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《Journal of Stratigraphy》 2004-01
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PERMIAN PALYNOSTRATIGRAPHY OF THE AKE 1 BOREHOLE,TARIM BASIN AND ITS GEOLOGICAL SIGNIFICANCE

HUANG Zhi bin 1),2) , DU Pin de 1) , TAN Ze jin 1) , GAO Qin qin 1) , LI Meng 1)2) , and ZHAN Jia zhen 3) ( 1) Institute of Exploration and Development of Tarim Oilfield Division Company,CNPC,Korla,841000; 2) University of Petroleum, Beijing,100249; 3) Institute of Exploration and Development of Xinjiang Oilfield Division Company,CNPC,Kelamayi,834000)  
The Ake 1 borehole, located the north of Southwest Depression of the Tarim Basin, Xinjiang, is a wildcat well. The Middle Permian Biyoulieti Group (P 1 by ) is 255.50m(3 954~4 209.50m) in drilled thickness and consists of gray brown, gray and dark gray mudstone, silty mudstone and calcareous mudstone with light gray marl and gray shaly siltstone and siltstone. There are much sporopollen in the Biyoulieti Group. One sporopollen assemblage, Florinites Protohaploxypinus Vittatina Assemblage,has been proposed. It indicates a Middle Permian age for the Biyoulietic Group. The drilled Biyoulieti Group of the Ake 1 Borehole is of great geological significance. It not only improves and perfectes the stratigraphic sequence of this area,but also enriches the Permian sporopollen data, filles in the gap in the Permian palaeopalynologic studies,changes the appraisal of the capacity for oil producing, and upgrades the oil and gas prospect evaluation.
【Fund】: 中国石油天然气股份有限公司《中国北方石炭—二叠系划分对比、古环境研究及含油气远景评价》项目
【CateGory Index】: P534
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