|
|||||
|
|
| 武当山推覆构造的几何结构──鳞片叠覆模式 | |
| 引用本文： | 石绍清,蔡学林,吴德超,邓明森. 武当山推覆构造的几何结构──鳞片叠覆模式[J]. 成都理工大学学报(自然科学版), 1995, 0(4) |
| 作者姓名： | 石绍清 蔡学林 吴德超 邓明森 |
| 作者单位： | 成都理工学院地质学系 |
| 摘 要： | 武当山推覆构造由主滑脱面、前缘叠瓦褶断带、中央推覆体带和后缘挤压－伸展带４种构造成分组成。中央推覆体带划分为７个推覆体。各推覆体在平面上呈鳞片状越覆，在剖面上呈送冲叠覆，构成鳞片叠覆的几何模式。 |
| 关 键 词： | 武当山，推覆构造，推覆体，越覆，鳞片叠覆模式 |
GEOMETRIC STRUCTURE OF THE NAPPE TECTONIC OF WUDANG MOUNTAIN: A SCALY IMBRICATION MODEL |
|
| Shi Shaoqing, Cai Xuelin, Wu Dechao, Deng Mingsen. GEOMETRIC STRUCTURE OF THE NAPPE TECTONIC OF WUDANG MOUNTAIN: A SCALY IMBRICATION MODEL[J]. Journal of Chengdu University of Technology: Sci & Technol Ed, 1995, 0(4) | |
| Authors: | Shi Shaoqing Cai Xuelin Wu Dechao Deng Mingsen |
| Affiliation: | Shi Shaoqing; Cai Xuelin; Wu Dechao; Deng Mingsen |
| Abstract: | The nappe tectonic of Wudang Mountain consiSts of the main slip plane,the imbricate foldfault zone tri the leading edge,the central nappe zone,and the co m pressional- extensional zone in the posterior border. The central nappe zone is divided into seven nappes, which have an appearance of horizontal scaly imbrication and vertical thruSt overlap,and thus form a seometric model of scaly imbrication. |
| Keywords: | Wudang Mountain nappe tectonic nappe overlap scaly imbrication model |
| 本文献已被 CNKI 等数据库收录！ | |