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《Geological Science and Technology Information》 2017-01
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Paleogeomorphology and Karst Reservoir Development of Ordovician Carbonate in Halahatang Area,Northern Tarim Basin

Zhang Qingyu;Qin Fengrui;Liang Bin;Dan Yong;Li Jingrui;Chen Lixin;School of Environmental Studies,China University of Geosciences(Wuhan);Institute of Karst Geology,Chinese Academy of Geological Sciences/Karst Dynamics Laboratory,MLR & GZAR;CAGS;Reservoir Institute of Exploration and Development,Tarim Oilfield Company,PetroChina;  
In order to research the Ordovician carbonate paleogeomorphology and the development of the karst reservoir,this study is conducted based on the seismic,drilling,core and the thin section analysis,and also uses"the residual thickness and the formation of ancient structure trend surface"method to restore the ancient landscape and ancient water system.The paper has divided the study area into three kinds of secondary geomorphic types and 6kinds of triple geomorphic types and number of micro morphology.Based on the carbon and oxygen isotope characteristics of ancient karst seam hole filling calcite,and the carbonate chemical characteristics and reservoir properties,the study analyzes the ancient karst development and filling period of time.The results show that the later dissolution pore,cave and karst fissures are the main reservoir space.The value of δ~(13)C and δ~(18)O is large,withδ13C ranging from-4.17‰to 1.59‰,averaged at-1.05 ‰,and δ~(18)O ranging from-15.71‰to-5.17‰,averaged at-11.15‰.Then,four different stages of ancient karstification are divided:marine sedimentary environment,atmospheric fresh water environment,shallow buried and buried depth of high temperature environment.
【Fund】: 国家自然科学基金项目(41302122);; 国家重点基础研究973计划项目(2011CB201001);; 国土资源部公益性行业科研专项(201211082)
【CateGory Index】: P618.13;P534.42
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