Sedimentology, petrography and early diagenesis of a travertine–colluvium succession from Chusang (southern Tibet)

The Chusang travertine is situated in southern Tibet at an altitude of ~4200m asl. in a cold-arid, periglacial environment and is characterized by interbedding of hydrothermal carbonate with colluvium. Here we present sedimentological and petrographical data to elucidate the depositional environment...

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