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《Journal of Jilin University(Earth Science Edition)》 2012-S1
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Reservoir Types and Distribution of Nantun Formation in Ta'nan Depression

Fang Shi1,2,Xie Rong-xiang1,Miao Chang-sheng3,Liu Zhao-jun1,2, Meng Qi-an4,Zhang Ge4,Qu Yong-hong4,Zhang Jun-long4 1.College of Earth Sciences,Jilin University.Changchun 130061,China 2.Oil Shale Laboratory Center,Jilin University,Changchun 130061,China 3.Northeast Oil and Gas Branch,SINOPEC,Changchun 130062,China 4.Research Institute of Exploration and Development,Daqing Oilfield Limited Company,Daqing 163712,Heilongjiang,China  
The present dustpan faulted depression of Ta'nan sag is created by segmenting and reforming the large faulted basin by the many warping and tilting blocks,and the basin is consisted of gentle slop,sedimentary center and steep slop sedimentation.Through the comprehensive analysis of structure,sedimention,inversion and oil testing information,the authors find that the reservoir types and exhibition are controlled by deposition process,synsedimentary and postsedimentary structures,which are completely different from the common continental dustpan faulted depression.On the position of warping and tilting blocks of the gentle slop,there are mainly sand bodies of delta front and develop structural-lithologic reservoirs which are segmented or sheltered by faults.Sandbodies in sedimentary center are mainly formed in far-side fan and delta front,also,lenticular-shape lithologic reservoirs and structural-lithologic reservoirs are always found there.In the oblique part of depositional centers and subsiding centers,there are mainly far-side fan sandbodies and develop lithologic reservoirs and anticline-lithologic reservoirs.On the abrupt slope there are mainly sandbodies of nearshore subaqueous fan and develop mainly lenticular-shape lithologic reservoirs,sometimes updip wedge out lithologic reservoirs and structural-lithologic reservoirs.
【Fund】: 国家自然科学基金项目(40902057 40702027);; 吉林大学创新团队建设项目(201004001);吉林大学基本科研业务费平台基地建设项目;; 国家地震局地质研究所开放实验室基金(LED0609)
【CateGory Index】: P618.13
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