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新生代以来青藏高原东北部构造运动过程的盆地响应
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摘要
<正>青藏高原东北部构造运动过程的研究是解析高原新生代开始形成及三维空间扩展过程的重要场所。青藏高原东北部是昆仑山构造带、阿尔金构造带及祁连山构造带围限的三角形区域。印度板块向欧亚板块的俯冲及两个板块的陆陆碰撞过程应力向北部传递造成了围限高原东北部的三个构造带构造运动的同时,高原东北部内部(柴达木盆地)也发生了明显的构造变形,主要表现为盆地内部断裂的活跃及沉积环境的明显改变。然而由于新生代年代学的限定,对于高原东北部构造运动过程及高原在
引文
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