An Experimental Study of Fe-Mg and Oxygen Isotope Exchange Between Relict Olivine and Chondrule Melt

Details An Experimental Study of Fe-Mg and Oxygen Isotope Exchange Between Relict Olivine and Chondrule Melt An Experimental Study of Fe-Mg and Oxygen Isotope Exchange Between Relict Olivine and Chondrule Melt

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1621b&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

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2

Scientific paper

Isothermal and dynamic crystallization experiments show that relict
olivines retain their original d18O signature despite significant Fe-Mg
exchange with chondrule melt. Relicts can easily be obscured from
electron microprobe detection.

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