Oxygen Isotope Compositions of the Kaidun Meteorite — Indications for Aqueous Alteration of E-Chondrites

Details Oxygen Isotope Compositions of the Kaidun Meteorite — Indications for Aqueous Alteration of E-Chondrites Oxygen Isotope Compositions of the Kaidun Meteorite — Indications for Aqueous Alteration of E-Chondrites

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2414z&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2414

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The Kaidun microbreccia meteorite contains E-chondrite clasts with signs
of pre-Kaidun aqueous alterations that vary in type and degree.
Oxygen-isotope and mineralogical data attest to the presence of water in
E-chondrite parent bodies.

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