Exhumation history of the West Kunlun Mountains, northwestern Tibet: Evidence for a long-lived, rejuvenated orogen
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Zircon U–Pb/FT double dating provides new ages for the sediments in southwestern Tarim Basin.

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The data show episodic exhumation and magmatism in the West Kunlun Mountains.

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The orogen has emerged since the Triassic–Early Jurassic and was rejuvenated in the Meso-Cenozoic.

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A double-sided lithospheric wedge model is proposed to explain Neogene tectonism in western Tibet.

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