鄂尔多斯盆地西缘奥陶系克里摩里组白云岩成因

doi:10.7623/syxb202508006

石油学报 ›› 2025, Vol. 46 ›› Issue (8): 1517-1535,1627.DOI: 10.7623/syxb202508006

鄂尔多斯盆地西缘奥陶系克里摩里组白云岩成因

白莹, 高建荣, 赵振宇

中国石油勘探开发研究院北京 100083

收稿日期:2024-09-04 修回日期:2025-01-06 发布日期:2025-09-06
通讯作者: 白莹,女,1990年2月生,2017年获北京大学博士学位,现为中国石油勘探开发研究院高级工程师,主要从事沉积储层与地质勘探研究工作。Email:byshimmer@petrochina.com.cn
作者简介:白莹,女,1990年2月生,2017年获北京大学博士学位,现为中国石油勘探开发研究院高级工程师,主要从事沉积储层与地质勘探研究工作。
基金资助:
中国石油长庆油田公司科学研究与技术开发项目(2023-KTSY-DO32)资助。

Dolomite genesis of Ordovician Kelimoli Formation in western Ordos Basin

Bai Ying, Gao Jianrong, Zhao Zhenyu

PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China

Received:2024-09-04 Revised:2025-01-06 Published:2025-09-06

摘要/Abstract

摘要： 以鄂尔多斯盆地西缘典型钻井中奥陶系克里摩里组白云岩储层为研究对象,通过岩心观察和岩石薄片鉴定,结合多种地球化学分析成果(同位素、主量/微量元素、流体包裹体测温及U-Pb同位素定年等),明确了白云岩的岩石学特征,揭示了白云岩成因,建立了白云石化模式。研究结果表明:①根据宏观分布特征和微观晶体形态,克里摩里组白云岩可分为粉晶—细晶白云岩、纹层白云岩、残余结构细晶白云岩、细晶—中晶白云岩A、细晶—中晶白云岩B和中晶—粗晶斑状白云岩。②在鄂尔多斯盆地西缘东部局限台地,克里摩里组的纹层白云岩受准同生期微生物白云石化作用影响,其白云石化流体为近地表海水;而粉晶—细晶白云岩形成于准同生期蒸发泵吸白云石化作用,其白云石化流体为低盐度蒸发海水。在盆地西缘中部台缘带,克里摩里组白云岩形成于准同生期的回流渗透作用并叠加了浅层—中层埋藏期孔隙水白云石化作用,对应发育残余结构细晶白云岩、自形—半自形细晶—中晶白云岩A和他形细晶—中晶白云岩B,其中,部分发育在台缘带东侧风化壳附近的细晶—中晶白云岩B在成岩过程中有大气淡水加入。盆地西缘中部台缘带还发育与断裂相关的中晶—粗晶斑状白云岩,该类白云岩形成于早期有海源卤水参与的中层—深层埋藏期热液白云石化作用。③准同生期蒸发泵吸白云石化作用与回流渗透白云石化作用是克里摩里组的主要白云石化模式,浅层—中层埋藏期孔隙水白云石化作用、中层—深层埋藏期热液白云石化作用以及早期微生物白云石化作用为次要白云石化模式。

