P-T Parameters of Magmatic Replacement in Ureilites

Details P-T Parameters of Magmatic Replacement in Ureilites P-T Parameters of Magmatic Replacement in Ureilites

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1041z&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

Scientific paper

Our thermo- and barometric results obtained on ureilites indicates that
their pyroxene-olivine material was replaced by diamond-bearing
graphite-kamacite veinlets at temperatures of 1280°-1466°C and
pressures of 0-5.7 kbar.

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