裂谷系

  • 网络rifting;rift system
裂谷系裂谷系
  1. 汾渭地堑与贝加尔裂谷系的比较构造分析

    Comparative tectonic analysis of FEN-WEI graben and Baikal rift system

  2. 论中国东北大陆裂谷系的形成与演化

    On the origin and evolution of continental rift system in Northeast China

  3. 东北大陆裂谷系的形成与地震活动

    Continental rift valley system and seismic activities in Northeast China

  4. 试论航磁异常与北疆裂谷系

    On aeromagnetic anomaly and rift system in Northern Xinjiang

  5. 鲁西裂谷系的地质特征及演化

    Geological characteristics and evolution of Luxi ( west Shandong province ) rift system

  6. 渤海湾裂谷系的含油性

    Oil potential of Bohai Gulf rift system

  7. 山西裂谷系的深部地球物理探测

    Deep geophysical exploration of Shanxi rift system

  8. 渤海裂谷系的形成和演化

    Formation and evolution of Bohai rift system

  9. 杨子地台北缘裂谷系构造初析

    Preliminary analysis of the structures in the rift system at the northern margin of the Yangtze Platform

  10. 在晚白垩世&始新世夷平面基础上,由于断裂作用形成了贝加尔裂谷系。

    The Baikal rift system was formed due to faulting on the late Cretaceous ? Eocene . Epoch planation surface base .

  11. 依据世界主要裂谷系的基本特征,提出了新的裂谷分类。

    According to the basic characteristics of the major rift systems in the world , a new classification of rifts is proposed .

  12. 认为在区域拉张应力场作用下,汾渭裂谷系为盆山耦合形成,其形成模型为伸展造山,断陷沉盆,后推成台;

    The model is that the mountain , basin , and platform were formed by extension , subsidence , and tectonic push , respectively .

  13. 中国大陆中部中晚元古宙复合三叉裂谷系及演化初析

    A preliminary analysis for the recurrent three arm rift systems and evolution of the central part of the Chinese continent during the middle Late Proterozoic

  14. 凤太铅-锌矿田位于华北地块和扬子地块间的秦岭古生代陆间裂谷系南部裂谷之中。

    The Fengtai Fengtai Pb-Zn ore field is located within the south rift valley of the Paleozoic Qinling intercontinental rift system between the North China and Yangtzeplatforms .

  15. 中三叠世,个旧矿区处于特殊的沉积环境&陆裂谷系中的局限边缘海盆。

    During Middle Triassic , the Gejiu area was in a special sedimental environment , i.e. in a restricted marginal sea basin within the continental rift system .

  16. 山西地堑系是一个由一系列方向不同的断陷盆地及盆地内部次级构造组成的新生代大陆裂谷系。

    The Shanxi rift system is a continental rift that composed by a series of fault basins with different directions and the secondary structions in the fault basins .

  17. 鄂尔多斯地块西南部早古生代为界于秦祁贺三叉裂谷系之秦岭、贺兰裂谷间的大陆边缘。

    The southwestern part of the Ordos Block was a rift continental margin opened to the Qinling and Helan trough of the Qinling-Qilian-Helan three-arm rift system in Early Paleozoic .

  18. 本项研究成果支持华南裂谷系沉积超覆的开启时间为820Ma左右的观点。

    The results of research in this study strongly support the viewpoint that the initial age of the sedimentary onlap within the Nanhua rift systems should be dated at ca. 820 Ma .

  19. 利用地质和地球物理资料论述了渤海裂谷系存在的科学依据。总结和归纳了渤海裂谷系形成和演化的过程。

    This paper discusses the scientific basis of existing Bohai rift system based upon a large number of geological and geophysical data , and comprehensively summarizes formation and evolution of the Bohai rift system .

  20. 鄂尔多斯盆地西缘古生代槽台过渡带裂谷系弧形构造带的形成与发展及对油气聚集富集规律的影响

    The influence to the accumulation of oil and gas , of the development of the arcuate structure zone in the transition zone from the plat to the geosyncline in the west of Ordos Basin

  21. 熊耳裂谷火山岩系金-多金属矿床成矿模式

    The genesis model of the gold-polymetal deposit from the volcanic rocks in the Xiong'er rift

  22. 丰富的铜质来自巨厚的裂谷火山岩系(橄榄拉斑玄武岩)。

    Abundant copper material was derived from volcanic rock series ( olivine tholeiite ) in the rift .

  23. 滇黔桂裂谷②湘桂断裂系;

    THE YUNNAN-GUIZHOU-GUANGXI RIFT SYSTEM ( 2 ) Hunan & Guangxi fracture series ;

  24. 黄骅裂谷盆地第三系水循环和渗流场形成演化的重溯

    Tertiary water circulation and vadose field formation and evolution of Huanghua rift basin

  25. 黄骅裂谷盆地第三系深层水成因

    Tertiary Deep Water Genesis in Huanghua Rift Basin

  26. 黄骅含油气裂谷盆地第三系地下水化学场及其形成演化模式

    Tertiary Groundwater Chemical Field and Pattern of Its Formation and Evolution in Huanghua Oil Gas-Bearing Rift Basin

  27. 辽河盆地为中国东部大陆裂谷渤海湾裂谷系的北延部分,是中、新生代发育起来的断陷盆地。

    Liaohe Basin is situated at the northern section of the Bohai Bay rift system . It is a fault depression developed in the Mesozoic and Cenozoic .

  28. 岩石地球化学特征表明,无论是基龙组火山岩还是色龙群火山岩,都具有大陆拉伸-大陆裂谷环境火山岩系的主、微量元素地球化学特征。

    Volcanic rocks of both the Jilong Formation and the Selong Group show major element , trace element and REE geochemical characteristics of the volcanic series occurring in the continental extensional-rift environments .