Genetic mechanisms and exploration targets of high-quality Permian clastic rock reservoirs in Bohai Bay Basin, East China

Expand
  • 1. National Key Laboratory of Deep Oil and Gas, China University of Petroleum (East China), Qingdao 266580, China;
    2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China;
    3. PetroChina Dagang Oilfield Company, Tianjin 300280, China;
    4. Sinopec Shengli Oilfield Company, Dongying 257001, China

Received date: 2022-06-09

  Revised date: 2023-08-16

  Online published: 2023-08-21

Abstract

Based on core observation, thin section examination, fluid inclusions analysis, carbon and oxygen isotope analysis, and other approaches, the structural and burial evolution histories were investigated, and the diagenetic evolution process and genetic/development models were systematically discussed of the Upper Paleozoic Permian clastic rock reservoirs in the Bohai Bay Basin. The Bohai Bay Basin underwent three stages of burial and two stages of uplifting in the Upper Paleozoic. Consequently, three stages of acidic fluid (oil and gas) leaching, generated by the thermal evolution of kerogen, and two stages of meteoric freshwater leaching occurred. Dissolution in deeply buried, nearly closed diagenetic system was associated with the precipitation of authigenic clay and quartz, leading to a limited increase in storage space. Different structural uplifting-subsidence processes of tectonic zones resulted in varying genetic-reservoir-forming processes of the Permian clastic reservoirs. Three genetic models of reservoirs are recognized. Model I reservoirs with pores formed in shallow strata and buried in shallow to medium strata underwent two phases of exposure to long-term open environment and two phases of meteoric freshwater leaching to enhance pores near the surface, and were shallowly buried in the late stage, exhibiting the dominance of secondary pores and the best physical properties. Model II reservoirs with pores formed in shallow strata and preserved due to modification after deep burial experienced an early exposure-open to late burial-closed environment, where pore types were modified due to dissolution, exhibiting the dominance of numerous secondary solution pores in feldspar and the physical properties inferior to Model I. Model III reservoirs with pores formed after being regulated after multiple periods of burial and dissolution experienced a dissolution of acidic fluids of organic origin under a near-closed to closed environment, exhibiting the dominance of intercrystalline micropores in kaolinite and the poorest physical properties. The target reservoirs lied in the waterflood area in the geological period of meteoric freshwater leaching, and are now the Model II deep reservoirs in the slope zone-depression zone. They are determined as favorable options for subsequent exploration.

Cite this article

CAO Yingchang, SUN Peipei, ZHOU Lihong, YUAN Guanghui, LIU Huimin, LOU Da, WU Zhiping, JIN Qiang, JIANG Youlu . Genetic mechanisms and exploration targets of high-quality Permian clastic rock reservoirs in Bohai Bay Basin, East China[J]. Petroleum Exploration and Development, 0 : 20231012 -20231012 . DOI: 10.11698/PED.20220403

