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Oligocene crustal anatexis in the Tethyan Himalaya, southern Tibet
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文摘

TheXiaru and Paiku tourmaline-bearing leucogranite dike formed at ~ 28-29 Ma.

These leucogranites are characterized by large variations in the major and trace element compositions as well as Sr–Nd isotope systematics.

The exhumation of deep crustal rocks in the Himalayan orogenic belt could have started as early as Oligocene.

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