Himalayan orogeny

基本解釋

The Himalayan orogeny caused the uplift and erosion of NE Sichuan area, the reservoir temperature fell to less than 120℃ and the TSR ended.
喜馬拉雅運動使川東北地區(qū)遭受擡陞剝蝕，儲集層溫度降至低於120℃，TSR反應停止。
The Yanshan movement in Eastern China and the Himalayan movement in Western China all reached to the peak of intracontinental orogeny in the earth.
中國東部燕山運動、西部喜馬拉雅運動都達到全球陸內(nèi)搆造運動高峰。
Himalayan orogeny made the area uplift to continent, confirming that the late-Paleocene coast line was probably at southeast Nanbianzhen-Shuiguowei-Jitang area.
喜馬拉雅運動使本區(qū)擡陞爲陸地，進一步証實晚古新世海侵邊界大致在南邊鎮(zhèn)-水鍋尾-基塘連線之南東地帶。