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Mesozoic reactivation of the Beishan, southern Central Asian Orogenic Belt: Insights from low-temperature thermochronology
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文摘
Late Triassic–Early Jurassic cooling was related to the Qiangtang/Eurasia collision. Early Cretaceous cooling was related to the Lhasa–Eurasia collision and slab break-off. Potential late Cretaceous–early Palaeogene cooling was related to the Karakarom–Eurasia collision. No evidence was found for a far-field response to the India–Eurasia collision.

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