2 . structural systems exposed in the studied area include latitudinal , ns - trending , nw - trending , cathaysian , neocathaysian , and rotated - and sheared - related structural systems , the enrichment and formation of gold and multi - metal deposit were tightly related with the formation and development of above - mentioned structural systems . especially , the compound and joint of those structural systems , and their relation to the geological process in deep , were mainly ore - controlling factors of gold deposits in this area 2 、辽宁医巫闾山地区出露的构造体系有纬向、经向、北西向、华夏、新华夏、旋扭构造体系等，这些构造体系的成生演化与该区金-多金属矿富集成矿有着密切的关系，尤其是构造体系的复合与联合、深部地质作用与构造体系的联系，是控制该区金矿的主要构造因素。
The result show , most of the medium - strong earthquakes faults are dip - slip reversed , distribution of the main stress p axis is sector from west to east ; there are large difference between kuche and baicheng region in seismic activities , but the characteristic of cluster is same in the two region ; the distribution of medium - strong earthquakes is nw direction in baicheng region , it show , there can have a concealed fault ; small earthquake clusters ' activities can reflect the effect that local medium - strong earthquakes to the secondary small structure around it 结果表明：南天山东段中强震震源断错以倾滑逆断为主，主压应力p轴由西到东呈扇形分布；相距较近的库车与拜城地区地震活动存在较大差异，但均存在明显的成丛性分布特点；拜城地区中强地震分布呈北西向可能预示著该区存在隐伏断裂，小震群活动则可能反映了局部中强震对周围次级小构造的影响。
The dislocation interfaces of early stage were controlled by the slide of the ne fold . the dominant dislocation interfaces , in the dam area , is the one of the second stage , which resulted from the slide of the lava layer and lagerkluftes from nw to se because of the affect of the majiaheba faultage ' s thrusting overriding to the dam area from nw to se . the dislocation interfaces of the third stage were the result of the overprint of the structure of ne to the one of nw 早期阶段形成的错动带受控于北东向纵弯褶皱的层间弯滑机制；第二阶段形成的错动带在坝区占主导地位，它们是由于北东向马家河坝断层由北西向南东的滑脱逆冲推覆影响坝区，并造成坝区向南东缓倾的岩层沿原生构造面向南东滑动的结果；第三阶段形成的错动带则是由于北西向构造叠加于早期北东向构造之上而致。
Especially interesting is the serpentinous peridotite in this belt occurred as lense blocks of various sizes , and superimposed with other geological masses with faults , and in combine to constitute the mixture . system in the belt . five tectonic stage can be discerned in this area : ( 1 ) south - north ward overthrust ; ( 2 ) sinistral strike - slip ( 3 ) dextral strike - slip ( 4 ) south - north ward overthrust ( 5 ) northeast , northwest late stage fault 本区上述的结构构造特征先后经历了五期构造作用，依次为： ( 1 )南北向逆冲推覆； ( 2 )左行走滑； ( 3 )右行走滑； ( 4 )南北向挤压推覆； ( 5 )北东向、北西向晚期断裂；
Northeast faults control the spread of the anhui riverway , and eastwest faults resulted in the widening of the river and the occurrence of nodes , then the stream raised and the riverway turn into goose pattern braided river . northwest faults and northsouth faults influence the evolvement of partial riverway , for example , the northwest lujiang - zhongming fault influence the evolvement of tongning shoals , and the northsouth faults passing through zongyang - digang make the riverway ' s direction from north - east to north - south 北东向断裂构造控制了皖江河型的展布；东西向断裂构造影响河道的拓宽，形成矶头，矶头挑流进一步使河道形成稳定的鹅头型；北西、南北向断裂影响局部河道的发育演变，如北西向庐江-钟鸣断裂影响铜陵沙洲的发育演变，南北向断裂影响枞阳、铜陵、获港河道使其延伸方向由北东转向南北向。
Jiyang depression is a field where nonhydrocarbon is rich . these resources have close relation with the activities of the volcanos . at the same time , the activities of volcanos have deep contact with the activities of the faults . the growth of the faults in jiyang depression is great . by the research of the index number of the faults growth and the other researches , nw direction faults are the most ones in mesozoic , nw and ne and approximately ew directions all exist in cenozoic . the above reflects the whole geotectonic background that sinistral shearing stress field exists in mesozoic , but dextral shearing stress field exists in cenozoic 这些气藏与火山活动有密切的成生关系，同时火山活动与断裂活动也有密切的关系。济阳坳陷内断裂活动极为发育，通过断层生长指数等的分析，推断中生代断裂以北西向为主，新生代则兼有北西向北东向和近东西向的断裂，上述断裂发育特征反映了该区的大地构造背景，在中生代是左旋的剪切应力场，在新生代则是右旋的剪切应力场。
Multistage structural deformations are experienced in kongquehe area , the basical fault systems of nww - near ew , nne - near sn , nnw and nee are established , the fault movement has the characteristics of multistage and inheritance , in the area multi - structural deformations are experienced in sinian to early ordovician , early ordovician - silurian , jurassic cretaceous - caenozoic , etc . late structural deformation shapes are changed for different levels of formar structural layer , in which different deforming shapes are created and integrated overlying of deformation is induced 摘要孔雀河地区经历了多期次的构造变形作用，形成了现今北西西近东西向、北北东近南北向、北北西向和北东东向基本断裂体系，同时断裂活动表现为多期性和继承性的特点；该区经历了震旦纪至早奥陶世、早奥陶世末志留纪、侏罗系、白垩纪新生代等多期构造变形作用，且后期的构造变形作用在不同程度上对前期的构造层的变形样式有所改造，形成了有一定差异的变形面貌，造成变形的复合登加。
The discourse think that the deposits are restricted by two nw - orientation geochemistry blocks , the ne - orientation structures and nne - orientation ruptures , that is to say , there are industry gold deposit when nne - orientation ruptures locate in two block and crossed by ne - orientation ruptures , but other region is difficult in forming ore beds 认为矿床的产出部位受两条北西向的构造地球化学条块、北东向断裂和北北东向断裂共同制约，即北北东向断裂在通过构造地球化学条块并有北东向断裂交叉时往往形成工业金矿床，而其它地区则难以成矿。
Chener gold deposit is located in north of xunmadao fault , the types of ore are gold - brazil - quartz of vein and gold - multimetal - quartz of vein . the occurrence of gold - bearing quartz vein is controlled by ductile - brittle shear zone , most the occurrence of gold - bearing quartz vein included by schistous zone and cracked zone , in the strike direction of gold - bearing quartz vein , it " s high content and great thickness appear on nww , in the direction of tilt , it " s high content and great thickness appear on the part of transformation from big angel of tilt to small angel of tilt 矿石类型为金-黄铁矿-脉石英型和金-多金属硫化物-脉石英型。含金石英脉受韧-脆性剪切带控制，主要赋存于片理化带与破碎带中。在脉体走向上，北西西向脉体品位高，矿体厚度大；在倾向上，南倾，倾角较缓处品位高、矿体厚度大。
The results show that the acting direction of tectonic stress field since the neotectonic ( the contemporary ) age has obvious zoning characteristics under the affect of near eastwestward tectonic stress field in the large area , i . e . , there is a nww compression in the north part of studied area , a nw compression in the west part , a ne compression in the east part 结果表明，研究区在大区域近东西向构造应力场作用下，新构造期现代构造应力场的作用方向具有明显的分区性，即北区呈近北西西向挤压；西区呈北西向挤压；东区呈北东向挤压。
