矿床受近南北向断裂构造控制，矿体以脉状、透镜状、豆芽状赋存于这些断裂破碎带中。
Mineral deposit controlled by north and south faulted structure, mineral body exist in faulted structure with lenticular style, vein style and sprouted style.
它的发育、展布、组合结构等特征都与先存的南北向断裂紧密相关，并表现出明显的分段活动特性。
Its characteristics about fault development, fault distribution and fault compound structure are correlate with meridional fault existed early and show a sectional activity.
推覆构造使得该区断裂、断层发育，主要以南北向或近南北向断裂为主，断裂带的发育为流体的形成提供了有利的条件。
The faultage is along or close to meridional direction, and it offered favorable conditions for the formation of the mineralizing fluid.
由活动断裂所构成的一系列医陷谷地显示了该区新构造应力为近南北向的水平挤压应力。
A series of compressional depressed valleys formed by active faults show that the neotectonic stress field in the area is controlled by horizontal compressional stress.
本次研究共提取162条断裂，主要有南北向、北西向、北西西向、北东向、北东向和东西向五组。
Total 162 faults are extracted in this research. These faults contain five groups of NS trending, NW trending, NWW trending, NE trending and EW trending.
由活动断裂所构成的一系列医陷谷地显示了该区新构造应力为近南北向的水平挤压应力。
Few faults had sinistral activities. A series of compressional depressed valleys formed by active faults show that the neotectonic stress field in...
由活动断裂所构成的一系列医陷谷地显示了该区新构造应力为近南北向的水平挤压应力。
Few faults had sinistral activities. A series of compressional depressed valleys formed by active faults show that the neotectonic stress field in the a...
矿体产出形态及空间分布，严格受近南北向弧形张扭性断裂控制。
The morphology and spacial distribution of the ore body are strictly controlled by the N-S arc-shaped tensional and torsional fractures.
矿体产出形态及空间分布，严格受近南北向弧形张扭性断裂控制。
The morphology and spacial distribution of the ore body are strictly controlled by the N-S arc-shaped tensional and torsional fractures.
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