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OALib Journal期刊
ISSN: 2333-9721
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三塘湖盆地及其周缘地区古生代构造演化及原型盆地研究
Keywords: 原型盆地,构造演化,裂谷盆地,古生代,三塘湖盆地
Abstract:
？在早古生代，三塘湖地区是吐哈地块的组成部分，位于地块北缘，具有弧—沟—盆系统的结构特征。到志留纪末期，阿尔曼太古洋盆发生闭合碰撞作用形成了阿尔曼太碰撞带。进入早泥盆世，在吐哈地块北部、三塘湖地区早古生代岛弧南侧发生裂解、扩张作用，形成了克拉麦里古洋盆，从而使三塘湖地块从吐哈地块中分裂出来。在中泥盆世—早石炭世时期，克拉麦里古洋盆发生双向俯冲作用，北侧的三塘湖地块再次形成火山弧火山—沉积建造，南侧形成了哈尔里克火山弧及弧后裂谷盆地并接受相应的火山沉积岩系；早石炭世末期，克拉麦里古洋盆发生持续时间较为短暂的闭合碰撞作用，形成了克拉麦里碰撞带，之后进入后碰撞伸展演化阶段；至晚石炭世，该碰撞带又发生拉开，形成后造山伸展裂谷。结合石炭纪—二叠纪构造岩浆事件，以及构造地质学、沉积学的一些证据研究认为，早石炭世三塘湖盆地及其周缘原型盆地为岛弧环境（弧后盆地）;晚石炭世三塘湖盆地南缘及其相邻区域发育后造山伸展裂谷，大约以三塘湖盆地石头梅潜伏隆起及其以东为界，东部为大黑山裂谷，西部为石头梅裂谷。
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