Brown and Clear Olivine in Chassignite NWA 2737: Water and Deformation

Details Brown and Clear Olivine in Chassignite NWA 2737: Water and Deformation Brown and Clear Olivine in Chassignite NWA 2737: Water and Deformation

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1314t&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1314

Physics

1

Scientific paper

Olivine in the NWA 2737 chassignite is brown, and cut by ribbons of
visually colorless olivine. The latter formed by deformation along the
system [100]{021}. The brown color arises from ferric iron in the
olivine, probably formed by loss of dissolved H+.

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