The discourse discusses structure pattern , rupture - distributing law and ore - controlling action about mouru ore belt . grasping distribution rule of the fractures in ore - forming zone by remote sensing analyse and field survey , and made a research about the ruptures " ore - containing character in the different orientation , putting forward that four ne - orientation structure containing - ore zone alternate with strong and feebleness 论文详细地论述了牟乳含矿带的构造格局、断裂分布规律及控矿作用，通过遥感构造解译和实地考察，从宏观上整体把握了区域上和成矿带内断裂的分布规律，对不同方向上断裂的含矿性做了研究，并提出了牟乳矿带内北东向的四个强弱构造含矿带。
The results indicate : ( 1 ) the distribution of magmatic rocks shows the feature that in the middle and western part of the study area basic igneous rocks dominate , and in the middle - eastern part intermediate rocks are predominant , while in the southeastern part acid ones are developed . ( 2 ) in the area west to the shiwandashan basin , intermediate magmatites were controlled by deep ne - striking and nw - striking faults , especially at the conjunction site of these two group faults , magmatic activity was strong ; and its tectonic background can be attributed to extensional continental rift 其中，在十万大山盆地以西地区的偏基性岩浆活动受北东和北西向深断裂控制明显，尤其以此两组断裂交汇处的岩浆活动强烈，盆地构造背景属大陆伸展裂谷环境；在十万大山盆地以东地区为偏酸性岩浆活动，主要受东吴运动形成的钦防造山带的控制，属大陆边缘造山带或岛弧造山带环境。
There are two sets of elements geochemical anomalies : one extends nw , and is controlled by regional faults ; the other extends ne , and intersects with the former taking on " v " form , and is important to mineral exploration . 3 . almost all au deposits are situated in greenstone belt of tectonic sutures 元素地球化学场表现出两个方向的特点：一组异常呈北西向展布，受区域构造控制；另一组异常呈北东向展布，与北西向异常交叉呈“ v ”字形，具有重要找矿意义。
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。
The good reservoir facies are braided stream and braided delta in alaer area , fan - delta in arhati area and lake - floor fan in shizigou - ganchaigou area . all of these areas are the main targets for oil exploration , it has discovered that there is an important unconformity between upper youshashan and lower youshashan formation of tertiary , on which there are a large amount of erosion and long time of depositional hiatues 在上述研究的基础上，对区内油气勘探的有利区带进行了预测，指出阿拉尔北东辫状河三角洲相带、阿哈提南东扇三角洲相带和狮子沟一干柴沟湖底扇相带为区内有利的储集相带，是今后勘探的主要目标。
It is believed that three northeast - striking dextral slip fault zones , i . e . the baxian - shulu - handan fault zone , the huanghua - dezhou - dongming fault zone , and the linyi - huanghekou fault zone , are the result of the tectonic transform of paleogene extending to neogene - quaternary laterally slipping of north china plain rift systems , which extend along the central axis of rifts and accord with the quaternary centers of subsidence as the main seismic structures within the rifts 认为坝县束鹿邯郸断裂带、唐山河间磁县断裂带和黄骅德州东明断裂带3条北东向右旋走滑断裂带为华北平原裂谷系从早第三纪伸展拉张作用进入晚第三纪第四纪走滑剪切拉张作用的产物，这3条断裂带分别位于3个北东向坳陷带中部，并构成了第四纪沉降中心，与营口潍坊断裂带起构成华北平原内的主要强震构造。
The fault controlled the magmatism and metallization relevant to the contact zone , and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene . the fault zone deformed right - laterally under ne - sw striking transtention , and new joints zone was produced at the end of the two main faults because of local stress concentration . the fault produced inchoative cataclastic rocks , and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks , which was during the himalayan movement 其后的继承性活动在断裂带内形成碎裂程度最强达到碎裂岩的碎裂岩系列构造岩，变形带两侧发育两组典型的共轭剪节理；第二次在晚白垩世?始新世，断裂在北东?南西向近水平挤压作用下右行张扭性活动，断裂带两主断裂在斜列重叠的端部由于局部应力集中进一步扩展形成节理带，而断裂在岩体区也发育两组典型的共轭剪节理，断裂内形成初碎裂岩为主的构造岩；第三次是喜山期以西侧抬升、东侧下降的强烈升降为主的活动，在基岩中，主断层两侧围岩出现微破裂。
There is a north - north - east negative anomaly belt of aerial magnetism in the middle - east part of the basin , which could be displayed by the aerial magnetism of commutative field , upwardly continuation , lvt in earthquakes , the experimentation of granite liquation ( demagnetization ) , the distribution of neozoic era volcanic rock , earthquake , hot spring and ground feature . the anomaly shows the blocking in east - west direction , and it is also associated with intense activity of deep heat interaction and the development of the crust - mantle mixed layer in the north qiangtang 从区域航磁、向上延拓、地震低速层、花岗岩熔融(退磁)实验、新生代火山岩的分布、地震、温泉、地貌等发现，盆地中东部存在一北北东向航磁负异常带，既显示出东西分块，也与北羌塘深部热力作用强烈活动、发育“壳幔混合层”有联系。
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。
