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《ACTA SCICENTIARUM NATURALUM UNIVERSITIS PEKINESIS》 1995-03
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Late Quaternary Movement on the Heihekou Fault, West Gansu,China

LI Youli Li Baojun YANG Jingchun (Deparrment of Geography,Peking University,Beijing , 100871)  
The Heihekou fault ,being apart 30 km from Zhangye in the southwest ,is a reversed fault which trends to the northwest and dips to the southwest. It is found that the fault on a natural section along the bank of the Heihe River dips steeply to the southwest. and that the Ordovician system thrusts to the northeast on the Late Pleistocene alluviam with a throw of 17 m.A fault scarp was formed in the faultmovement on terraces of the Heihe River.The terrace with an estimated age of 5ka B. P. is vertically dislocated by 2 m,age of 10 ka B. P by 4 m,and age of 13 kaB. P. by 9 m.These dislocations and the sediments near the faul indicate there hadbeen 3 movement enents at least.The vertical dislocation is 2~5 m each,the aver-age recurrence interval is 3~5ka ,and the average slip rate is 1. 67~0. 4mm/a.
【Fund】: 国家教委博士点基金
【CateGory Index】: P542.3
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