Relict Forsterite in Chondrules: Implications for Cooling Rates

Details Relict Forsterite in Chondrules: Implications for Cooling Rates Relict Forsterite in Chondrules: Implications for Cooling Rates

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1426g&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1426

Physics

Scientific paper

Models of diffusional exchange between relict forsterite and overgrowth
olivine in chondrules suggest typical cooling rates during chondrule
formation of ~200 6000 K/hr under reducing conditions.

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