SiO2 precipitation in olivine: ATEM Investigation of dunites annealed at 300 MPa in hydrous conditions.
Two natural dunites were annealed at pressure P = 300 MPa, temperature T = 1373, 1473 and 1573 K, and fO2 within the stability field of olivine. The starting materials contained small amounts of hydroxyls in the form of minor phases of hydrated minerals,
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|Source:||Earth and Planetary Science Letters|
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