Iron isotopes constrain sub-seafloor hydrothermal processes at the Trans-Atlantic Geotraverse (TAG)...
Iron isotopes constrain sub-seafloor hydrothermal processes at the Trans-Atlantic Geotraverse (TAG) active sulfide mound
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London: Nature Publishing Group
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English
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London: Nature Publishing Group
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Sub-seafloor hydrothermal processes along volcanically active plate boundaries are integral to the formation of seafloor massive sulfide deposits and to oceanic iron cycling, yet the nature of their relationship is poorly understood. Here we apply iron isotope analysis to sulfide minerals from the Trans-Atlantic Geotraverse (TAG) mound and underlyi...
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Iron isotopes constrain sub-seafloor hydrothermal processes at the Trans-Atlantic Geotraverse (TAG) active sulfide mound
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TN_cdi_doaj_primary_oai_doaj_org_article_111cf11dd7b34972b56851f27ab3baf7
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_111cf11dd7b34972b56851f27ab3baf7
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ISSN
2662-4435
E-ISSN
2662-4435
DOI
10.1038/s43247-022-00518-2
