{ "labelLang" : "hun", "responseDate" : "2024-03-29 07:53", "content" : { "otype" : "JournalArticle", "mtid" : 31432823, "status" : "VALIDATED", "published" : true, "comment" : "State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249, China \n College of Geosciences, China University of Petroleum (Beijing), Beijing, 102249, China \n Research Institute of Petroleum Exploration and Development, Liaohe Oilfield Company, PetroChina, Panjin, Liaoning 124010, China \n Department of Petroleum Engineering, University of North Dakota, Grand Forks, ND 58202, United States \n Cited By :3 \n Export Date: 12 February 2021 \n Correspondence Address: Zeng, L.; China University of Petroleum (Beijing), 18 Fuxue Road, Changping, China; email: lbzeng@sina.com \n Funding text 1: The authors greatly acknowledge the PetroChina Liaohe Oilfield Company for their help in providing information and other support. The authors would also like to thank the works made by Professor Peng Shimi in China University of Petroleum-Beijing, and Ms. He Shuting in PetroChina Liaohe Oilfield exploration and development research institute, which has enabled our work to proceed smoothly. We are particularly grateful to JMPG Associate Editor Dr. Nicolas Beaudoin and two anonymous reviewers for their constructive comments, which contributed significantly to the improvement of the manuscript.\nState Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249, China \n College of Geosciences, China University of Petroleum (Beijing), Beijing, 102249, China \n Research Institute of Petroleum Exploration and Development, Liaohe Oilfield Company, PetroChina, Panjin, Liaoning 124010, China \n Department of Petroleum Engineering, University of North Dakota, Grand Forks, ND 58202, United States \n Cited By :5 \n Export Date: 12 September 2021 \n Correspondence Address: Zeng, L.; China University of Petroleum (Beijing), 18 Fuxue Road, Changping, China; email: lbzeng@sina.com \n Funding text 1: The authors greatly acknowledge the PetroChina Liaohe Oilfield Company for their help in providing information and other support. The authors would also like to thank the works made by Professor Peng Shimi in China University of Petroleum-Beijing, and Ms. He Shuting in PetroChina Liaohe Oilfield exploration and development research institute, which has enabled our work to proceed smoothly. 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Based on the analyses of outcrops, cores, thin sections, imaging logs, and laboratory measurements, tectonic fractures are the dominant type of natural fractures, and their development is mainly influenced by petrology and faulting. Tectonic fractures are more developed in metamorphic rocks with a higher content of brittle minerals, while fracture orientations are primarily parallel or almost parallel to the fault strikes. Opening-mode fractures, which account for more than 65% of the total reservoir porosity, provide the primary storage space for metamorphic basement reservoirs. Besides, opening-mode fractures serve as the major pathways for fluid flow throughout the reservoirs and ultimately determine the quality of these reservoirs. Therefore, the discrepancies in fracture development are speculated to be the primary reason leading to the vertical stratification of reservoirs. According to the degree of fracture development, various rock types in metamorphic basement reservoirs can be arranged in order as leptite, granulite, migmatitic granite, gneiss, lamprophyre, diabase, and amphibolite. In this sequence, the former rocks are more likely to become effective reservoirs, while the latter ones are usually inner interlayers. However, the lithology boundary of reservoir rocks and inner interlayers is not definite in this sequence. In a specific metamorphic basement reservoir, the rocks that can become reservoirs have a lower limit in the sequence. 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