渤海湾盆地沙河街组—东营组深部热液对有机质富集的影响及模式

doi:10.7623/syxb202506005

石油学报 ›› 2025, Vol. 46 ›› Issue (6): 1089-1107.DOI: 10.7623/syxb202506005

• 地质勘探 • 上一篇

渤海湾盆地沙河街组—东营组深部热液对有机质富集的影响及模式

杨海风¹, 房舟^2,3, 王飞龙¹, 姜福杰^2,3, 齐振国^2,3, 刘梦醒¹, 郑晓薇^2,3, 陈迪^2,3, 胡涛^2,3

1. 中海石油(中国)有限公司天津分公司天津 300459;
2. 油气资源与工程全国重点实验室, 中国石油大学(北京) 北京 102249;
3. 中国石油大学(北京)地球科学学院北京 102249

收稿日期:2024-10-29 修回日期:2025-01-03 发布日期:2025-06-28
通讯作者: 姜福杰,男,1979年12月生,2008年获中国石油大学(北京)博士学位,现为中国石油大学(北京)教授、博士生导师,主要从事油气成藏机理与分布规律研究。Email:jfjhtb@163.com
作者简介:杨海风,男,1984年2月生,2009年获中国石油大学(北京)博士学位,现为中海石油(中国)有限公司天津分公司教授级高级工程师,主要从事海洋油气勘探管理和综合研究工作。Email:yanghf3@cnooc.com.cn
基金资助:
国家自然科学基金面上项目(No.42372147,No.42302142)、国家自然科学基金重点支持项目"渤海海域中生界潜山火山岩相发育机制及成储机理"(No.U24B2017)和中海石油(中国)有限公司"十四五"科技重大项目(CCL2022TJT0NST1844)资助。

Influence of deep hydrothermal fluid on organic matter enrichment and its activity mode in Shahejie Formation and Dongying Formation of Bohai Bay Basin

Yang Haifeng¹, Fang Zhou^2,3, Wang Feilong¹, Jiang Fujie^2,3, Qi Zhenguo^2,3, Liu Mengxing¹, Zheng Xiaowei^2,3, Chen Di^2,3, Hu Tao^2,3

1. Tianjin Branch, CNOOC China Limited, Tianjin 300459, China;
2. State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum (Beijing), Beijing 102249, China;
3. College of Geosciences, China University of Petroleum, Beijing 102249, China

Received:2024-10-29 Revised:2025-01-03 Published:2025-06-28

摘要/Abstract

摘要： 渤海湾盆地古近纪热液活动对沉积物中的有机质富集和烃源岩形成具有重要影响。综合岩石热解、常量元素、微量元素、稀土元素以及生物标志化合物等分析测试资料,探究了热液活动背景下渤海湾盆地东南缘古近系沙河街组—东营组烃源岩的有机质富集机理,建立了不同热液作用强度下的有机质富集模式。研究结果表明,随着热液活动强度不断增大,以δEu=2为界,烃源岩的总有机碳(TOC)含量具有先增大后减小的变化趋势,水体还原性具有先增强后减弱的变化规律,指示热液作用对研究区富有机质泥页岩的形成具有控制作用。当热液作用强度适宜(δEu＜2)时,深部热液上涌带来的大量营养物质会促进藻类勃发,古生产力迅速增大,且热液流体中携带的大量H₂S、SO₂等还原性气体将促进缺氧性水体的形成,有利于沉积有机质保存,因此强度适宜的热液作用有利于有机质大量富集。当热液活动强烈(δEu＞2)时,强烈的喷涌作用破坏有机质的保存条件,底层水体中氧气的溶解量增加,有机质被大量氧化分解,导致TOC含量逐渐降低。以δEu=2为界,建立了热液强度适宜条件下古生产力-保存条件主导的有机质富集模式,以及热液活动强烈条件下的有机质差异分布模式。未来,应重点探究热液活动-水介质条件(包括盐度、温度和非营养物质)-成烃生物种属-有机质富集之间的耦合关系,以更好地解释热液作用对沉积中有机质形成与富集的影响。研究认识对于明确优质烃源岩的分布进而寻找油气藏具有重要指导与借鉴意义。

