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《Acta Geologica Gansu》 1990-00
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THE RESEARCH OF QUATERNARY BASIN OF DUN HUANG INTHE WESTERNCANSU

wang yongtian ( No .908 Hydrogeologic Engineering Geological Team, Ministry of Geology ana Mineral Resourees)  
This paper pursues the tentative approach to the stractigraphical division of Quaternary period, The neotectonic movement and the hydrogeo-logical condition of Dun-Huang basin in the western Gansu . By means of the bore detection and the anaslyis determination, the strata of the flu-violacustrine facies is granted the nomenclature . The sediments of Holo-cene Epoch-pleistocence Epoch are represented respectively by Huang Dun-zi Formation Yii Men guan Formation, Ma Mijuan Formation and Dun Huang Formation. Because the Dun Huang basin is situated at the position of the Complex tectonic zone in the direction of East-west and the western reflex of are of Qilian Shan, Luliang Shan and Helan Shan E type structural system. The neotectonic movement is very violent and is interrupted and remoulded each other . It has been pointed out that the basin has the characteristics of Neotectonic movement namely the in harititance, uplift, new born, boundery and oscillation. Dun Huang basin has the Characteristic of "facies belt" that is situated along the pediment of the typical arid area, The ground water stems mainly from the river water oozing, By means of the outflow of unit drawdown depth, The enriched water division may be pursued, If can ronghly reflect the enreuriiched regulation of ground water .
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