References

[1] 周心怀, 王德英, 于海波, 等. 环渤中地区浅层大规模岩性油藏的成藏主控因素与成藏模式[J]. 石油勘探与开发, 2022, 49(4): 660-669, 740.
ZHOU Xinhuai, WANG Deying, YU Haibo, et al.Major controlling factors and hydrocarbon accumulation models of large-scale lithologic reservoirs in shallow strata around the Bozhong Sag, Bohai Bay Basin, China[J]. Petroleum Exploration and Development, 2022, 49(4): 660-669, 740
[2] 韩文中, 赵贤正, 金凤鸣, 等. 渤海湾盆地沧东凹陷孔二段湖相页岩油甜点评价与勘探实践[J]. 石油勘探与开发, 2021, 48(4): 777-786.
HAN Wenzhong, ZHAO Xianzheng, JIN Fengming, et al.Sweet spots evaluation and exploration of lacustrine shale oil of the second member of Paleogene Kongdian Formation in Cangdong Sag, Bohai Bay Basin[J]. Petroleum Exploration and Development, 2021, 48(4): 777-786.
[3] 赵贤正, 周立宏, 蒲秀刚, 等. 湖相页岩型页岩油勘探开发理论技术与实践: 以渤海湾盆地沧东凹陷古近系孔店组为例[J]. 石油勘探与开发, 2022, 49(3): 616-626.
ZHAO Xianzheng, ZHOU Lihong, PU Xiugang, et al.Theories, technologies and practices of lacustrine shale oil exploration and development: A case study of Paleogene Kongdian Formation in Cangdong Sag, Bohai Bay Basin, China[J]. Petroleum Exploration and Development, 2022, 49(3): 616-626.
[4] 付晓飞, 宋宪强, 王海学, 等. 裂陷盆地断层圈闭含油气有效性综合评价: 以渤海湾盆地歧口凹陷为例[J]. 石油勘探与开发, 2021, 48(4): 677-686.
FU Xiaofei, SONG Xianqiang, WANG Haixue, et al.Comprehensive evaluation on hydrocarbon-bearing availability of fault traps in a rift basin: A case study of the Qikou Sag in the Bohai Bay Basin, China[J]. Petroleum Exploration and Development, 2021, 48(4): 677-686.
[5] 黄士鹏, 龚德瑜, 于聪, 等. 石炭系—二叠系煤成气地球化学特征: 以鄂尔多斯盆地和渤海湾盆地为例[J]. 天然气地球科学, 2014, 25(1): 98-108.
HUANG Shipeng, GONG Deyu, YU Cong, et al.Geochemical characteristics of the gases sourced from the Carboniferous-Permian coal measures: A case study of Ordos and Bohai Bay basins, China[J]. Natural Gas Geoscience, 2014, 25(1): 98-108.
[6] 钱铮, 张松航, 唐书恒, 等. 文安-杨村斜坡石炭-二叠系煤成气成藏模式[J]. 煤炭科学技术, 2016, 44(12): 160-166.
QIAN Zheng, ZHANG Songhang, TANG Shuheng, et al.Accumulation mode of Carboniferous-Permian coal-formed gas in Wen’an-Yangcun Slope[J]. Coal Science and Technology, 2016, 44(12): 160-166.
[7] 张亮. 冀中坳陷北部石炭-二叠系煤成油气成藏作用与主控因素分析[D]. 青岛: 中国石油大学(华东), 2009.
ZHANG Liang.Study on the reservoir-forming process and exploration directions of coal-derived oil and gas from the Permo-Carboniferous in the north of Jizhong Depression[D]. Qingdao: China University of Petroleum (East China), 2009.
[8] 付立新, 楼达, 冯建元, 等. 歧口凹陷中位序、低位序潜山地质特征及油气勘探潜力[J]. 天然气地球科学, 2010, 21(4): 559-565.
FU Lixin, LOU Da, FENG Jianyuan, et al.Geologic features and hydrocarbon exploration potential of middle-and low-buried hill in Qikou Sag[J]. Natural Gas Geoscience, 2010, 21(4): 559-565.
[9] 侯中帅, 陈世悦, 鄢继华, 等. 大港探区上古生界沉积特征与控制因素[J]. 地球科学, 2017, 42(11): 2055-2068.
HOU Zhongshuai, CHEN Shiyue, YAN Jihua, et al.Sedimentary characteristics and control factors of Upper Palaeozoic in Dagang exploration area[J]. Earth Science, 2017, 42(11): 2055-2068.
[10] 侯中帅, 陈世悦, 郭宇鑫, 等. 华北中南部博山地区上古生界沉积相与沉积演化特征[J]. 沉积学报, 2018, 36(4): 731-742.
HOU Zhongshuai, CHEN Shiyue, GUO Yuxin, et al.Sedimentary facies and their evolution characteristics of Upper Paleozoic in Zibo Boshan area, central and southern region of North China[J]. Acta Sedimentologica Sinica, 2018, 36(4): 731-742.
[11] XU J J, JIN Q.Hydrocarbon generation from Carboniferous-Permian coaly source rocks in the Huanghua Depression under different geological processes[J]. Petroleum Science, 2020, 17(6): 1540-1555.
[12] 金强, 宋国奇, 梁宏斌, 等. 渤海湾盆地源于石炭系-二叠系的煤成气成因特征和潜力分析[J]. 地质学报, 2009, 83(6): 861-867.
JIN Qiang, SONG Guoqi, LIANG Hongbin, et al.Characteristics of Carboniferous-Permian coal-derived gas in the Bohai Bay Basin and their implication to exploration potential[J]. Acta Geologica Sinica, 2009, 83(6): 861-867.
[13] 赵贤正, 李宏军, 付立新, 等. 渤海湾盆地黄骅坳陷古生界煤成凝析气藏特征、主控因素与发育模式[J]. 石油学报, 2021, 42(12): 1592-1604.
ZHAO Xianzheng, LI Hongjun, FU Lixin, et al.Characteristics, main controlling factors and development mode of Paleozoic coal-formed condensate gas reservoirs in Huanghua Depression, Bohai Bay Basin[J]. Acta Petrolei Sinica, 2021, 42(12): 1592-1604.
[14] FOLK R L, ANDREWS P B, LEWIS D W.Detrital sedimentary rock classification and nomenclature for use in New Zealand[J]. New Zealand Journal of Geology and Geophysics, 1970, 13(4): 937-968.
