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韧性剪切带的英文

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"韧性剪切带"怎么读用"韧性剪切带"造句

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  • ductile shear belt

例句与用法

  • The component variation and volume loss of xiaotieshan shear ductile zone in baiyin ore field , gansu province
    甘肃白银厂小铁山韧性剪切带体积亏损与成分变异
  • Ductile zone is anxious the brining guides the structure in mine and accuseeing the mine , rong kuang constitutes
    韧性剪切带既是导矿构造,也是控矿、容矿构造。
  • In this paper the author discusses the petrography feature of the rock in the scale ductile shear zone and the characteristics of the shear belt
    本文主要从岩石学的角度论述了两条韧性剪切带内的岩石岩相学特征,讨论了韧性剪切带以及剪切带内岩石的特征。
  • 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。
  • The lower member of typical ophiolite suit is exposed at outsides of the qimanyuter ophiolite melange and in between , there distribute the basalt , deep sea limestone and silicalites . these different litho - members contact to each other with ductile shear zones
    带内蛇绿岩套下部单元出露于两侧,玄武岩和相关的深水灰岩、硅质岩等分布于中部,各单元间均以韧性剪切带接触。
  • The huachanggou gold deposit lies in the south of mianlue fold bend , in the triangle area of mianluening , the south of the qinling mountain orogenic zone . this deposit ' s happening and development have been controlled by ductile zone , as ductiled gold deposit
    铧厂沟金矿床位于秦岭造山带南部勉-略-宁三角地区勉-略断裂带以南。本矿床的发生、发展受韧性剪切带控制,属于韧性剪切带型金矿。
  • 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。
  • 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。
  • 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。
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