变形带的英文

• deformable zone
• deformatio and
• deformation bands
• deformation zone

• "变形"英文翻译    be out of shape; become defo ...
• "带"英文翻译    belt; girdle; ribbon; band; ...
• "变形带长度" 英文翻译 :    length of deformation band
• "变形带属" 英文翻译 :    amoebotaenia
• "低级变形带" 英文翻译 :    low-deformation zone
• "扭结变形带" 英文翻译 :    kink band
• "纹饰变形带" 英文翻译 :    amorphous band
• "正常变形带" 英文翻译 :    normal transformation zone
• "楔形变形带绦虫" 英文翻译 :    amoebotaenia cuneata
• "v形带" 英文翻译 :    v-belt; wedge shaped belt
• "y形带" 英文翻译 :    y bandage; y-bandage
• "齿形带" 英文翻译 :    cog belt
• "弓形带" 英文翻译 :    arcus
• "弧形带" 英文翻译 :    arcuate zone
• "环形带" 英文翻译 :    circumferential band; continuous belt; endless band; endless belt; endless loop built belt; endless loop tape; endless strip; tape loop
• "矫形带" 英文翻译 :    orthopaedic belt
• "梯形带" 英文翻译 :    ladder web
• "楔形带" 英文翻译 :    triangular belt; wedge belt
• "移形带" 英文翻译 :    transformation zone
• "变形" 英文翻译 :    1.(形状、格式起变化) be out of shape; become deformed; transshape; transfiguration; transformation; variant; transmogrification; modification : 自行车的前轮变形了。 the front wheel of the bicycle was out of shape. 孩子的腿变形了。 the child has a deformed leg.2.[物理学] (形变) deformation; distortion; (应变) strain; [生物学] (动植物的形态渐进) anamorphosis; (变异) metamorphosis; (畸形) dysmorphosis; (组织替换) transubstantiation; (器官变形) metallaxis; (物种演变) transmutation◇变形比 deformable ratio; 变形能力 deformability
• "v形带钢" 英文翻译 :    v-strap
• "齿形带带轮" 英文翻译 :    toothed belt pulley
• "帆布镫形带" 英文翻译 :    canvas stirrup
• "非环形带" 英文翻译 :    non-endless belt
• "复杂地形带" 英文翻译 :    complex terrain

• The places of gold ore is not only in the powerfulness place , but also in the place of tenacity - brittleness and the place of powerful deformation girdle place to the feeble the deformation in ductile zone gold bed
  韧性剪切带型金矿床中金的富集不仅在应变最强部位或韧性向脆性转换的部位，还可以在强变形带与弱变形域交接的部位。
• Another is shear - model fracture which is thought that it is associated with dislocation motion ( shear + rotation ) of crystal at microlevel , fragmentation of solid at mesoscale level and large plastic strains at the macroscopic level
  剪切型断裂在微观上与晶粒内或晶粒间的滑移和位错有关，细观上与集中变形带中的微剪切面集中有关，宏观上则与结构内的集中剪切带有关。
• 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。
• In the early period , the progressive cosxial compression caused the competent sodium - rich series and the uncompetent pelitic series to deform and partition , forming a lens - like weak - deformation domain distributed at approximate equidistance and a lineat srong - deformation zone respectively
  早期共轴递进挤压使能干性富钠质岩系与非能干性富泥质岩系发生变形分解，分别形成近等距分布的透镜状弱变形域与线性强变形带。
• Thermal deposits mainly formed during middle - late yanshanian age , related to extension structure , with main mineralization in qingfeng competent deformation zone , western shennongjia fault arch , northern huangling fault arch , xianfeng anticline of enshi platforman fold bundle
  热液型铅锌矿床主要形成燕山中晚期，与滑脱拆离构造密切相关，矿化主要集中于青峰强变形带、神农架断穹西部、黄陵断穹北部、恩施褶皱束咸丰背斜、长阳褶皱束走马坪背斜中。
• 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。
• Among them , the uncompetent pelitic series are cleaved in the srong - deformation zone with relatively high temperature , high pressure ; with weak hydrofracturing , the competent sodium - rich series dilatacying and forming microfracture ( ie , embryonic fracture ) in the core of the weak - deformation demain , which is a natural lens - like pumping centre with relatively low temperature , low pressure and high permeability
  强变形带中的非能干性泥质岩系强烈劈理化，为相对高温高压带；弱变形域内的能干性钠质岩系则伴随弱水力压裂作用发生扩容，形成雏形断裂的微裂隙，同时，它是一个相对低温、低压、高渗透率的透镜状天然泵吸中心。

• 变形带的日语：へんけいたい