Discovery of Ringwoodite, Wadsleyite, and γ-Ca3(PO4)2 in Chassigny: Constraints on Shock Conditions

Details Discovery of Ringwoodite, Wadsleyite, and γ-Ca3(PO4)2 in Chassigny: Constraints on Shock Conditions Discovery of Ringwoodite, Wadsleyite, and γ-Ca3(PO4)2 in Chassigny: Constraints on Shock Conditions

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.1586g&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

Physics

Scientific paper

The olivine high-pressure polymorphs ringwoodite and wadsleyite as well
as the high-pressure phosphate γ-Ca3(PO4)2 were discovered in melt
pockets of the martian dunite Chassigny attesting a minimum prevailing
shock pressure of ~20 GPa.

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