羌塘地块

  • 网络qiangtang block
羌塘地块羌塘地块
  1. 印支期主要呈NW-SE向和NNE-SSW向、SN向,主要受中特提斯构造动力体系中羌塘地块与欧亚大陆碰撞拼贴产生的远程构造效应影响;

    During the Indosinian movement , the directions of the major tectonic stress fields are along NW-SE , NNE-SSW and SN , which were basically resulted from the collision between the Qiangtang block , a part of the Tethyan dynamic system , and the Eurasian plate .

  2. 羌塘地块、拉萨地块及喜马拉雅地体和印度洋板块向北漂移与欧亚大陆的拼合是柴北缘盆地形成演化的主要动力来源。

    The Qiangtang block , the Lhasa block , the Himalayan block and the Indian plate drift northward and combine with the Eurasian continent , which are the main power sources of formation and evolution of the northern margin of Qaidam Basin .

  3. 论羌塘地块结构的不均一性和深部信息

    Information model of construction machinery CAID On Structural Anisotropism of the Qiangtang Massif and Deep Information

  4. 对青藏高原羌塘地块中部双湖地区发育的二叠系碱性系列和拉斑系列玄武岩进行了详细的地球化学研究。

    This paper reports the petrological and geochemical characteristics of Permian alkaline and tholeiitic basalts in the Shuanghu Area , central Qiangtang Block .

  5. 根据藏北羌塘地区最新地质、地球物理资料(以MT为主)综合分析,对比西部和东部综合剖面各单元结构特征,发现羌塘地块结构不均一性特征明显。

    Based on synthetic analysis of recent geological and geophysical data ( mainly from MT survey ) and the comparison of the structural features between the west and east composite profiles , the authors have found very obvious anisotropic features of the structure in the Qiangtang massif .