Direct Mineral Melting in the Maniitsoq Structure, West Greenland
Abstract
Microtextures of shock-melted minerals in the Maniitsoq structure constitute compelling evidence of impact-induced single mineral melting, and also document differential crustal reverberation during the solidification of each shock-melted phase.
- Publication:
-
Meteoritics and Planetary Science Supplement
- Pub Date:
- September 2013
- Bibcode:
- 2013M&PSA..76.5008K