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(dòng)使川東北地區(qū)遭受擡陞剝蝕，儲(chǔ)集層溫度降至低於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(guó)東部燕山運(yùn)動(dòng)、西部喜馬拉雅運(yùn)動(dòng)都達(dá)到全球陸內(nèi)搆造運(yùn)動(dòng)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(dòng)使本區(qū)擡陞爲(wèi)陸地，進(jìn)一步証實(shí)晚古新世海侵邊界大致在南邊鎮(zhèn)-水鍋尾-基塘連線(xiàn)之南東地帶。