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    PANGAEA
    In:  Mineralogisk-Geologisk Museum of Oslo | Supplement to: Morten, L; Landini, F; Bocchi, G; Mottana, A; Brunfelt, Arild O (1980): Fe-Mn crusts from the southern Tyrrhenian Sea. Chemical Geology, 28, 261-278, https://doi.org/10.1016/0009-2541(80)90048-0
    Publication Date: 2023-08-28
    Description: Dark crusts and concretions on volcanic and calcareous rocks dredged from seamounts west of the Aeolian Islands, southern Tyrrhenian Sea, consists mainly of amorphous Fe-Mn hydroxides, with some goethite, todorokite, birnessite and clastic minerals. Chemically they consist of predominant Fe (up to 45%) and Mn (up to 12%), with significant amounts of Zn, Ni, Co and Cu. That the REE distribution patterns are similar to those of shallow Pacific derivation - from hydrothermal waters cognate or cycled through volcanic rocks of intermediate composition - is tentatively suggested.
    Keywords: Aluminium; Bannock; BAN-T76EL; BAN-T76EN; Calcium; Cerium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Enarete Seamount; Enolo Seamount; Europium; Event label; Identification; Iron; Lanthanum; Loss on ignition; Lutetium; Magnesium; Manganese; Neodymium; Neutron activation analysis; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Samarium; Silicon; Substrate type; T76; Terbium; Titanium; Vanadium; Wet chemistry; X-ray fluorescence (XRF); Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 240 data points
    Location Call Number Expected Availability
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