堆晶体发生部分熔融，拆沉物熔融岩浆与地壳熔融岩浆于地壳岩浆房产生完全混合作用，形成古近纪具同碰撞及弧火山属性的岩浆。
The magma of melted detaching and sinking crystal completely mixes with that of the melted crust in the magmatic chamber of crust, which forms the Palaeogene syncollision and volcanic arc magma.
青藏高原不是印度板块与欧亚板块碰撞的结果，而是形成于下地壳流动驱动的板内盆山作用。
The formation of the Qinghai-Tibet Plateau was not caused by the collision between India plate and Eurasia plate, but by intraplate basin-mountain coupling driven by lower crustal flow.
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