Himalayan orogeny

基本解释

The Himalayan orogeny caused the uplift and erosion of NE Sichuan area, the reservoir temperature fell to less than 120℃ and the TSR ended.
喜马拉雅运动使川东北地区遭受抬升剥蚀，储集层温度降至低于120℃，TSR反应停止。
The Yanshan movement in Eastern China and the Himalayan movement in Western China all reached to the peak of intracontinental orogeny in the earth.
中国东部燕山运动、西部喜马拉雅运动都达到全球陆内构造运动高峰。
Himalayan orogeny made the area uplift to continent, confirming that the late-Paleocene coast line was probably at southeast Nanbianzhen-Shuiguowei-Jitang area.
喜马拉雅运动使本区抬升为陆地，进一步证实晚古新世海侵边界大致在南边镇-水锅尾-基塘连线之南东地带。