近东西向深大断裂控制了金矿的空间展布。
Nearly WEtrending deep fault controlled the spatial extension of gold deposit.
南河与秀延河分水岭近东西向从整合区中部通过。
Yanhe River watershed, and show nearly East-West from the integration of areas in the central passage.
北东和近东西向两组断层于该区的存在对本地震带的形成有重要作用。
The existence of the TWD groups of ne and near EW fault groups plays a very important role in the formation of this earthquake belt.
矿区内闪长岩近东西向侵入上石炭统奇尔古斯套组上部，构造破碎作用严重。
In mining area, nearly east-westward Diorites body invaded to upper rocks of Qiergustao formation, and was fragmentated serious.
最大水平主应力方向以近东西向为主，水力压裂裂缝的延伸方向也以近东西向为主；
The conclusion is that the size of terrestrial stress mainly is vertical principal stress maximum and the fracture of hydraulic fracturing is vertical.
在水平方向上，中国东部地壳的主应力方向为近东西向的压应力，但总体上是向东推移的。
The main horizontal stress in eastern China is the pressure near EW direction, but as a whole, the crust is moving east.
阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.
福建省德化县邱村金矿床主要受构造断裂带控制，北东向断裂和近东西向断裂与成矿关系密切。
The Quicun Gold Deposit in Dehun County, Fujian Proince is controlled by the tectonic faulted zones. The north east and east west faults have a close relation with mineralization.
深层的泥盆系内大型构造十分发育，并组成了近南北向与近东西向构造带的分带、分块与叠加现象。
Big scale structures developed well in Devonian strata which is in the deep area, and formed the approximately south and north, east and west zones.
研究区发育侏罗纪盆地和白垩纪盆地，侏罗纪盆地受近东西向断裂的控制，为东西向展布的断陷湖盆。
There exist Jurassic and Cretaceous basins in the Beishan Alaxa area. The Jurassic basins are controlled by near EW trending faults, and the faulted basins extend in EW direction.
靖州平茶金矿为多硫化物型锑金矿床，矿化受近东西向次级断裂和蚀变带控制，矿床规模小，但品位高。
Pingcha gold deposit is a Sb-Au of rich in sulphide, controlled by the E-W secondary fracture and alteration zone and being small in scal but high in grade.
武汉市岩溶地面塌陷发生在具二元结构的北东向长江一级阶地与近东西向褶皱构造向斜核部碳酸岩盐地层相交的部位。
The karst surface collapse in Wuhan happened at the intersection between the ne first terrace binary-structured deposits of Yangtze River and carbonate in the core of E-W syncline.
区域上受多组近东西向断裂控制，区内地层较简单，但岩性复杂，岩浆活动强烈，特别是在雅满苏、沙泉子附近有明显的火山活动中心及残留的火山机构。
The metallogenic district is controlled by a few nearly east and west fractures. In the region, the stratum is simple, but the rock character is complex. The magma activity is fierceness.
区域上受多组近东西向断裂控制，区内地层较简单，但岩性复杂，岩浆活动强烈，特别是在雅满苏、沙泉子附近有明显的火山活动中心及残留的火山机构。
The metallogenic district is controlled by a few nearly east and west fractures. In the region, the stratum is simple, but the rock character is complex. The magma activity is fierceness.
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