地质通报2011，Vol.30Issue(9)：1369-1373,5.
西昆仑山北缘下更新统西域组中上部泥石流沉积的发现及其意义
The discovery of debris flow sediments in the middle-upper Xiyu Formation of Lower Pleistocene on the northern margin of West Kunlun Mountains and its significance
摘要
Abstract
Dozens of layers of debris flow were discovered in Qiaha,Sangzhu and Kekeya areas on the northern margin of West Kunlun Mountains. Density measurements show that they are mainly clayey debris flows. Typical combinations of sedimentary facies are AC,AA1C,DAA,BC,AA1BC,AA1B and A1BC,suggesting that the sedimentary facies of debris flow evolved from top to edge of the alluvial fan,and the age of debris flow sediments is early-middle Early Pleistocene through comparison. The discovery of debris flow sedimentation in middle -upper Xiyu Formation on the northern margin of Tibetan Plateau provides important new information on tectonic background,geomorphic conditions and climate characteristics for analyzing sedimentation age of Xiyu Formation in the north margin of West Kunlun Mountains and also supplies new evidence for the uplift of Tibetan Plateau ant its geological disaster effects , thus putting forward warning for the prevention and treatment of debris flow disaster.关键词
泥石流/西域组/发现/意义/西昆仑山北缘Key words
debris flow/Xiyu Formation/discovery/significance/northern margin of West Kunlun Mountains分类
天文与地球科学引用本文复制引用
黎敦朋,刘健..西昆仑山北缘下更新统西域组中上部泥石流沉积的发现及其意义[J].地质通报,2011,30(9):1369-1373,5.基金项目
中国地质调查局项目《中国气候变化记录对全球气候变化重要事件响应》(编号:1212011120044) （编号:1212011120044）
