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北喜马拉雅片麻岩穹隆 NHGD
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喜山早期，受印度板块与欧亚板块碰撞作用的影响，形成了北东—南西方向的水平挤压应力场。
During the Early Himalayan stage, the NE SW trending horizontal compressive TSF was formed by the effect of the collision of India plate and Eurasian plate.
喜山运动以后油气聚集的规律，受三组走向相互平行的北倾逆断裂所控制。
Oil and gas accumulation after Ximalaya movement was controlled by 3 sets of north tilted reversed fault system with parallel strikes.
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