Physics
Scientific paper
Jun 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004pepi..143..305k&link_type=abstract
Physics of the Earth and Planetary Interiors, Volume 143, p. 305-309.
Physics
Scientific paper
A possible low-pressure polymorph of Mg7Si2H6O14 (phase AII) was derived from forsterite as a recombination structure. The present study suggests that phase A, high-pressure polymorph of Mg7Si2H6O14, can be regarded as one member of a homologous series of hypothetical post-humite high-pressure phases derived from ringwoodite as a parent structure. This implies the possible significance of post-humite high-pressure phases whose stability field might be close to phase A as candidates for the hosts of water in the mantle.
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