Xu Zeng, Jinying Dong, P. Zhao, Wei Liu, C. Bian, Chunlin Zhang
{"title":"鄂尔多斯盆地陇东地区三叠纪延长组长7-3亚段陆相页岩油藏岩相分类及测井识别","authors":"Xu Zeng, Jinying Dong, P. Zhao, Wei Liu, C. Bian, Chunlin Zhang","doi":"10.1190/int-2022-0070.1","DOIUrl":null,"url":null,"abstract":"The division and identification of lithology and lithofacies are very important in exploration and development of oil and gas reservoirs. Information on lithofacies determines the development modes and provides the favorable \"sweet spot\" intervals of shales. The Chang 7-3 sub-member of the Triassic Yanchang Formation in the Longdong area of the Ordos Basin is an important shale formation in China. Core photos, cast thin sections, and log response characteristics were used to clarify the development and distribution characteristics of the various lithofacies in this formation. The lithofacies of target intervals are classified into fine grained sandy debrite, silty to fine grained sandy turbidite, fine grained sandy slump, semi-deep to deep lacustrine mudstone, and deep lacustrine shale. Further, the conventional and micro-resistivity imaging log response characteristics of different lithofacies are analyzed. Compared with other lithofacies, deep lacustrine shale facies are characterized by high gamma ray (GR), high compensated neutron log (CNL), high acoustic log (AC), and low density (DEN) log values. Crossplots of GR-AC, DEN-CNL, and DEN-AC are proposed to identify most of the lithofacies, and a criterion was established for use of well logs to characterize the lithofacies. Finally, a method joining conventional logs and micro-resistivity imaging log data was applied to field wells, achieving the very high accuracy rate of 88%. The distribution maps of different lithofacies thickness in the study area are obtained. Deep lacustrine shale faces have the widest development area and many thickness centers. Accurate and effective identification of lithofacies shows that within Ordos Basin, there is an area of about 20,000 km2 with shale thickness greater than 6 m, providing an important basis for shale oil exploration in the study area.Keywords: Continental shale oil; Lithofacies; Lacustrine shale; Micro-resistivity imaging","PeriodicalId":51318,"journal":{"name":"Interpretation-A Journal of Subsurface Characterization","volume":" ","pages":""},"PeriodicalIF":1.1000,"publicationDate":"2022-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Classification and well log identification of lithofacies of continental shale oil reservoirs in Chang 7-3 sub-member of Triassic Yanchang Formation in Longdong area of Ordos Basin, China\",\"authors\":\"Xu Zeng, Jinying Dong, P. Zhao, Wei Liu, C. Bian, Chunlin Zhang\",\"doi\":\"10.1190/int-2022-0070.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The division and identification of lithology and lithofacies are very important in exploration and development of oil and gas reservoirs. Information on lithofacies determines the development modes and provides the favorable \\\"sweet spot\\\" intervals of shales. The Chang 7-3 sub-member of the Triassic Yanchang Formation in the Longdong area of the Ordos Basin is an important shale formation in China. Core photos, cast thin sections, and log response characteristics were used to clarify the development and distribution characteristics of the various lithofacies in this formation. The lithofacies of target intervals are classified into fine grained sandy debrite, silty to fine grained sandy turbidite, fine grained sandy slump, semi-deep to deep lacustrine mudstone, and deep lacustrine shale. Further, the conventional and micro-resistivity imaging log response characteristics of different lithofacies are analyzed. Compared with other lithofacies, deep lacustrine shale facies are characterized by high gamma ray (GR), high compensated neutron log (CNL), high acoustic log (AC), and low density (DEN) log values. Crossplots of GR-AC, DEN-CNL, and DEN-AC are proposed to identify most of the lithofacies, and a criterion was established for use of well logs to characterize the lithofacies. Finally, a method joining conventional logs and micro-resistivity imaging log data was applied to field wells, achieving the very high accuracy rate of 88%. The distribution maps of different lithofacies thickness in the study area are obtained. Deep lacustrine shale faces have the widest development area and many thickness centers. 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Classification and well log identification of lithofacies of continental shale oil reservoirs in Chang 7-3 sub-member of Triassic Yanchang Formation in Longdong area of Ordos Basin, China
The division and identification of lithology and lithofacies are very important in exploration and development of oil and gas reservoirs. Information on lithofacies determines the development modes and provides the favorable "sweet spot" intervals of shales. The Chang 7-3 sub-member of the Triassic Yanchang Formation in the Longdong area of the Ordos Basin is an important shale formation in China. Core photos, cast thin sections, and log response characteristics were used to clarify the development and distribution characteristics of the various lithofacies in this formation. The lithofacies of target intervals are classified into fine grained sandy debrite, silty to fine grained sandy turbidite, fine grained sandy slump, semi-deep to deep lacustrine mudstone, and deep lacustrine shale. Further, the conventional and micro-resistivity imaging log response characteristics of different lithofacies are analyzed. Compared with other lithofacies, deep lacustrine shale facies are characterized by high gamma ray (GR), high compensated neutron log (CNL), high acoustic log (AC), and low density (DEN) log values. Crossplots of GR-AC, DEN-CNL, and DEN-AC are proposed to identify most of the lithofacies, and a criterion was established for use of well logs to characterize the lithofacies. Finally, a method joining conventional logs and micro-resistivity imaging log data was applied to field wells, achieving the very high accuracy rate of 88%. The distribution maps of different lithofacies thickness in the study area are obtained. Deep lacustrine shale faces have the widest development area and many thickness centers. Accurate and effective identification of lithofacies shows that within Ordos Basin, there is an area of about 20,000 km2 with shale thickness greater than 6 m, providing an important basis for shale oil exploration in the study area.Keywords: Continental shale oil; Lithofacies; Lacustrine shale; Micro-resistivity imaging
期刊介绍:
***Jointly published by the American Association of Petroleum Geologists (AAPG) and the Society of Exploration Geophysicists (SEG)***
Interpretation is a new, peer-reviewed journal for advancing the practice of subsurface interpretation.