The ground stress distribution within southern margin of junggar basin assumes that its compressing stress increases vertically with depth and compatible with the structural layers ， which can be divided into deep compressive belt ， medium shear zone and shallow tensile fracture belt 盆地南缘区域地应力分布规律表现为纵向上压应力随深度增加而增大,并与构造层配伍,可分为深层挤压带、中层剪切带、浅层张裂带。
The plane strain tests of sand and clay , and the emergence and development of shear bands were simulated numerically by pfc to analyze the stress - strain relationship curves of pfc models and test results under different confining pressures 对砂土和粘性土的室内平面应变试验及其剪切带形成和发展进行了数值模拟，分别对比了不同围压下颗粒流试样与室内试验的应力应变关系曲线，基本再现了砂土和粘性土试样应力应变关系。
According to the test results of localization and shear bands formation under the consolidated undrained plane strain compression tests on soft clay in shanghai , it was found that the deviator stress of shear band beginning to form was very close to its yield point in clay soils 摘要根据上海软土在固结不排水平面应变压缩试验条件下应变局部化和剪切带形成的实测研究结果，发现粘性土剪切带开始形成的偏应力为其屈服点。
In the process of writing paper , assimilating sufficiently procedessor " research achievement , exertting ductile - brittle shear zone , resolving mechanism of formation of gold - bearing quartz vein of chener . lining out ductile - brittle shear zone of chener gold deposit , presenttig pattern of controlling chener gold deposit , with analyzing of dominant ore vein - q507 , graph of change of trace element on different spot level and graph of change of gold element of different construct , researching construct geochemistry of ore zone 在论文撰写的过程中，充分吸收前人的研究成果，运用韧性剪切带理论，解析了陈耳金矿区含金石英脉体的形成机理，划出了控制陈耳金矿床的韧-脆性剪切带，提出了矿床的构造控矿模式。
The division of regional structural systems in the study area , the timing and distribution range of the ductile shearing zone and the metamorphic core complex , and their compounding were made by the author in the light of results of the synthetic study on geology in deep , geophysical prospecting , and interpretation of remote sensing image 结合深部地质、物探和遥感解译资料，划分了辽东巫闾山地区构造体系和构造带归属、韧性剪切带与变质核杂岩的时代、范围分区及其复合关系。
In the resin matrix composite materials filled with fsmf , the load is undertaken by the grain of fsmf and the resin matrix . the grain of fsmf restricts the deformation of the resin matrix , so the strength is improved . furthermore , the grain of fsmf can consume the energy of strain and controls the crack expand , so build up toughness 在fsmf填充树脂复合材料中，载荷是由fsmf颗粒和树脂基体共同承担的， fsmf颗粒以机械约束方式限制树脂基体变形，从而产生强化； fsmf颗粒可以引发银纹和剪切带等损伤消耗应变能，并通过钝化和钉扎机制阻碍裂纹的扩展，从而产生增韧。
Different rock mass on the remote sensing images were obtained , based on a comprehensive remote - structure analysis , a new acknowledge on the characteristics of regional structure in tonghuashan - yushugou area was acquired . it was suggested that tonghuashan - yushugou area underwent multi - phase structure movement , multi - phase , multi - orientation > multi - level deformed structure superimposed each other accompanied with complex deformation 通过遥感?构造的综合解析，总结出从遥感图像上辨识高压麻粒地体、韧性剪切带、叠加褶皱及不同应变带、不同类型面理和不同岩体的图像处理方法，并获得榆树沟?铜花山地区区域地质特征的重新认识。
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 large - scale composite ductile shear zone around laerdun daban is analyzed into three stages including horizontal dispatch , uplift by compression and magrnatic intrusion , and dextral strike - slip ductile shearing , respectively of late early paleozoic to early late paleozoic , late devonian , and permian - triassic ages 摘要拉尔敦达坂一带发育的大型复合式韧性剪切带，经解析分为水平拆离、挤压和岩浆侵入隆升、左行走滑韧性剪切三个不同阶段，变形时限分别限定在早古生代晚期至晚古生代早期、晚泥盆世和二叠三叠纪。
Numerical viscoelastic modeling for porphyroclast rotation in ductile shear zones is done by a viscoelastic finite element program based on detailed investigation to three ductile shear zones , the taihangshan mountains , north china . in this model porphyroclast garnet is assumed as isotropic elastic material with small elastic deformation , while the matrix quartz , feldspar as viscous fluid maxwell material which has increasing deformation with time . the viscosity of matrix is supposed to be 10 采用粘弹性力学分析程序对太行山阜平地区剪切带中斑晶旋转问题进行了有限元数值模拟。在计算模型中假定：石榴石斑晶为弹性材料，在应力作用下只产生很小的弹性变形石英长石质的基质部分为粘弹性材料，它具有随时间变形不断增大的特性。