关键词: 断陷湖盆, 有机质富集模式, 热液活动, 主控因素, 铕异常

Abstract: Paleogene hydrothermal activity in Bohai Bay Basin has a significant influence on the organic matter (OM)enrichment and formation of source rocks. Based on the analytical and testing data of rock pyrolysis, major and trace elements, rare earth elements and biomarkers, the paper explores the mechanism of OM enrichment under the background of hydrothermal activity in the Paleogene Shahejie Formation in the southeastern margin of Bohai Bay Basin, and then establishes the OM enrichment mode under different intensity of hydrothermal activity. The results show that using the threshold value of δEu=2, total organic carbon (TOC)content tends to increase first and then decrease with an increase in hydrothermal activity, and the water reducibility follows a pattern of first strengthening and then weakening. This suggests that hydrothermal activity plays a role in controlling the formation of OM-rich shale. Specifically, under the appropriate intensity of hydrothermal activity (δEu<2), the upwelling of deep hydrothermal fluid brings a large amount of nutrients, which can promote algal blooms and rapidly increase paleo-productivity. Additionally, a large number of reductive gas from hydrothermal fluids, such as H₂S and SO₂, and can also facilitate the formation of anoxic water body, which is favorable for the sedimentary OM preservation. Therefore, the hydrothermal activity with appropriate intensity is conducive to large-scale OM enrichment. Under the strong hydrothermal activity (δEu>2), the intensified upwelling destroys the OM preservation conditions, and the amount of dissolved oxygen in bottom waters increases. Moreover, a large amount of OM will be oxidized and decomposed, leading to the gradually decreasing TOC content. Using δEu=2 as the threshold value, this paper sets up the OM enrichment mode dominated by paleo-productivity and preservation conditions under the moderate hydrothermal activity, and the OM differential distribution pattern under intense hydrothermal activity. Future research should focus on investigating the coupling relationships between hydrothermal activity, water conditions (involving salinity, temperature, and non-nutrients), hydrocarbon-forming organism species, and OM enrichment, so as to better explain the mechanisms by which hydrothermal activities influence the OM formation and accumulation. The research results are of significant guidance and reference value for identifying the distribution of high-quality source rocks and then locating the oil and gas reservoirs.

Key words: faulted lacustrine basin, organic matter enrichment mode, hydrothermal activity, main controlling factors, Eu anomaly

中图分类号:

TE122.1

杨海风, 房舟, 王飞龙, 姜福杰, 齐振国, 刘梦醒, 郑晓薇, 陈迪, 胡涛. 渤海湾盆地沙河街组—东营组深部热液对有机质富集的影响及模式[J]. 石油学报, 2025, 46(6): 1089-1107.

Yang Haifeng, Fang Zhou, Wang Feilong, Jiang Fujie, Qi Zhenguo, Liu Mengxing, Zheng Xiaowei, Chen Di, Hu Tao. Influence of deep hydrothermal fluid on organic matter enrichment and its activity mode in Shahejie Formation and Dongying Formation of Bohai Bay Basin[J]. Acta Petrolei Sinica, 2025, 46(6): 1089-1107.

