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Detrital zircon provenance constraints on the initial uplift and denudation of the Chinese western Tianshan after the assembly of the southwestern Central Asian Orogenic Belt
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文摘

Sediment provenance shifted abruptly in the mid-Triassic in the northern Tarim basin.

The provenance shift reflects the first-phase intense uplift of the Tianshan range.

The uplifting event resulted from the far-field effects of Qiangtang–Tarim collision.

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