Condensation During Chondrule Formation: Elemental and MG Isotopic Evidence

Details Condensation During Chondrule Formation: Elemental and MG Isotopic Evidence Condensation During Chondrule Formation: Elemental and MG Isotopic Evidence

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1342n&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1342

Computer Science

7

Scientific paper

Evidence for condensation of Mg, Si, Fe, Na, and K due to temperature
decrease during chondrule formation is found in two Semarkona
chondrules. The evidence includes compositional zoning in glass and
heavier Mg isotopic composition in forsterite core.

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