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Title: Geochemistry and crystallochemistry of oceanic hydrothermal manganese oxyhydroxides showing Mn-Cu association

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
;  [1]
  1. Universite Pierre et Marie Curie, Paris (France)

Hydrothermal iron and manganese oxides have been found in association with sulfides dredged on the E.P.R. near 7{degree}N. The Mn phase, mainly a 10-7 {angstrom} phyllomanganate, presents a very important enrichment in Cu (up to 30% as weight of oxide). The Fe phase, mainly hydro-goethite, has a very low content of metals of economic interest. Also Mn-Cu oxide particles have been collected in sediment traps near the hydrothermal vents at 13{degree}N. Using the Mn oxide samples of 7{degree}N, Cu shows two simultaneous oxidation states: +I and +II (ESCA and XAS edge measurements). Cu is adsorbed on the Mn(O,OH){sub 2} layers and partially belongs to the water layers (EXAFS results). This seems to be the first report of naturally occurring Cu-buserite in this environment. Lead isotope abundances, the presence of Cu(I), thermodynamic considerations on the stability of the Mn-Cu oxyhydroxides and unsuccessful attempts made with synthetic 10-7 {angstrom} phyllomanganates (buserite and birnessite types) at low temperature in order to stabilize Cu(I) and incorporate it in the interlamellar space of the manganate, lead the authors to accept a high temperature origin for the formation of the Mn-Cu oxyhydroxides. They present a transport model for Cu and Mn precipitation from oceanic hydrothermal fluid, to explain the formation of Mn-Cu oxyhydroxides.

OSTI ID:
5127150
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Vol. 53:4; ISSN 0016-7037
Country of Publication:
United States
Language:
English