Inferred Depths of Formation of Spinel Cataclasites and Troctolitic Granulite, 76535 Using New Thermodynamic Data for Cr-Spinel

Details Inferred Depths of Formation of Spinel Cataclasites and Troctolitic Granulite, 76535 Using New Thermodynamic Data for Cr-Spinel Inferred Depths of Formation of Spinel Cataclasites and Troctolitic Granulite, 76535 Using New Thermodynamic Data for Cr-Spinel

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1308s&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1308

Physics

1

Scientific paper

New thermodynamic calculations of equilibria pertinent to spinel
cataclasites and troctolites reveal that these assemblages formed at
depths <25 km (cataclasites) and >45 km (troctolites).
Calculations also suggest that symplectite textures formed from trapped
melt.

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