Alteration of Suevitic Impactites at the Ries Crater, Germany: Stable Isotope Composition of Smectite Minerals and Fluid Temperatures

Details Alteration of Suevitic Impactites at the Ries Crater, Germany: Stable Isotope Composition of Smectite Minerals and Fluid Temperatures Alteration of Suevitic Impactites at the Ries Crater, Germany: Stable Isotope Composition of Smectite Minerals and Fluid Temperatures

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1468m&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1468

Physics

1

Scientific paper

This study represents δ18O and δD analyses of smectite
minerals in crater fill and surficial suevite from the Ries crater,
Germany to elucidate the origin and temperature of the fluids
responsible for alteration of impact glass and primary silicates.

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