Record of assembly and breakup of Rodinia in the Southwestern Altaids: Evidence from Neoproterozoic magmatism in the Chinese Western Tianshan Orogen
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文摘

The Neoproterozoic gneissic granitoids in the CTA represent a continental arc setting.

The ca. 730 Ma bimodal intrusive complex was generated in a continental rift setting.

A record of assembly and breakup of Rodinia exists in the Southwestern Altaids.

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