关键词: 鄂尔多斯盆地西缘, 奥陶系, 克里摩里组, 白云石化作用, 储层

Abstract: This paper focuses on dolomite reservoirs of Ordovician Kelimoli Formation in western Ordos Basin. Through core observation and microscopic identification, combined with comprehensive geochemical analytical methods including isotopes, major and trace elements, fluid inclusion thermometry, and U-Pb isotopic dating, the paper clarifies the petrological characteristics of dolomites, reveals the genesis of dolomites, and establishes dolomitization model. The research results show as follows. (1)Based on the macroscopic distribution characteristics and microscopic grain morphology, the dolomites of Kelimoli Formation can be divided into finely-powder crystalline dolomite, laminated dolomite, residual structure fine grain dolomite, fine-medium grain dolomite A, fine-medium grain dolomite B, and medium-coarse porphyritic dolomite. (2)In the eastern restricted platform of western Ordos Basin, the laminated dolomite of Kelimoli Formation is affected by the quasi-contemporaneous microbial dolomitization, and its dolomitization fluid is from near-surface seawater. The finely-powder crystalline dolomite is originated from the quasi-contemporaneous evaporative pumping dolomitization, and its dolomitization fluid is from low-salinity evaporative seawater. In the central platform margin of western Ordos Basin, the dolomites of Kelimoli Formation are formed by quasi-contemporaneous reflux dolomitization and superimposed by shallow-medium burial-stage porewater dolomitization, where the residual structure fine grain dolomite, euhedral-subhedral fine-medium grain dolomite A, and anhedral fine-medium grain dolomite B are developed. Part of the fine-medium grain dolomite B developed near weathering crust in the east side of the platform margin zone is involved by the incorporation of meteoric water during diagenetic process. The medium-coarse porphyritic dolomite structurally associated with faults are developed on the central platform margin of western Ordos Basin, which corresponds to the medium-deep burial hydrothermal dolomitization involving marine-derived brines in the early period. (3)The dolomitization of Kelimoli Formation are mainly attributed to the quasi-contemporaneous evaporative pumping and reflux-seepage processes, followed by porewater dolomitization in shallow-medium burial period, hydrothermal dolomitization in medium-deep burial period, and early microbial dolomitization.

Key words: western Ordos Basin, Ordovician, Kelimoli Formation, dolomitization, reservoir

中图分类号:

TE121.1

白莹, 高建荣, 赵振宇. 鄂尔多斯盆地西缘奥陶系克里摩里组白云岩成因[J]. 石油学报, 2025, 46(8): 1517-1535,1627.

Bai Ying, Gao Jianrong, Zhao Zhenyu. Dolomite genesis of Ordovician Kelimoli Formation in western Ordos Basin[J]. Acta Petrolei Sinica, 2025, 46(8): 1517-1535,1627.

