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伸展构造的英文

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"伸展构造"怎么读用"伸展构造"造句

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  • extensional fault
  • extensionalfault

例句与用法

  • Physical experiments on continent extensional structures
    用物理模拟实验研究大陆伸展构造
  • Sichuan basin ; extension compression ; dynamical environment ; extensional structures ; inversion structures
    四川盆地拉张-挤压动力学环境伸展构造反转构造
  • The main structure style of chagan sag included four kinds , such as extension , compression , inversion and strike - slip structure , in which the extension structure was the principle part
    查干凹陷的主要构造样式包括伸展、挤压、反转和具有走滑分量的构造,其中伸展构造是主体。
  • The structure units are redivided . the main structure style of chagan fault depression is summarized , in which the extensional structure are the principle part . its kinematics characteristics are analysed
    对查干凹陷的构造单元重新进行了划分,总结了查干凹陷的主要构造样式,伸展构造是主体,并对其运动学特征进行了分析。
  • This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement , whose tectonic deformation and magma intrusion is fiercely , and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian , it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area , such as a - granite ' s stock , batholiths and diabase ' s dike . there are many fault depressions possible
    按照不同构造层,研究了各构造层的构造特征:基底构造层:受早海西期构造作用的影响,与准噶尔洋盆俯冲闭合、而后陆-陆碰撞的区域挤压构造作用有关,为一构造变形和岩浆侵入活动强烈的古生代褶皱基底。二叠系构造层:受中海西区域性伸展断陷作用的影响,盆地及其周缘地区发育与伸展构造有关的构造-岩浆组合,如呈岩株、岩基状侵位的a型花岗岩以及呈岩墙状侵位的辉绿岩等。
  • Viewing from the global tectonics , the authors dynamically described the dialectical relationships between extensions and compressions in time special 4 - d , and pointed out the different tectonic deformation systems corresponding to different tectonic dynamical environments . considering the geological evolution of sichuan basin , from nine aspects , the authors proved that the tectonic dynamical environments of sichuan basin , after its formation , has experienced the early extension , middle transition and late compression environments . correspondingly , as the paper suggests , a considerable attention need to be paid to the comprehensive studies of the early extensional structures , middle inversion structures and the late compression structures of sichuan basin when analyzing its tectonics
    从全球构造着眼,动态地从时间-空间四维阐述了拉张-挤压构造动力学环境的辩证关系,指出了不同构造动力学环境对应于不同的构造变形系统。结合四川盆地地质演化历程,从9个方面论证了四川盆地自其形成以来,构造动力学环境曾经历了早期拉张中期过渡晚期挤压的过程,相应地在对四川盆地进行构造分析时,要注意早期伸展构造中期反转构造晚期挤压构造的识别和综合研究。
  • The extending major fault has a strike of north - east , controlling the forming of depressions and evolution of sedimentation . the nature of the fault is normal in the early stage . later with the reformation of sliding effect , normal faults are still the main faults , and the plane distribution of the faults occurs sectionally
    取得了一系列的研究成果:辽河滩海地区主要有三种构造样式,即伸展构造样式、走滑构造样式及反转构造样式,其中,以伸展构造样式为主,伸展主干断裂走向以北东走向为主,控制凹陷形成和沉积演化,断裂性质早期为正断层,后期经走滑作用改造,至今仍以正断层形式出现,断裂平面展布具有分段性。
  • The paper gives a mechanical and history analysis on the characteristic of laojunshan metamorphic core complex in southeastern yunnan and its structural environment , and considers that metamorphic core complex is actually a nuclear column of a vortex structure , which was caused by the wenshan ? malipo strike - slip fault
    通过滇东南老君山变质核杂岩特征及周围构造环境的力学分析及历史分析认为,该变质核杂岩实质上是旋扭构造的砥柱,而旋扭构造又源于文山?麻栗坡断裂的走滑运动,拆离伸展构造晚于旋扭构造。
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