陆陆碰撞

  • 网络Continental collision
陆陆碰撞陆陆碰撞
  1. 结合区域构造背景,认为银洞沟银矿形成于陆陆碰撞体制,并可以借助CMF模式解释成因。

    Considering the tectonic evolution of the host terrane , we suggest the deposit was formed in continental collision regime and the CMF model can be used to interpret its origin .

  2. 羊八井热田是属于陆陆碰撞板缘非火山型高温地热田。

    The Yangbajing Geothermal Field is one of non volcanic high temperature geothermal fields .

  3. 实验结果表明,陆陆碰撞是岩石圈或地壳缩短和增厚的主要机制之一。

    Experimental results have already indicated that the continent continent collision is one of the principal mechanism to lead to lithosphere / crust thickening and mountain building .

  4. 新近纪以来,受南面印度欧亚陆陆碰撞的影响,天山地区发生强烈陆内变形,以逆冲推覆和褶皱堆叠为特征;

    Since Neogene , a collision between Indian and Eurasian plates took place in the southern side of Tianshan belt , causing a strong intra-continental deformation characterized by thrusting and folding .

  5. 扬子板块和华北板块在晚三叠纪末完成陆陆碰撞,东秦岭地区进入陆内造山演化阶段,形成区域上北西-近东西向基本构造格架。

    After the continent to continent collision of the Yangtze and North China Craton in the late Triassic , the basic near EW-NW tectonic lines in east Qinling orogen are formed in the following intracontinental orogeny .

  6. 由此而论,可能存在着华北板块与扬子板块相向俯冲于苏鲁地体之下的陆陆碰撞机制,苏鲁地体可能具有与大别地体相似的花状造山带结构。

    As a result , a collision mechanism is perhaps present between continents where North China plate and Yangtze plate subducted to each other below the Sulu terrene which has the same flower-shape orogenic structure as that of Dabie terrane .