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《Journal of Jilin University(Earth Science Edition)》 2007-S1
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The Originatio Study of Mid-Holocene Sand Bed in Zhangbei,Northern Hebei Province

WANG Xing-jun1,LIN Xiao-feng2,WANG De-qiang1,ZHUAN Shao-peng1,BAN Chang-yong1,LIU Yu-jun1 1.Hebei Institute of Geology Survery,Langfang,Hebei 065000,China 2.Hebei University of Technology,Langfang,Hebei 065000,China  
There is a special sand bed in Zhangbei county,northern Hebei province.It's attented by many geology workers,because there are many microlithic tools in it.But there are different cognition on its genesis.The paper studied the character of the special sand bed form stratigraphy and chronology and paleontology and sand surface structure and sand combination and sand bed shade and attitude of rocks.Deposit lay on the second terrace and facing the sun and low and short and flat mountain slope,and draws near waterhead,disperses by east-west direction.Deposit is a suit of gray brown fine sand.It does not show bedding,and there are many remains of ancient man,such as microlithic tools,crockery pieces,ash bed.It is bad that the sorting and roundness.The result of grain size distribution and Scanning electron microscope analysising shows that the Mid-Holocence sand bed's sand primitive formatting environment is the water environment of medium river,moreover has been reformed in evening again.The sands contains rich mammal fossil and rich sporopollen which is fond of wet and warm environment.The measuring year result expresses that sand bed formed in Mid-Holocence,which is the climate optimum time of Holocence.A lot of evidences show that Mid-Holocence sand bed in northern Hebei province formed in the river environment,moreover has been reformed by ancient man in evening again,is remains of ancient man activity,belong to manual deposit,is site of ancient villages.
【Fund】: 国土资源部区域地质调查项目(冀勘地1998[70])
【CateGory Index】: P534.632
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