节点文献

翠华山水湫池及其附近崩塌堆积形成年代探疑

A study on the Formation Age of Shuiqiuchi Pool And the Colluvial Deposits Around the Pool in Cuihuashan Mountain

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 苏惠敏贺明静

【Author】 Su Huimin, He Mingjing (College of Tourism and Environmental Science, Shaanxi Normal University, Xi’an, 710062 )

【机构】 陕西师范大学旅游与环境学院陕西师范大学旅游与环境学院 陕西西安710062陕西西安710062

【摘要】 通过对相关史料的分析,论证了翠华山主景区崩塌堆积不可能是唐天宝年间地震诱发山崩形成的。通过实地考察,认为这些崩塌堆积不是同时发生,而是多期崩塌活动的结果,并且崩塌活动又都发生在水湫池被堰塞成湖之后。因此,水湫池不可能是唐代的地震山崩形成的。

【Abstract】 The paper based on analyzing historical materials demonstrated that it is impossible that the colluvial deposits in the central scenic area of Cuihuashan Mountain were formed by the landslide, which were induced by the earthquake happened in TianBao period of Tang Dynasty. Through fieldwork research, we considered that the colluvial deposits were not formed at the same time, but the result of multi-period landslide activities. The dammed lake, Shuiqiuchi pool, had been formed when the landslide activities happened. Therefore, the Shuiqiuchi pool can not be formed by the landslide induced by the earthquake happened in the Tang dynasty.

【关键词】 山崩崩积物泥石流堰塞湖
【Key words】 landslidecolluvial depositsdebris flowdammed lake
  • 【文献出处】 中国历史地理论丛 ,Collections of Essays on Chinese Historical Geography , 编辑部邮箱 ,2005年04期
  • 【分类号】K928.6
  • 【被引频次】7
  • 【下载频次】174
节点文献中: 

本文链接的文献网络图示:

本文的引文网络