The Loss of Iron from the 2.7 Ga Mt. Roe Paleosols (Pilbara, Australia) by Methane-rich Hydrothermal Fluids

Details The Loss of Iron from the 2.7 Ga Mt. Roe Paleosols (Pilbara, Australia) by Methane-rich Hydrothermal Fluids The Loss of Iron from the 2.7 Ga Mt. Roe Paleosols (Pilbara, Australia) by Methane-rich Hydrothermal Fluids

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1971n&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1971

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Chlorite-sericite zone of the Mt.Roe basalt in Pilbara is famous as
Archean Paleosol formed under anoxic atmosphere. We found that the
sericite zone is a hydrothermal production and oxic environment is
expected for the Archean atmosphere.

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