cataclastic rock meaning in Chinese
碎裂岩
压碎岩
Examples
- Practices on bolt , mesh , anchor and beam support in coal drift under unstable roof condition of cataclastic rock mass
不稳定顶板煤巷锚网索梁支护实践 - Three stages of deformation can be distinguished from the cataclastic superposition of matrices that infilled the microcracks in cataclastic rocks , and two phas es of paleotectonic stress field from the typical conjugated shear joints by stereograms illustrating
构造岩中胶结物和微裂隙充填脉反映了岩石碎裂变形的三次叠加。断裂变形带内发育两期典型的共轭剪节理，但区域分布各有特点，反映出断裂变形的空间演化。 - Zijingguan fault zone is characterized with cataclasite series of tectonic rocks and joints alongside the deformational zone , and sometimes with uniclinal flexure or folds . the intensity of deformation increases from the sides to the center of the fault in the section , which appears from joints to cataclastic rocks
紫荆关断裂带两主断裂变形带以碎裂岩系列构造岩和节理带组合为特征，局部出现挠曲和褶皱，由两盘至断裂中心变形强度增大，一般由节理带过渡为碎裂岩带。 - 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。 - It is further indicated by the fusion of various geo - factors that the major targets include gold - bearing limonitic cataclastic rock in ningwei domain , auriferous quartz in nanhua mountain and xihua mountain domain , where the 50 - 85 strike mylonite and sulfur - bearing quartz - calcite veins of cataclastic rock is the prior ore - search targets
同时，通过多源地学因素的融合还显示，宁卫地区找金的主攻对象以含金褐铁矿化碎裂岩为主，南华山、西华山地区以脉型金矿为主，且重点应在50 - 85度方向糜棱岩、碎裂岩带中寻找含硫化物的石英-方解石脉。