紫荆关的英文

• zijingguan

• "紫荆"英文翻译    Chinese redbud; judas tree
• "关"英文翻译    close; shut
• "紫荆" 英文翻译 :    [植物学] chinese redbud; judas tree
• "艳紫荆" 英文翻译 :    bauhinia blakeana
• "洋紫荆" 英文翻译 :    bauhinia blakeana
• "紫荆果" 英文翻译 :    chinese redbud fruit; fruit of chinese rebud; fruit of chinese redbud
• "紫荆花" 英文翻译 :    cercis; flower of chinese redbud; redbud
• "紫荆木" 英文翻译 :    madhuca pasquieri; wood of chinese redbud
• "紫荆皮" 英文翻译 :    bark of chinese colden erdbud; bark of chinese redbud; chinese redbud bark; cortex kadsurae radicis; kadsura root-bark; zijingpi lignum cercis chinensis
• "紫荆山" 英文翻译 :    zijing shan
• "紫荆属" 英文翻译 :    cercis; redbud
• "紫荆厅" 英文翻译 :    redbud room
• "紫荆丫" 英文翻译 :    engler abelia fruit or flower
• "【植物；植物学】紫荆。" 英文翻译 :    redbud
• "垂花紫荆" 英文翻译 :    c.racemosa
• "大紫荆勋章" 英文翻译 :    gbm; grand bauhinia medal
• "海南紫荆" 英文翻译 :    madhuca hainanensis
• "海南紫荆木" 英文翻译 :    madhuca hainanensis
• "黄山紫荆" 英文翻译 :    c.chingii
• "加拿大紫荆" 英文翻译 :    c.canadensis
• "金紫荆广场" 英文翻译 :    golden bauhinia square
• "金紫荆奖" 英文翻译 :    golden bauhinia awards
• "金紫荆星章" 英文翻译 :    gold bauhinia star [gbs
• "美国紫荆" 英文翻译 :    redbud
• "南方紫荆花" 英文翻译 :    bauhinia purpurea

• 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。
• Those two phases of conjugated shear joints are differ from each other in spatial distribution , which is a reflection of the spatial evolution of the fault zone . it can beinferredfrom the information about macrostructure , superimposed deformation of tectonites , paleotectonic stress field of joints and other related documents that there had been three stages of significant activity since zijingguan fault zone was activated . the first stage was about from middle juiassic to early cretaceous , when the fault zone activated left - laterally under nw - se striking transpression
  宏观构造组合特征、构造岩变形叠加信息、节理的古构造应力场信息及前人区域资料表明，紫荆关断裂带自古生代末开始活化以来有三次主要构造活动：第一次是中侏罗世?早白垩世，在北西?南东向近水平挤压作用下，断裂左行压扭性活动，控制太行山地区岩浆岩带及与其相关的接触交代型矿床的形成。