Origin of PO Chondrules from Thermally Annealed Granoblastic Olivine Aggregates

Details Origin of PO Chondrules from Thermally Annealed Granoblastic Olivine Aggregates Origin of PO Chondrules from Thermally Annealed Granoblastic Olivine Aggregates

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1748w&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

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Scientific paper

Clasts of GOA break up rapidly when heated isothermally and olivine
shows reverse zoning. Cooling at 10°-100°C/hr gives porphyritic
textures with normally zoned olivine. Whether GOA are planetary or
nebular they represent potential chondrule precursors.

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