参考文献

[1] 赵文智, 沈安江, 胡素云, 等.中国碳酸盐岩储集层大型化发育的地质条件与分布特征[J].石油勘探与开发, 2012, 39(1):1-12.
ZHAO Wenzhi, SHEN Anjiang, HU Suyun, et al.Geological conditions and distributional features of large-scale carbonate reservoirs onshore China[J].Petroleum Exploration and Development, 2012, 39(1):1-12.
[2] JIANG Lei, CAI Chunfang, WORDEN R H, et al.Multiphase dolomitization of deeply buried Cambrian petroleum reservoirs, Tarim Basin, north-west China[J].Sedimentology, 2016, 63(7):2130-2157.
[3] 钱一雄, 武恒志, 周凌方, 等.川西中三叠统雷口坡组三段-四段白云岩特征与成因——来自于岩相学及地球化学的约束[J].岩石学报, 2019, 35(4):1161-1180.
QIAN Yixiong, WU Hengzhi, ZHOU Lingfang, et al.Characteristic and origin of dolomites in the third and fourth members of Leikoupo Formation of the Middle Triassic in NW Sichuan Basin:constraints in mineralogical, petrographic and geochemical data[J].Acta Petrologica Sinica, 2019, 35(4):1161-1180.
[4] ADAMS J E, RHODES M L.Dolomitization by seepage refluxion[J].AAPG Bulletin, 1960, 44(12):1912-1920.
[5] BAI Ying, LIU Wei, XU Wanglin.Dolomite genesis and dolomitization mechanisms of the Ordovician Lower Yingshan Formation, Gucheng area, Tarim Basin, China[J].Journal of Petroleum Science and Engineering, 2022, 215:110570.
[6] VASCONCELOS C, MCKENZIE J A.Microbial mediation of modern dolomite precipitation and diagenesis under anoxic conditions (Lagoa Vermelha, Rio de Janeiro, Brazil)[J].Journal of Sedimentary Research, 1997, 67(3):378-390.
[7] QING Hairuo, QIAO Zhanfeng, ZHANG Siyang, et al.δ²⁶Mg-δ¹³C-δ¹⁸O systems as geochemical tracers for dolomite recrystallization:a case study of Lower Ordovician dolomite from Tarim Basin[J].Chemical Geology, 2023, 619:121302.
[8] MACHEL H G, BURTON E A.Burial-diagenetic sabkha-like gypsum and anhydrite nodules[J].Journal of Sedimentary Research, 1991, 61(3):394-405.
[9] 沈安江, 罗宪婴, 胡安平, 等.从准同生到埋藏环境的白云石化路径及其成储效应[J].石油勘探与开发, 2022, 49(4):637-647.
SHEN Anjiang, LUO Xianying, HU Anping, et al.Dolomitization evolution and its effects on hydrocarbon reservoir formation from penecontemporaneous to deep burial environment[J].Petroleum Exploration and Development, 2022, 49(4):637-647.
[10] JIANG Lei, WORDEN R H, CAI Chunfang, et al.Dolomitization of gas reservoirs:the Upper Permian Changxing and Lower Triassic Feixianguan formations, northeast Sichuan Basin, China[J].Journal of Sedimentary Research, 2014, 84(10):792-815.
[11] 吴东旭, 孙六一, 周进高, 等.鄂尔多斯盆地西缘克里摩里组白云岩储层特征及成因[J].天然气工业, 2019, 39(6):51-62.
WU Dongxu, SUN Liuyi, ZHOU Jin’gao, et al.Characteristics and genesis of the Ordovician Kelimoli dolomite reservoirs in the western edge of the Ordos Basin[J].Natural Gas Industry, 2019, 39(6):51-62.
[12] 于洲, 周进高, 李程善, 等.鄂尔多斯盆地西缘奥陶纪克里摩里期—乌拉力克期构造-岩相古地理特征[J].天然气地球科学, 2021, 32(6):816-825.
YU Zhou, ZHOU Jin’gao, LI Chengshan, et al.Tectonic-lithofacies paleogeographic characteristics of Ordovician Kelimoli and Wulalike stages in the western edge of Ordos Basin[J].Natural Gas Geoscience, 2021, 32(6):816-825.
[13] 席胜利, 刘新社, 任军峰, 等.鄂尔多斯盆地风险勘探领域油气成藏认识新进展与勘探潜力[J].中国石油勘探, 2023, 28(3):34-48.
XI Shengli, LIU Xinshe, REN Junfeng, et al.New understanding of hydrocarbon accumulation and exploration potential in risk exploration field in Ordos Basin[J].China Petroleum Exploration, 2023, 28(3):34-48.

