Discovery of Andradite Garnet and Evidence for High Temperature Hydrothermal Processes (>300°C) in the Lower Yaxcopoil-1 Impact-Melt Breccias

Details Discovery of Andradite Garnet and Evidence for High Temperature Hydrothermal Processes (>300°C) in the Lower Yaxcopoil-1 Impact-Melt Breccias Discovery of Andradite Garnet and Evidence for High Temperature Hydrothermal Processes (>300°C) in the Lower Yaxcopoil-1 Impact-Melt Breccias

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1751n&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1751

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Scientific paper

Andradite garnet discovered in the matrix of the lower breccia units of
the Yax-1 core in the Chicxulub impact provides evidence of an early
high temperature hydrothermal system (>300°C), with a fluid that
became more oxidizing with time.

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