摘要
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 。
Shaanxi Cuihuashan landslides mainly consist of Shuiqiuchi (Tianchi) landslide,Ganqiuchi landslide and Daping landslide.Shuiqiuchi(tianchi) landslide explored and studied more mature is a golden section to attract sightseers.Its accumulation is because of facts of the geologic setting of Cuihuashan granite body,joints,faults and metamorphic beddings,along with ancient Shaaxi earthquake and rainstorm.Cuihuashan landslides could be divided into three periods orderly.Every periodic landslids has its own distinct tour landform environment.It reflects landslides have positive sides for people.
出处
《山地学报》
CSCD
2001年第4期355-358,共4页
Mountain Research
基金
国家自然科学基金项目资助 (批准号 :49972 0 66)