[14] 李江海, 韩喜球, 毛翔.全球构造图集[M].北京:地质出版社, 2014.
LI Jianghai, HAN Xiqiu, MAO Xiang.Global atlas of tectonics[M].Beijing:Geological Publishing House, 2014.
[15] 孙华丽, 高建荣, 付玲, 等.鄂尔多斯盆地西缘奥陶系古环境恢复及沉积体系分析[J].东北石油大学学报, 2023, 47(1):44-56.
SUN Huali, GAO Jianrong, FU Ling, et al.Restoration of Ordovician paleoenvironment and analysis of sedimentary system in the western margin of Ordos Basin[J].Journal of Northeast Petroleum University, 2023, 47(1):44-56.
[16] 何登发, 包洪平, 孙方源, 等.鄂尔多斯盆地中央古隆起的地质结构与成因机制[J].地质科学, 2020, 55(3):627-656.
HE Dengfa, BAO Hongping, SUN Fangyuan, et al.Geologic structure and genetic mechanism for the central uplift in the Ordos Basin[J].Chinese Journal of Geology, 2020, 55(3):627-656.
[17] 包洪平, 杨帆, 蔡郑红, 等.鄂尔多斯盆地奥陶系白云岩成因及白云岩储层发育特征[J].天然气工业, 2017, 37(1):32-45.
BAO Hongping, YANG Fan, CAI Zhenghong, et al.Origin and reservoir characteristics of Ordovician dolostones in the Ordos Basin[J].Natural Gas Industry, 2017, 37(1):32-45.
[18] 郭彦如, 赵振宇, 付金华, 等.鄂尔多斯盆地奥陶纪层序岩相古地理[J].石油学报, 2012, 33(增刊2):95-109.
GUO Yanru, ZHAO Zhenyu, FU Jinhua, et al.Sequence lithofacies paleogeography of the Ordovician in Ordos Basin, China[J].Acta Petrolei Sinica, 2012, 33(S2):95-109.
[19] 郭彦如, 赵振宇, 徐旺林, 等.鄂尔多斯盆地奥陶系层序地层格架[J].沉积学报, 2014, 32(1):44-60.
GUO Yanru, ZHAO Zhenyu, XU Wanglin, et al.Sequence stratigraphy of the Ordovician System in the Ordos Basin[J].Acta Sedimentologica Sinica, 2014, 32(1):44-60.
[20] 陈志雄, 张凤奇, 赵振宇, 等.鄂尔多斯盆地西缘下古生界奥陶系包裹体特征及油气充注史[J].天然气地球科学, 2023, 34(6):1028-1038.
CHEN Zhixiong, ZHANG Fengqi, ZHAO Zhenyu, et al.Characteristics of Lower Paleozoic Ordovician inclusions and oil and gas filling history in the western margin of Ordos Basin[J].Natural Gas Geoscience, 2023, 34(6):1028-1038.
[21] 吴伟涛, 赵靖舟, 孙六一, 等.鄂尔多斯盆地西部奥陶系克里摩里组天然气成藏特征[J].天然气地球科学, 2015, 26(10):1862-1872.
WU Weitao, ZHAO Jingzhou, SUN Liuyi, et al.Accumulation characteristics of natural gas from the Ordovician Kelimoli Formation, western Ordos Basin[J].Natural Gas Geoscience, 2015, 26(10):1862-1872.
[22] 杨华, 包洪平.鄂尔多斯盆地奥陶系中组合成藏特征及勘探启示[J].天然气工业, 2011, 31(12):11-20.
YANG Hua, BAO Hongping.Characteristics of hydrocarbon accumulation in the Middle Ordovician assemblages and their significance for gas exploration in the Ordos Basin[J].Natural Gas Industry, 2011, 31(12):11-20.
[23] 张道锋, 刘新社, 高星, 等.鄂尔多斯盆地西部奥陶系海相碳酸盐岩地质特征与成藏模式研究[J].天然气地球科学, 2016, 27(1):92-101.
ZHANG Daofeng, LIU Xinshe, GAO Xing, et al.Geological characteristics and accumulation model of Ordovician marine carbonate in western Ordos Basin[J].Natural Gas Geoscience, 2016, 27(1):92-101.
[24] 姜在兴.沉积学[M].2版.北京:石油工业出版社, 2010:295.
JIANG Zaixing.Sedimentology[M].2nd ed.Beijing:Petroleum Industry Press, 2010:295.
