Jurassic-Cretaceous granitoids and related tectono-metallogenesis in the Zapug-Duobuza arc, western Tibet
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文摘

The Zapug–Duobuza magmatic arc is composed of small scattered granitoid intrusions.

The widely distributed Middle–Late Jurassic granitoids have ore-forming potentials.

A northward flat subduction model can explan the regional tectono-metallogenesis.

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