The stability of hydrous phases beyond antigorite breakdown for a magnetite-bearing natural serpentinite between 6.5 and 11 GPa
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DOI: 10.1007/s00410-018-1507-9
Abstract: Phase relations for a natural serpentinite containing 5 wt% of magnetite have been investigated using a multi-anvil apparatus between 6.5 and 11 GPa and 400–850 °C. Post-antigorite hydrous phase assemblages comprise the dense hydrous magnesium silicates (DHMSs) phase… read more here.
Keywords: phase; hydrous phases; magnetite; natural serpentinite ... See more keywords