[25] GOLDSMITH J R, GRAF D L.Structural and compositional variations in some natural dolomites[J].The Journal of Geology, 1958, 66(6): 678-693.
[26] REEDER R J, MARKGRAF S A.High-temperature crystal chemistry of dolomite[J].American Mineralogist, 1986, 71(5/6):795-804.
[27] YOU Xuelian, SUN Shu, ZHU Jingquan.Significance of fossilized microbes from the Cambrian stromatolites in the Tarim Basin, northwest China[J].Science China Earth Sciences, 2014, 57(12):2901-2913.
[28] 黄擎宇, 刘伟, 张艳秋, 等.塔里木盆地中央隆起区上寒武统—下奥陶统白云岩地球化学特征及白云石化流体演化规律[J].古地理学报, 2016, 18(4):661-676.
HUANG Qingyu, LIU Wei, ZHANG Yanqiu, et al. Geochemistry and evolution of dolomitizing fluids of the Upper Cambrian-Lower Ordovician dolostones in central uplift, Tarim Basin[J].Journal of Palaeogeography, 2016, 18(4):661-676.
[29] DAVIES G R, SMITH L B JR.Structurally controlled hydrothermal dolomite reservoir facies:an overview[J].AAPG Bulletin, 2006, 90(11):1641-1690.
[30] SMITH L B JR.Origin and reservoir characteristics of Upper Ordovician Trenton-Black River hydrothermal dolomite reservoirs in New York [J].AAPG Bulletin, 2006, 90(11):1691-1718.
[31] CHOQUETTE P W, PRAY L C.Geologic nomenclature and classification of porosity in sedimentary carbonates[J].AAPG Bulletin, 1970, 54(2):207-250.
[32] LØNØY A.Making sense of carbonate pore systems[J].AAPG Bulletin, 2006, 90(9):1381-1405.
[33] HU Yongjie, CAI Chunfang, LI Ying, et al.Sedimentary and diagenetic archive of a deeply buried, Upper Ediacaran microbialite reservoir, southwestern China[J].AAPG Bulletin, 2023, 107(3):387-412.
[34] HU Yongjie, CAI Chunfang, PEDERSON C L, et al.Dolomitization history and porosity evolution of a giant, deeply buried Ediacaran gas field (Sichuan Basin, China)[J].Precambrian Research, 2020, 338:105595.
[35] MCLENNAN S M.Relationships between the trace element composition of sedimentary rocks and upper continental crust[J].Geochemistry, Geophysics, Geosystems, 2001, 2(1):2000GC000109.
[36] GOLDSTEIN R H, REYNOLDS T J.Systematics of fluid inclusions in diagenetic minerals[M].Tulsa:SEPM Short Course, 1994:199.
[37] 任战利.鄂尔多斯盆地热演化史与油气关系的研究[J].石油学报, 1996, 17(1):17-24.
REN Zhanli.Research on the relations between geothermal history and oil-gas accumulation in the Ordos Basin[J].Acta Petrolei Sinica, 1996, 17(1):17-24.
[38] 任战利.利用磷灰石裂变径迹法研究鄂尔多斯盆地地热史[J].地球物理学报, 1995, 38(3):339-349.
REN Zhanli.Thermal history of Ordos Basin assessed by apatite fission track analysis[J]. Chinese Journal of Geophysics, 1995, 38(3):339-349.
[39] 刘大卫, 蔡春芳, 扈永杰, 等.深层白云岩多期白云石化及其对孔隙演化的影响——以川中地区下寒武统龙王庙组为例[J].中国矿业大学学报, 2020, 49(6):1150-1165.
LIU Dawei, CAI Chunfang, HU Yongjie, et al.Multi-stage dolomitization process of deep burial dolostones and its influence on pore evolution:a case study of Longwangmiao Formation in the Lower Cambrian of central Sichuan Basin[J].Journal of China University of Mining & Technology, 2020, 49(6):1150-1165.
