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.