摘要
文章依据区调工作成果,把龙门山南段金台山飞来峰划分为上中下三层。并认为金台山飞来峰是一个“多层楼式”的几何结构样式。是龙门山南段逆冲推覆构造发展过程中形成的,其形成机制是重力滑动和后推挤压的综合作用。
Based on the results of geological surveys, this paper considered that in southern segment of the Longmen Mountains, the Jintaishan Klippe can be devided into upper, middle and lower parts and it possesses a 'multi-floored' textural style. It was formed during the developing process of thrust nappe tectonics in southern segment of the Longmen Mountains. The formational mechanism is the combination of gravitation and back compression.
关键词
金台山
龙门山
飞来峰
结构样式
southern segment of Longmen Mountains, Jintaishan Klippe, 'multi-floored' textural style, gravitational slip