Eurasia-India plate collision 欧亚印度板块碰撞事件
The late Cenozoic deformation is considered as a response to the India and Eurasia plate collision and continuous compression.
准噶尔盆地南缘的晚新生代构造变形被认为是天山地区对印度和欧亚板块的碰撞与会聚作用过程的构造响应。
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.
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 origin of porphyry copper deposits has an affinity with the collision of Eurasia plate with the Pacific plate.
斑岩铜矿的出现与欧亚、太平洋两大板块碰撞有密切关系。
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