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构造期的英文

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"构造期"怎么读用"构造期"造句

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  • tectonic epochs

例句与用法

  • Application of acoustic emission in the study of the number of cenozoic tectonic phases in the dongying subbasin
    利用声发射研究东营凹陷新生代构造期
  • According to mineralization characteristic in ore - hosted strata , it is suffered from four stages structural rework . , and its reason is discussed in this paper
    根据含矿岩系中的矿化特征,认为含矿岩系主要遭受了4个构造期次的构造变形,并探讨其构造成因。
  • In order to find new pegmatite nb - ta ore - deposit , it is very important practical - significances to ascertain the host structure characteristics and the relations between the tectonic epochs and ore - forming
    通过查明矿床的容矿构造特征以及构造期次与成矿的关系,对寻找新的铌钽伟晶岩矿床具有重要的实践意义。
  • The middle cambrian early devonian ( 513 - 397ma ) tectonic stage was characterized by a series of tectonic events with different features , which are completely different from the caledonian event that occurred in the appalachian orogen and in scotland
    摘要中国大陆早古生代(中寒武世早泥盆世)构造期以发生系列各具特征、分布局限、准同时的构造事件为特征。
  • The results show that the acting direction of tectonic stress field since the neotectonic ( the contemporary ) age has obvious zoning characteristics under the affect of near eastwestward tectonic stress field in the large area , i . e . , there is a nww compression in the north part of studied area , a nw compression in the west part , a ne compression in the east part
    结果表明,研究区在大区域近东西向构造应力场作用下,新构造期现代构造应力场的作用方向具有明显的分区性,即北区呈近北西西向挤压;西区呈北西向挤压;东区呈北东向挤压。
  • Through the all - sided tectonic analyses , it can be deduced that there are two aspects will be the hidden defects to the dam and the engineering stability of the reservoir area . one is the dislocation interfaces resulting from the the majiaheba faultage ' s thrusting overriding and other causes of formation . the second is the region of strong deformation , such as the above of the dam , middle and high positions of the lava layers and the regions of overprint of the structure of ne to the one of nw , which should be taken into account especially
    通过区域和坝区错动带的全面构造解析,认为由马家河坝断层逆冲推覆作用而在坝区形成的向金沙江下游缓倾的错动带以及其它成因的错动带是坝区和库区工程稳定的隐患,尤其是变形较强的坝址区上游区、中高层位以及北西向构造期的错动带叠加于北东向构造期错动带的部位,更应该引起足够的重视。
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