[an error occurred while processing this directive] ������� 2013, 32(2) 305-316 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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Tectonic evolution and oil-gas reservoir forming period of Changling fault depression
MA Chang-Chun-1, WANG Jian-Qiang-2, 3, SUN Jing-2, 3, ZHANG Jian-Wei-4
1. College of Earth Sciences��Jilin University��Changchun 130061��China; 2. Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology��Ministry of Land and Resources�� Qingdao 266071��Shandong��China; 3. Qingdao Institute of Marine Geology��Qingdao 266071��Shandong��China; 4. Geo-engineering Investigation Institute of Qingdao��Qingdao 266071��Shandong��China
Abstract:

Changling fault depression went through three stages in evolution��including the faulted period�� depression period and inversion period�� The fault rised and the formation generated erosion were in the late Yingcheng formation��late Nenjiang formation and late Mingshui formation�� Based on seismic and drilling data of the 4 wells located in the studied area by sonic velocity analysis and stratigraphic trend extension method��we get the result that the average erosion volume of the three periods mentioned above were 417. 5 m��205 m and 342. 5 m respectively�� Based on the stratigraphic denudation quantity calculation and the comprehensive study on homogenization temperature fluid inclusion in reservoir��we research on the oil-gas reservoir forming time and the period of each tectonic unit in Changling fault depression�� The Yingcheng Formation and Denglouku Formation of Shuangtuozi structure have gas accumulation for two phases�� The Yingcheng Formation and Denglouku Formation of Haerjin structure have gas accumulation for one phase�� The Quantou Formation of Fulongquan structure has gas accumulation for one phase��

Keywords: Changling fault depression   tectonic evolution history   homogenization temperation of fluid incusion   formation time and period  
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1�� ���, ��ռ��, ����ǿ.������س���������������������ؼ��ֲ�[J]. �������, 2010,29(4): 622-627
2�� ������.����������ڶ�ѷ�����ϲ������ɲ��ڴ��о�[J]. �������, 2012,31(4): 748-752
3�� ����1, �����1, ������2, ������2, ������1, 2, ����1, 2.������س������Ӫ�����ɽ�ҵ�ʱ������ʯ����[J]. �������, 2013,32(3): 522-530

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