Shock-Induced Ringwoodite Rims Around Olivine Fragments in Melt Vein of Antarctic Chondrite GRV022321: Transformation Mechanism

Details Shock-Induced Ringwoodite Rims Around Olivine Fragments in Melt Vein of Antarctic Chondrite GRV022321: Transformation Mechanism Shock-Induced Ringwoodite Rims Around Olivine Fragments in Melt Vein of Antarctic Chondrite GRV022321: Transformation Mechanism

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2776x&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2776

Physics

Scientific paper

We study the formation of ringwoodite via diffusion at high temperatures
and shock pressures in GRV022321 chondrite by using FIB/TEM techniques.
The result suggests transformation occurred by a solid-state mechanism,
enhanced by extreme deformation.

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