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黔西南及南盘江地区三迭纪相变带的逆冲推覆构造研究
引用本文:杜定全. 黔西南及南盘江地区三迭纪相变带的逆冲推覆构造研究[J]. 贵州工业大学学报(自然科学版), 1995, 0(5)
作者姓名:杜定全
作者单位:贵州工学院资源工程系
摘    要:沿黔西南和滇、黔、桂三省区交界的南盘江地区的三迭纪相变带上,发育一系列飞来峰,构造窗等构造,其运动学特征为自台地向盆地方向运动,局部地段有自盆地向台地方向的逆冲作用存在,两者在空间上构成一复杂的被动顶板双重构造模式。逆冲推覆构造由逆冲作用和重力滑动作用所致。

关 键 词:逆冲推覆构造;运动特征;构造模式;黔西南及南盘江地区

A STUDY ON THE THRUST AND NAPPE TECTONICS IN THE FACIES CHANGE BELT OF TRIASSIC PERIOD IN SOUTHWESTERN GUIZHOU AND NANPAN JIANG AREA
Du Dingquan. A STUDY ON THE THRUST AND NAPPE TECTONICS IN THE FACIES CHANGE BELT OF TRIASSIC PERIOD IN SOUTHWESTERN GUIZHOU AND NANPAN JIANG AREA[J]. Journal of Guizhou University of Technology(Natural Science Edition), 1995, 0(5)
Authors:Du Dingquan
Affiliation:Dept.of Resource Engineering
Abstract:There are a series of klippen and windows in the facies change belt of Triassic Period in Southwestern Guizhou and Nanpanjiang area.The kinematical direction of thrust and nappe tectonics is from platform to basin,and there is the kinematical direction from basin to platform in partial area.These blocks of both directional movements form a mold of passive roof duplex which is caused by thrusting and gravity sliding.
Keywords:thrust and nappe tectonics  kinematical characters  structural mold  southwestern Guizhou and Nanpanjiang area
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