论文部分内容阅读
陕西翠华山山崩主要由水湫池 (天池 )山崩体、甘湫池山崩体及大坪山崩体三部分组成。其中水湫池 (天池 )山崩体开发及研究较为成熟 ,是吸引游客的黄金地段。翠华山山崩的形成主要由内力因素及外力因素所控制 ,其中内力因素包括翠华山花岗岩体背景因素和节理面理、断裂面理及变质地层面理等因素 ,外力因素包括陕西关中地震及暴雨等因素。翠华山山崩首次发现由三期山崩体组成 ,不同期次山崩有各自特色旅游环境 ,反映了出山崩自然现象亦有造福人类的积极方面
Shaanxi Cuihuashan landslide mainly consists of three parts: Minamata pool (Tianchi) landslide body, Ganchongchi landslide body and Daping landslide body. Among them, Mizobe Pool (Tianchi) landslide body has been developed and studied more maturely, which is a golden area to attract tourists. The formation of Cuihuashan landslide is mainly controlled by the internal and external factors, including the background factors of Cuihuashan granite body, such as the joints, fractures and metamorphic strata. External factors include the Guanzhong earthquake and heavy rainfall in Shaanxi Province factor. Cuihuashan landslide was first discovered by three landslides, different periods of landslides have their own characteristics of the tourism environment, reflecting the natural phenomenon of landslides also have a positive aspect of the benefit of mankind