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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2010-01
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Stratigraphic division of Middle-Upper Ordovician and characteristics of the first episode karstification of Middle Caledonian in Akekule uplift,Xinjiang,China

LIU Cun-ge1,2,LI Tao2,LU Hai-tao2,DING Yong21.Basin & Reservoir Research Center,China University of Petroleum,Beijing 102249,China;2.Northwest Oilfield Company of SINOPEC,Urumqi 830011,China  
It is necessary to newly study the stratigraphic division of Middle-Upper Ordovician and the characteristics of the first episode karstification of Middle Caledonian along with the oil and gas exploration in the peripheral regions of the Akekule uplift in Xinjiang.Through comparing and analysing the bore cores,FMI image logging,NGS and conodont fossil,the argillaceous limestone segment under the GR peak of O3q(Upper Ordovician Qiaerbake Formation) belongs to Upper Ordovician,and the thickness of O3q is controlled by the bed form of shoal facies of O2yj(Middle Ordovician Yijianfang Formation).The argillaceous limestone developed in depression areas.FMI and two parameters of NGS,KU and KThU are effective means for this borderline,and this scheme is important for the north of Tarim area.According to this stratigraphic division scheme,the areas to the south of Wells S109-S119-S114 are successive sedimentation for Middle-Upper Ordovician,and those to the north are exposed to the wether.The Yuqi regions in the north are greatly influenced by the first episode karstification of Middle Caledonian.
【Fund】: 国家重点基础研究发展规划“973”项目(2005CB422108)
【CateGory Index】: P618.13
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