[15] FRANÇA A B, ARAÚJO L M, MAYNARD J B, et al. Secondary porosity formed by deep meteoric leaching: Botucatu eolianite, southern South America[J]. AAPG Bulletin, 2003, 87(7): 1073-1082.
[16] YUAN G H, CAO Y C, SCHULZ H M, et al.A review of feldspar alteration and its geological significance in sedimentary basins: From shallow aquifers to deep hydrocarbon reservoirs[J]. Earth-Science Reviews, 2019, 191: 114-140.
[17] 邱隆伟, 侯立新, 汪丽芳. 埕110块碎屑岩储层物性表生作用分带性研究[J]. 油气地质与采收率, 2005, 12(5): 16-20.
QIU Longwei, HOU Lixin, WANG Lifang.A study on the zoning of hypergenesis of physical properties of clastic reservoir in Cheng 110 Block[J]. Petroleum Geology and Recovery Efficiency, 2005, 12(5): 16-20.
[18] BJØRLYKKE K, JAHREN J. Open or closed geochemical systems during diagenesis in sedimentary basins: Constraints on mass transfer during diagenesis and the prediction of porosity in sandstone and carbonate reservoirs[J]. AAPG Bulletin, 2012, 96(12): 2193-2214.
[19] GILES M R, MARSHALL J D.Constraints on the development of secondary porosity in the subsurface: Re-evaluation of processes[J]. Marine and Petroleum Geology, 1986, 3(3): 243-255.
[20] YUAN G H, CAO Y C, GLUYAS J, et al.Feldspar dissolution, authigenic clays, and quartz cements in open and closed sandstone geochemical systems during diagenesis: Typical examples from two sags in Bohai Bay Basin, East China[J]. AAPG Bulletin, 2015, 99(11): 2121-2154.
[21] GILES M R.Mass transfer and problems of secondary porosity creation in deeply buried hydrocarbon reservoirs[J]. Marine and Petroleum Geology, 1987, 4(3): 188-204.
[22] SHEPPARD S M F, GILG H A. Stable isotope geochemistry of clay minerals[J]. Clay Minerals, 1996, 31(1): 1-24.
[23] SURDAM R C, CROSSEY L J.Integrated diagenetic modeling: A process-oriented approach for clastic systems[J]. Annual Review of Earth and Planetary Sciences, 1987, 15(1): 141-170.
[24] SCHMIDT V, MCDONALD D A.The role of secondary porosity in the course of sandstone diagenesis[M]//SCHOLLE P A, SCHLUGER P R. Aspects of Diagenesis. Tulsa: SEPM Society for Sedimentary Geology, 1979: 175-207.
[25] KAWAMURA K, KAPLAN I R.Dicarboxylic acids generated by thermal alteration of kerogen and humic acids[J]. Geochimica et Cosmochimica Acta, 1987, 51: 3201-3207.
[26] BARTH T, BJØRLYKKE K. Organic acids from source rock maturation: generation potentials, transport mechanisms and relevance for mineral diagenesis[J]. Applied Geochemistry, 1993, 8(4): 325-337.
[27] 郭宏莉, 王大锐. 塔里木油气区砂岩储集层碳酸盐胶结物的同位素组成与成因分析[J]. 石油勘探与开发, 1999, 26(3): 31-32.
GUO Hongli, WANG Darui.Stable isotopic composition and origin analysis of the carbonate cements within sandstone reservoirs of Tarim oilgas bearing area[J]. Petroleum Exploration and Development, 1999, 26(3): 31-32.
[28] GÖTTE T, RAMSEYER K, PETTKE T, et al. Implications of trace element composition of syntaxial quartz cements for the geochemical conditions during quartz precipitation in sandstones[J]. Sedimentology, 2013, 60(5): 1111-1127.
[29] EMERY D, MYERS K J, YOUNG R.Ancient subaerial exposure and freshwater leaching in sandstones[J]. Geology, 1990, 18(12): 1178-1181.
[30] LAWRENCE M G, GREIG A, COLLERSON K D, et al.Rare earth element and yttrium variability in south east Queensland waterways[J]. Aquatic Geochemistry, 2006, 12(1): 39-72.
[31] 操应长, 远光辉, 王艳忠, 等. 典型含油气盆地深层富长石碎屑岩储层长石溶蚀接力成孔认识及其油气地质意义[J]. 中国科学: 地球科学, 2022, 52(9): 1694-1725.
CAO Yingchang, YUAN Guanghui, WANG Yanzhong, et al.Successive formation of secondary pores via feldspar dissolution in deeply buried feldspar-rich clastic reservoirs in typical petroliferous basins and its petroleum geological significance[J]. SCIENCE CHINA Earth Sciences, 2022, 65(9): 1673-1703.
[32] YUAN G H, CAO Y C, SUN P P, et al.Genetic mechanisms of Permian Upper Shihezi sandstone reservoirs with multi-stage subsidence and uplift in the Huanghua Depression, Bohai Bay Basin, East China[J]. Marine and Petroleum Geology, 2021, 124: 104784.
[33] MASTALERZ M, DROBNIAK A, STANKIEWICZ A B.Origin, properties, and implications of solid bitumen in source-rock reservoirs: A review[J]. International Journal of Coal Geology, 2018, 195: 14-36.
Options
Outlines

/