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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2006-01
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An intensive erosion event in the last glaciation in the west of China

WANG Yun-sheng,HUANG Run-qiu,DUAN Hai-peng,WEI MengGeological Hazards and Environment Protection National Speciality Lab.,Chengdu University of Technology,Chengdu 610059,China  
In the recent years,more and more exploration data show that deep overburdens are well developed in the west of China.According to the composition,three layers can be divided upward: alluvial and glacial fluvial boulders and pebbles gravel layer in the lower part;multi-genetic block(boulder) pebble(granule) layer in the middle part,generally intercalated with silt-fine sand bed and sand lens;alluvial pebbles gravel layer in the upper part.Dating shows that the age of the lower part is about 20~25 ka,and that of the middle part is 16~19 ka.They are older than that of the second terrace along the river.These imply that the rock surface of the valley bottom was formed 25 ka ago by an intensive erosion event.This event is related with the second interglacial era of Würm.
【Fund】: 国家自然科学基金资助项目(40472143/D021490102002/D0214)
【CateGory Index】: P534.63
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