构造侵位

  • 网络tectonic emplacement
构造侵位构造侵位
  1. 瓦房复背斜水文地质条件及找水方向初论宝兴复背斜的构造侵位

    A first discussion on the tectonic emplacement of Baoxing anticlinorium , sichuan

  2. 喜马拉雅造山带中段麻粒岩构造侵位过程中变质变形演化

    Evolution of Deformation and Metamorphism During the Tectono Emplacement of the Granulite in the Middle Himalaya Orogen

  3. 花岗岩构造与侵位机制研究进展

    Advances in granitic structures and emplacement mechanisms

  4. 南岭钨锡多金属矿床成矿系列与构造岩浆侵位接触构造动力成矿专属

    Ore-forming specialty of the tectono-magmatic zone in Nanling region and its emplacement dynamics for metallogenic series of W-Sn polymetallic deposits

  5. 安徽董岭花岗岩类的构造特征及侵位机制

    Structural characteristics and emplacement mechanism of granitoid in dongling , anhui , China

  6. 磁面理的产状与岩体形态和岩石单元分布相吻合,清晰地反映了不同构造单元岩浆侵位方式;

    The attitude of magnetic foliation , which clearly suggests the emplacement of the magma in different tectonic units , is consistent with rock shapes and distribution of rock units .

  7. 岩石属于大陆板内张性构造环境下高侵位形成的壳源重熔型花岗岩类。

    The rocks are crustal remelting , shall level granites formed in a within-plate tensional tectonic environment .

  8. 根据上述特征,将该超单元岩浆侵位变形构造划分为强侵位变形、中等侵位变形、弱侵位变形及基本无侵位变形4个带。

    According to the above-mentioned features , the magmatic emplacement deforma-tional structures of this super-unit is classified into strong emplacement deformation , moderate emplacement deformation , weak emplacement deformation and essentially no emplacement deformation zones .

  9. 作为阜平幔枝构造轴部岩浆侵位的代表性岩体之一,麻棚岩体是岩浆多期次脉动侵入过程中的典型产物,空间上形成典型的多单元环状结构杂岩体。

    It is one of representative granitic intrusion in the axis of Fuping mantle branch structure , also is product of multi-stage pulsating process of the intrusive magmatism , which lead to form typical multi-unit ringed complex spatially .

  10. 本文主要讨论花岗岩类岩浆在不同构造环境下对岩浆侵位方式的控制机理,并提出在一个完整的岩浆演化序列中,受构造活动影响发生侵位方式改变的可能性。

    This paper discusses mainly the tectonic condition of the formation of granitoid magmas , the control mechanism of different tectonic environment for emplacement fashion , and poses a possibility of transformation of emplacement fashion as a result of tectonic active in a complete evolution of magmas .

  11. 鲁西的两个岩石单元沿北北西向古构造带拼贴,沿古构造带侵位一些深成闪长岩体。

    These two areas were amalgamated together at the latest Neoarchean along the NNW-trending paleo-structural belt with intrusion of some plutonic diorite bodies .