TEM Observations of Amorphized Silicate-Perovskite, Akimotoite and Ca-rich Majorite in a Shock-induced Melt Vein in the Tenham L6 Chondrite

Details TEM Observations of Amorphized Silicate-Perovskite, Akimotoite and Ca-rich Majorite in a Shock-induced Melt Vein in the Tenham L6 Chondrite TEM Observations of Amorphized Silicate-Perovskite, Akimotoite and Ca-rich Majorite in a Shock-induced Melt Vein in the Tenham L6 Chondrite

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1469x&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1469

Physics

Scientific paper

Two mineral assemblages in the melt vein of Tenham constrain
crystallization pressure at ~ 25 GPa, over a period of about 20 ms.
Crystallization is unlikely to have occurred during pressure release,
therefore the crystallization pressure represents the equilibrium shock
pressure.

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