Olivine Zoning and Retrograde Olivine-Orthopyroxene-Metal Equilibration in Types 5 and 6 Ordinary Chondrites

Details Olivine Zoning and Retrograde Olivine-Orthopyroxene-Metal Equilibration in Types 5 and 6 Ordinary Chondrites Olivine Zoning and Retrograde Olivine-Orthopyroxene-Metal Equilibration in Types 5 and 6 Ordinary Chondrites

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1735r&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1735

Physics

Scientific paper

We observed systematic olivine Fa zoning near olivine-metal interfaces
in types 5 and 6 ordinary chondrites. A thermodynamic study suggests
that the olivine zoning formed by localized silicate-metal reactions
during metamorphic cooling.

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