Mineralogical and Isotopic Effects of Shock Wave Thermal Histories on Chondrule Precursors

Details Mineralogical and Isotopic Effects of Shock Wave Thermal Histories on Chondrule Precursors Mineralogical and Isotopic Effects of Shock Wave Thermal Histories on Chondrule Precursors

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2123f&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2123

Physics

Scientific paper

Improved models show very significant Mg, Si, and Fe evaporation from
chondrule precursors in shock wave thermal histories that reach
near-liquidus Ts, resulting in preservation of large internal isotopic
heterogeneities, even at high-dust enrichments.

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