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Potassic volcanic rocks and adakitic intrusions in southern Tibet: Insights into mantle-crust interaction and mass transfer from Indian plate
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文摘
Existence of petrogenetic distinction between adakites and high-Sr/Y potassic rocks. Indian crust input is restricted to adakitic magmatism in southern Lhasa subterrane. Mantle-derived ultrapotassic melts have genetic links with potassic volcanic rocks. Magmatic differentiation contributed to high K2O contents in potassic and adakitic rocks.

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