The Qiantang terrane is one of three main west-east-trending terranes of the Tibetan Plateau. During the Triassic, a southward-directed subduction along its northern margin resulted in the Jin-Shajing suture, the limit between it and the Songpan-Ganzi terrane.
The Qiantang terrane is one of three main west-east-trending terranes of the Tibetan Plateau. During the Triassic, a southward-directed subduction along its northern margin resulted in the Jin-Shajing suture, the limit between it and the Songpan-Ganzi terrane.
Source: Wikipedia "Qiangtang terrane" · CC BY-SA 4.0
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