Formation of "Chemically Pure" Magnetite from Mg-Fe-Carbontes: Implications for Exclusively Inorganic Origin of Magnetite and Sulfides in Martian Meteorite ALH84001

Details Formation of "Chemically Pure" Magnetite from Mg-Fe-Carbontes: Implications for Exclusively Inorganic Origin of Magnetite and Sulfides in Martian Meteorite ALH84001 Formation of "Chemically Pure" Magnetite from Mg-Fe-Carbontes: Implications for Exclusively Inorganic Origin of Magnetite and Sulfides in Martian Meteorite ALH84001

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1199g&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1199

Physics

2

Scientific paper

Pure (Mg-free) magnetite was synthesized by heating Mg-Fe-carbonate at
350°C in the presence of pyrite in an evacuated sealed glass tube.
The Mg-free magnetite in the black rims of ALH84001 may have formed by a
similar inorganic abiotic process from Mg-Fe-carbonates.

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