High-resolution numerical simulations show that subduction of the Indian plate peeled off the mantle lithosphere from the Tibetan Plateau. This process successfully explains first-order observations of the stepwise growth of the plateau, the migration of magmatism in the region and its seismic properties.

中文翻译：

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青藏高原的崛起是受压倒性的板块地幔拆沉作用控制的


高分辨率数值模拟表明，印度板块俯冲使青藏高原地幔岩石圈剥离。这一过程成功地解释了高原逐步增长、该地区岩浆活动及其地震特性的一级观测结果。