of the dredge recoveries contained ferromanganese deposits. Substrate rocks consisted of intermediate to mafic volcanic rocks, volcaniclastic rocks, volcanic breccia, and minor limestone. Volcaniclastic rocks were dominantly sandstone but ranged from mudstone to conglomerate. Ferromanganese deposits occur in five ways: Yellow-brown to black ferromanganese encrustations on rocks; brown, grey, and black ferromanganese oxides cementing volcaniclastic sandstone; stratiform, stratabound Mn oxide rich layers that are pale to dark grey, rarely brownish-grey, with a submetallic luster; cobbles of dark grey submetallic, irregularly shaped masses of manganese (Mn nodules ?) and weatehered black cobbles rich in magnetite. A selection of these deposits was chemically analysed including major and minor elements, rare earth elements, and platinum-group elements. The chemistry determination was done by Induction Coupled Plasma analyses done by J. G. Crock, and K. Kennedy at the U.S. Geological Survey laboratories in Reston, Denver and Menlo Park respectively. Water and CO2 determinations were done by wet chemical techniques.
    Keywords: Aluminium; Arsenic; Barium; Cadmium; Calcium; Carbon dioxide; Cerium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Dysprosium; Elevation of event; Erbium; Europium; Event label; Gadolinium; Geochemistry; HalbachD36; Holmium; Identification; Induction-coupled plasma technique; Iron; Lanthanum; Latitude of event; Lead; Lithology/composition/facies; Longitude of event; Lutetium; Magnesium; Manganese; manganese micronodule; manganese nodule; Marianas; Molybdenum; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; Pacific Ocean; Palladium; Phosphorus; Platinum; Potassium; Praseodymium; Rhodium; Samarium; Sample code/label; sediment; Silicon; Sodium; Strontium; Terbium; Thomas G. Thompson (1964); Thulium; Titanium; TT192; TT192-D11; TT192-D12; TT192-D13; TT192-D15; TT192-D20; TT192-D21; TT192-D27B; TT192-D28; TT192-D3; TT192-D33; TT192-D36; TT192-D37; TT192-D41; TT192-D42; TT192-D44; TT192-D51; TT192-D52; TT192-D54; TT192-D55; TT192-D56; TT192-D57; TT192-D58; TT192-D59; TT192-D71; TT192-D73; TT192-D8; Vanadium; Water in rock; Wet chemistry; Ytterbium; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 1911 data points
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  • 2
    ISSN: 0016-7835
    Keywords: Key words Arabian-Nubian shield ; Continental crust ; granites ; Sraisotopes ; Nd-isotopes ; Pb-isotopes ; U-Pb zircon ages
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Major and trace element data, U–Pb zircon ages, and initial isotopic compositions of Sr, Nd, and Pb are reported for ten granitic and one rhyolitic rock sample from the neo-Proterozoic Nakasib suture in NE Sudan. Chemical data indicate that the samples are medium- to high-K, "I-type" granitic rocks that mostly plot as "volcanic arc granites" on discriminant diagrams. Geochronologic data indicate that rifting occurred 790±2 Ma and constrain the time of deformation associated with suturing of the Gebeit and Haya terranes to have ended by approximately 740 Ma. Isotopic data show a limited range, with initial 87Sr/86Sr=0.7021 to 0.7032 (mean=0.7025), εNd(t) =+5.5 to +7.0 (mean=+6.4), and 206Pb/204Pb = 17.50–17.62. Neodymium model ages (TDM; 0.69–0.85 Ga; mean = 0.76 Ga) are indistinguishable from crystallization ages (0.79–0.71 Ga; mean=0.76 Ga), and the isotopic data considered together indicate derivation from homogeneously depleted mantle. The geochronologic data indicate that the terrane accretion to form the Arabian–Nubian shield began just prior to 750 Ma. The isotopic data reinforces models for the generation of large volumes of juvenile continental crust during neo-Proterozoic time, probably at intra-oceanic convergent margins. The data also indicate that crust formation was associated with two cycles of incompatible element enrichment in granitic rocks, with an earlier cycle beginning approximately 870 Ma and culminating approximately 740 Ma, and the second cycle beginning after pervasive high-degree melts – possibly hot-spot related – were emplaced approximately 690–720 Ma.
    Type of Medium: Electronic Resource
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