X-ray in situ studies in electrically and laser-heated diamond anvil cells
(DACs) at pressures over 80 cpa and temperatures above 2500 K were used to
determine stable silica phase at extreme conditions. We demonstrate that so
far unidentified phases obtained on the compression of cc-cristobalite, ne
w dense silica polymorph in the Martian Shergotty meteorite, and controvers
ial post-stishovite phase is alpha -PbO2-like silica. (C) 2001 Elsevier Sci
ence B.V. All rights reserved.