thrust margin 中文意思是什麼
thrust margin
解釋
剩餘推力-
Growth strata and their application in timing deformation of foreland thrust - fold belts in the north margin of tianshan
生長地層及其在判斷天山北緣前陸沖斷褶皺帶形成時間上的應用 -
According to these results combined with exploration practice, foot favorable exploration zones are selected, these are the integrated anticline traps below the tertiary gypsum halite, gypsum mudstone in kuqa foreland thrust belts, the second and the third row structural bells in southern junggar foreland thrust belt, the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin, the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin, and the cold take and nanbaxian structural belt in northern margin of qaidam basin
依據理論分析及勘探實踐，優選出4個有利的勘探區帶，它們是：庫車前陸沖斷帶古近系、新近系膏鹽巖、膏泥巖之下的完整背斜圈閉；準南前陸沖斷帶第二、第三排構造帶；川西北部及南部燕山運動期古隆起、川中平緩褶皺構造帶以及深坳陷內部的非常規天然氣；柴北緣冷湖南八仙構造帶。 -
On the basis of lots of forerunners " data and my research in this thesis, i put forward that the formation and evolution of the west sichuan foreland - like basin were controlled asynchronally by thrust action of two tectonic zones ? longmen mountains and micang - daba mountains, and divided the west sichuan foreland - like basin into three evolutionary phases - - early margin foreland basin stage ( t3m - t3t ), middle foreland - like basin stage ( t3x - j3p ) and late shrinking and extinct stage ( k1 ? 2 )
在收集眾多前人資料和本論文編寫階段實際觀測研究的基礎上，提出和論證了川西類前陸盆地的形成和演化受龍門山和米倉山?大巴山兩構造帶非同步逆沖推覆作用的復合控制，並將川西類前陸盆地的構造演化劃分為三個階段：早期邊緣前陸盆地演化階段（ t _ 3m ? t _ 3t ） 、中期類前陸盆地演化階段（ t _ 3x ? j _ 3p ） ）和晚期萎縮消亡演化階段（ k _ 1 ? e _ 2 ） 。 -
Right - lateral strike - slip thrust system and its dynamics along the northern margin of qaidam basin
柴達木盆地北緣的右行走滑沖斷系統及其動力學 -
Deformation characteristics and time of cenozoic thrust belt in southern margin of jiuquan basin
酒泉盆地南緣新生代沖斷帶的變形特徵和變形時間
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