Late Jurassic sodium-rich adakitic intrusive rocks in the southern Qiangtang terrane, central Tibet, and their implications for the Bangong-Nujiang Ocean subduction
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Newly discovered adakitic rocks in the southern Qiangtang subterrane

Adakitic rocks were generated in the Late Jurassic (148–150 Ma).

Bangong–Nujiang Ocean subducted northward beneath the Qiangtang terrane.

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