Ultrametamorphism of Impure Carbonates Beneath the Manicouagan Impact Melt Sheet: Evidence for Superheating

Details Ultrametamorphism of Impure Carbonates Beneath the Manicouagan Impact Melt Sheet: Evidence for Superheating Ultrametamorphism of Impure Carbonates Beneath the Manicouagan Impact Melt Sheet: Evidence for Superheating

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2385s&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2385

Physics

1

Scientific paper

Ultrametamorphism of impure carbonates by impact melt at Manicouagan has
yielded refractory Ca-Mg alumino-silicates and in situ partial melts
that attained >900°C. This indicates that the melt sheet cooled
from >1800°C and was superheated.

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