Mid-Neoproterozoic ridge subduction and magmatic evolution in the northeastern margin of the Indochina block: Evidence from geochronology and geochemistry of calc-alkaline plutons
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文摘

Zircon U–Pb ages identify two groups of plutons emplaced at ~ 765 Ma and ~ 735 Ma.

The rocks were derived by mixing between mantle- and crust-derived magmas in continental arc setting.

The youngest plutons were generated by mantle upwelling related to ridge subduction.

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