[40] CAI Chunfang, LI Kaikai, LI Hongtao, et al.Evidence for cross formational hot brine flow from integrated ⁸⁷Sr/⁸⁶Sr, REE and fluid inclusions of the Ordovician veins in central Tarim, China[J].Applied Geochemistry, 2008, 23(8):2226-2235.
[41] HU Yongjie, CAI Chunfang, LIU Dawei, et al.Formation, diagenesis and palaeoenvironmental significance of Upper Ediacaran fibrous dolomite cements[J].Sedimentology, 2020, 67(2):1161-1187.
[42] HU Yongjie, CAI Chunfang, LI Ying, et al.Evolution of diagenetic fluids in the deeply buried, Upper Ediacaran Dengying Formation, central Sichuan Basin, China[J].Australian Journal of Earth Sciences, 2023, 70(2):285-301.
[43] 刘建章, 陈诚, 蔡忠贤, 等.柯坪地区中下寒武统走滑断裂带方解石脉期次、古流体演化与油气充注历史[J].地球科学, 2023, 48(6): 2189-2203.
LIU Jianzhang, CHEN Cheng, CAI Zhongxian, et al.Division of calcite veins stage, paleo-fluid evolution and hydrocarbon charging history in the Middle and Lower Cambrian strike-slip fault zone in Keping area, northwest of Tarim Basin[J].Earth Science, 2023, 48(6):2189-2203.
[44] CAI Chunfang, LIU Dawei, HU Yongjie, et al.Interlinked marine cycles of methane, manganese, and sulfate in the post-Marinoan Doushantuo cap dolostone[J].Geochimica et Cosmochimica Acta, 2023, 346:245-258.
[45] CAI Chunfang, LYONS T W, SUN Peng, et al.Enigmatic super-heavy pyrite formation:novel mechanistic insights from the aftermath of the Sturtian Snowball Earth[J].Geochimica et Cosmochimica Acta, 2022, 334:65-82.
[46] CAI Chunfang, LI Kaikai, LIU Dawei, et al.Anaerobic oxidation of methane by Mn oxides in sulfate-poor environments[J].Geology, 2021, 49(7):761-766.
[47] BUDD D A.Cenozoic dolomites of carbonate islands:their attributes and origin[J].Earth-Science Reviews, 1997, 42(1/2):1-47.
[48] 黄擎宇, 张哨楠, 张斯杨, 等.白云岩结构对储集空间发育的控制作用——以塔里木盆地中央隆起区寒武系—奥陶系白云岩为例[J].天然气地球科学, 2014, 25(3):341-350.
HUANG Qingyu, ZHANG Shaonan, ZHANG Siyang, et al.Textural control on the development of dolomite reservoir:a study from the Cambrian-Ordovician dolomite, central Tarim Basin, NW China[J].Natural Gas Geoscience, 2014, 25(3):341-350.
[49] 郝乐燃, 杨德彬, 许文良, 等.华北克拉通东北部新太古代晚期岩浆作用和地壳增生:锆石U-Pb-Hf同位素、微量元素和地球化学制约[J].岩石学报, 2020, 36(4):1076-1090.
H AO Leran, YANG Debin, XU Wenliang, et al.Late Neoarchean magmatism and crustal growth in northeastern North China craton:constraints from zircon U-Pb-Hf isotope, trace elements and whole rock geochemistry[J].Acta Petrologica Sinica, 2020, 36(4):1076-1090.
[50] HOOD S D, NELSON C S, KAMP P J J.Burial dolomitisation in a non-tropical carbonate petroleum reservoir:the Oligocene Tikorangi Formation, Taranaki Basin, New Zealand[J].Sedimentary Geology, 2004, 172(1/2):117-138.

