紫荆关 meaning in Chinese
zijingguan
Examples
- However , there are joints without any tectonites at the end of the two main faults
而乌龙沟断裂南端和紫荆关断裂北端是缺少碎裂岩带的节理带。 - Since the fault zone had been activated in the later paleozoic , it controlled the evolution of magmatism and metallization belt in taihang mountains . our field workspace is in the northern part of taihang mountains , which is the diagonal area of two main faults
太行山北段是紫荆关断裂带两主断裂斜列重叠部位，通过对该区作详细的野外断裂构造剖面观测，比较详尽地收集了断裂带构造组合资料及构造岩标本。 - 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。 - Zijingguan fault zone is the main structure in taihang mountains that are located in the central part of 20 ~ 30 ne - striking daxing ' anling - taihan - wuling tectonic belt . it is composed of two diagonalized faults that are wulonggou - shanghuangqi fault located in the west and zijingguan - lishan fault in the east
紫荆关断裂带是大兴安岭?太行山?武陵山构造带中段太行山地区的主体构造，总体走向20 30 ，由西侧的乌龙沟?上黄旗断裂和东侧的紫荆关?灵山断裂左阶斜列组成。 - Detailed structural information and specimens of tectonic rock had been collected in the outcrop sections along the fault zone , and deformation feature and superposition about the tectonic rocks were analyzed , and paleotectonic stress field was also analyzed by stereograms illustrating of joints in the following work
在室内对构造岩进行了变形特征和变形叠加分析，对断裂带典型共轭剪节理作主应力轴图解分析了古构造应力场。进而探讨了紫荆关断裂带的构造活动特征。