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Features, provenance, and tectonic significance of Carboniferous-Permian glacial marine diamictites in the Southern Qiangtang-Baoshan block, Tibetan Plateau
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文摘

Glacial sediments were transported by ice rafts and deposited in a marine environment.

Provenance of the glacial marine diamictite on the Tibetan Plateau was Indian Gondwana.

From the Early to the Late Paleozoic, the Indian Gondwana was an erosional zone.

Himalaya area, Lhasa and Southern Qiangtang–Baoshan blocks were depositional environments.

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