鄂尔多斯盆地西缘奥陶系克里摩里组白云岩成因

Dolomite genesis of Ordovician Kelimoli Formation in western Ordos Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	杨兆彪, 卢本举, 周国晓, 陈河青, 闫霞, 李存磊, 马行陟, 高为, 刘常青, 张宝鑫, 王怀厂, 冯帅龙, 王嘉楠, 梁宇辉, 王钰强. 深部煤层气地质特殊性与释放产出规律[J]. 石油学报, 2025, 46(8): 1464-1476.
[2]	胡宗全, 林会喜, 邓尚, 张继标, 李映涛, 王千军, 王石, 贾会冲, 潘磊, 刘大卫. 断裂及裂缝对不同岩性储层的改造作用[J]. 石油学报, 2025, 46(8): 1489-1501.
[3]	王福伟, 陈冬霞, 姜梦雅, 完玛仁增, 刘晨, 王翘楚, 王昱超, 荣澜熹, 王玉杞, 成铭. 鄂尔多斯盆地姬塬地区延长组7段致密储层石油多尺度运移机制、成藏效应及富集模式[J]. 石油学报, 2025, 46(6): 1126-1143.
[4]	徐长贵, 王昕, 杨海风, 黄志, 王蔚, 张江涛. 渤海海域渤中凹陷中生界超深层火山岩潜山天然气勘探发现及意义[J]. 石油学报, 2025, 46(5): 843-856,908.
[5]	崔传智, 王俊康, 吴忠维, 李惊鸿, 李静, 钱银. 低渗透非均质储层压驱注水井非稳态压力特征[J]. 石油学报, 2025, 46(5): 938-952.
[6]	谢继容, 罗冰, 张玺华, 张本健, 陈聪, 冉崎, 赵容容, 彭瀚霖, 李天军, 陈康, 赖强, 何青林, 李文正, 袁海锋, 胡广. 四川盆地川中地区龙女寺茅口组白云岩气田勘探发现及其意义[J]. 石油学报, 2025, 46(4): 661-675,742.
[7]	赵波, 尹淑敏, 李忠权, 孙国昕, 刘筝, 李晶. 松辽盆地北部中央隆起带岩浆岩潜山优质储层特征及控制因素[J]. 石油学报, 2025, 46(4): 692-707.
[8]	范彩伟, 周刚, 唐蓿, 陈奎. 北部湾盆地乌石油田成藏条件及勘探开发关键技术[J]. 石油学报, 2025, 46(2): 466-482.
[9]	邓勇, 胡德胜, 张建新, 周刚, 胡晨晖, 钟佳, 徐守立. 北部湾盆地致密油气勘探新领域及资源潜力[J]. 石油学报, 2025, 46(1): 205-219.
[10]	赖锦, 宋翔羽, 杨薰, 赵仪迪, 田银宏, 李栋, 信毅, 张荣虎, 王贵文. 致密砂岩气储层测井综合评价技术研究进展[J]. 石油学报, 2025, 46(1): 220-235.
[11]	文龙, 罗冰, 周刚, 张本健, 葛冰飞, 杨岱林, 陶佳丽, 田兴旺, 马华灵, 严威, 史甲航, 刘常祺, 聂美怡, 李淑琦, 杨振中, 孙奕婷, 蒋航, 宋泽章. 四川盆地威寒1井奥陶系宝塔组天然气勘探发现及其意义[J]. 石油学报, 2024, 45(9): 1324-1335.
[12]	张云蛟, 王冠民, 殷梓原. 富铝硅酸盐岩风化壳结构划分[J]. 石油学报, 2024, 45(9): 1372-1384.
[13]	唐浩钦, 张本健, 熊晓军, 李天军. 四川盆地中北部二叠系茅口组复杂滩相白云岩储层地震预测——以角探1井区为例[J]. 石油学报, 2024, 45(9): 1385-1398,1421.
[14]	武瑾, 郭为, 郭伟, 赵圣贤, 苟其勇, 曾凡成, 刘宇, 邹晓品, 王玉满, 刘兆龙. 深层海相页岩气立体开发"甜点"岩相及其成因机制——以四川盆地南部泸州区块龙马溪组一段一亚段为例[J]. 石油学报, 2024, 45(8): 1219-1233.
[15]	郭威, 孙友宏, 李强, 邓孙华, 白奉田, 陈晨, 朱超凡, 王元, 刘召. 油页岩局部化学反应法原位转化技术及松辽盆地先导试验工程[J]. 石油学报, 2024, 45(7): 1104-1121,1129.