Mineralogic and O-Isotope Evolution in CM Chondrites: On the Non-Relationship Between Bulk O-Isotopes and Degree of Aqueous Alteration

Details Mineralogic and O-Isotope Evolution in CM Chondrites: On the Non-Relationship Between Bulk O-Isotopes and Degree of Aqueous Alteration Mineralogic and O-Isotope Evolution in CM Chondrites: On the Non-Relationship Between Bulk O-Isotopes and Degree of Aqueous Alteration

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2429h&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2429

Computer Science

Scientific paper

Contrary to predictions, no obvious correlation exists between the
degree of aqueous alteration defined by PSD-XRD modal mineralogy and
O-isotope compositions of CM chondrites. Heterogeneous hydrous
reservoirs and/or consumption of water by oxidation may explain these
data.

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