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Mantle inputs to Himalayan anatexis: Insights from petrogenesis of the Miocene Langkazi leucogranite and its dioritic enclaves
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文摘

The Miocene Langkazi leucogranite contains a large number of dioritic enclaves.

The Langkazi dioritic enclaves are derived from an enriched lithospheric mantle source.

A large amount of mantle-derived melts were added into the Langkazi leucogranites.

Anatexis of the Himalayan crust should be facilitated by addition of mantle heat.

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