The hydrothermal component in ferromanganese nodules from the southeast Pacific Ocean

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The hydrothermal component in ferromanganese nodules from the southeast Pacific Ocean

Statistical analyses of geochemical data from ferromanganese nodule samples representing a broad area of the southeast Pacific Ocean indicate nodule compositions are controlled by four factors: (1) suboxic diagenesis; (2) oxic diagenesis; (3) hydrogenous precipitation; and (4) hydrothermal precipitation. The first three are identical to those identified in studies of nodules from the North Paci...

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ژورنال

عنوان ژورنال: Geochimica et Cosmochimica Acta

سال: 1989

ISSN: 0016-7037

DOI: 10.1016/0016-7037(89)90064-1