Multiphase solid inclusions in zoisite-bearing eclogite: evidence for partial melting of ultrahigh-pressure metamorphic rocks during continental collision
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文摘

Composite multiphase solid inclusions occur in garnet and omphacite of UHP eclogite;

The Qz + Pl ± Kfs inclusions would derive from dehydration melting of paragonite ± phengite;

The Brt + Pl + Kfs + Ep/Zo inclusions would derive from the reaction between melt and host mineral;

The breakdown of hydrous minerals is a key to partial melting of UHP metamorphic rocks;

Dehydration melting of the UHP eclogite would have occurred during its exhumation to the HP regime.

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