Structural relation of phase A to ringwoodite: predicted possible low-pressure polymorph of Mg7Si2H6O14 (phase AII) derived as recombination structure from forsterite
作者： Y. Kudoh
DOI: 10.1016/J.PEPI.2003.05.002
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摘要: 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 Mg7Si2H6O14, can be regarded one member homologous series hypothetical post-humite phases ringwoodite parent This implies the significance whose stability field might close to candidates for hosts water in mantle.
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