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(yùn)動使川東北地區(qū)遭受抬升剝蝕，儲集層溫度降至低于120℃，TSR反應(yīng)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(yùn)動、西部喜馬拉雅運(yùn)動都達(dá)到全球陸內(nèi)構(gòu)造運(yùn)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(yùn)動使本區(qū)抬升為陸地，進(jìn)一步證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。