Very-dense Silica Minerals in the Shergotty SNC Meteorite: Evidence for Exteme Shock Pressures

Details Very-dense Silica Minerals in the Shergotty SNC Meteorite: Evidence for Exteme Shock Pressures Very-dense Silica Minerals in the Shergotty SNC Meteorite: Evidence for Exteme Shock Pressures

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1827s&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1827

Physics

Scientific paper

Electron and X-ray diffraction confirm that SiO2 in Shergotty consists
of two very dense polymorphs in addition to stishovite. All three of
these high-density structures are quench phases from post-stishovite
structures stable at 47 to >80 GPa.

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