参考文献

[1] BRUYEVICH S V. Rates of mineralization of suspended organic carbon in the low latitudes of the Pacific during the pre-depositional stage[J].Geochemistry,1963,3:349-352.
[2] ERBA E.Calcareous nannofossils and Mesozoic oceanic anoxic events[J].Marine Micropaleontology,2004,52(1/4):85-106.
[3] JENKYNS H C.Cretaceous anoxic events:from continents to oceans[J].Journal of the Geological Society,1980,137(2):171-188.
[4] LECKIE R M,BRALOWER T J,CASHMAN R.Oceanic anoxic events and plankton evolution:biotic response to tectonic forcing during the Mid-Cretaceous[J].Paleoceanography,2002,17(3):13-1-13-29.
[5] WU Yuqi,JIANG Fujie,XU Yunlong,et al.Doubthouse climate influences on the carbon cycle and organic matter enrichment in lacustrine basins: astrochronological and paleontological perspectives[J].Journal of Asian Earth Sciences,2024,267:106155.
[6] JIANG Fujie,CHEN Di,ZHU Chenxi,et al.Mechanisms for the anisotropic enrichment of organic matter in saline lake basin:a case study of the Early Eocene Dongpu depression,eastern China[J].Journal of Petroleum Science and Engineering,2022,210:110035.
[7] 柳蓉,张坤,刘招君,等.中国油页岩富集与地质事件研究[J].沉积学报,2021,39(1):10-28.LIU Rong,ZHANG Kun,LIU Zhaojun,et al.Oil shale mineralization and geological events in China[J].Acta Sedimentologica Sinica,2021,39(1):10-28.
[8] SMITH M E,CARROLL A R,SINGER B S.Synoptic reconstruction of a major ancient lake system:Eocene Green River Formation,western United States[J].GSA Bulletin,2008,120(1/2):54-84.
[9] 杨华,梁晓伟,牛小兵,等.陆相致密油形成地质条件及富集主控因素——以鄂尔多斯盆地三叠系延长组7段为例[J].石油勘探与开发,2017,44(1):12-20.YANG Hua,LIANG Xiaowei,NIU Xiaobing,et al.Geological conditions for continental tight oil formation and the main controlling factors for the enrichment:a case of Chang 7 Member,Triassic Yanchang Formation,Ordos Basin,NW China[J].Petroleum Exploration and Development,2017,44(1):11-19.
[10] 陈志鹏,任战利,于春勇,等.银额盆地哈日凹陷下白垩统热水沉积岩特征及成因[J].地球科学,2018,43(6):1941-1956.CHEN Zhipeng,REN Zhanli,YU Chunyong,et al.Characteristics and genetic analysis of hydrothermal sediment of Lower Cretaceous in Hari depression,Yin’e Basin[J].Earth Science,2018,43(6):1941-1956.
[11] WU Yuqi,JIANG Fujie,HU Tao,et al.Shale oil content evaluation and sweet spot prediction based on convolutional neural network[J].Marine and Petroleum Geology,2024,167:106997.
[12] 周荔青,雷一心.松辽盆地断陷层系大、中型油气田形成条件及勘探方向[J].石油与天然气地质,2006,27(6):820-826.ZHOU Liqing,LEI Yixin.Formation conditions for middle and large oil/gas fields in rift sequences of Songliao Basin and thear future exploration targets[J].Oil & Gas Geology,2006,27(6):820-826.
[13] BEAULIEU S E,SZAFRAN ＇ SKI K M.InterRidge global database of active submarine hydrothermal vent fields version 3.4[dataset][DB/OL].(2020-05-26).https://doi.pangaea.de/10.1594/PANGAEA.917894.
[14] 朱日祥,赵盼,赵亮.新特提斯洋演化与动力过程[J].中国科学:地球科学,2022,52(1):1-25.ZHU Rixiang,ZHAO Pan,ZHAO Liang.Tectonic evolution and geodynamics of the Neo-Tethys ocean[J].Science China Earth Sciences,2022,65(1):1-24.
[15] 何治亮,金之钧,李双建,等.特提斯演化控制下盆地原型、改造与油气差异富集——基于波斯湾盆地与四川盆地的比较分析[J].中国科学:地球科学,2023,53(12):2914-2936.HE Zhiliang,JIN Zhijun,LI Shuangjian,et al.Prototypes,modifications,and hydrocarbon enrichment variations in basins influenced by Tethyan evolution:a comparative analysis of the Persian Gulf Basin and the Sichuan Basin[J].Science China Earth Sciences,2023,66(12):2871-2897.
[16] MOHAJJEL M,FERGUSSON C L,SAHANDI M R.Cretaceous-Tertiary convergence and continental collision,Sanandaj-Sirjan zone,western Iran[J].Journal of Asian Earth Sciences,2003,21(4):397-412.
[17] 贾智彬,侯读杰,孙德强,等.热水沉积判别标志及与烃源岩的耦合关系[J].天然气地球科学,2016,27(6):1025-1034.JIA Zhibin,HOU Dujie,SUN Deqiang,et al.Hydrothermal sedimentary discrimination criteria and its coupling relationship with the source rocks[J].Natural Gas Geoscience,2016,27(6):1025-1034.
[18] 朱光,刘程,顾承串,等.郯庐断裂带晚中生代演化对西太平洋俯冲历史的指示[J].中国科学:地球科学,2018,48(4):415-435. ZHU Guang,LIU Cheng,GU Chengchuan,et al.Oceanic plate subduction history in the western Pacific ocean:constraint from Late Mesozoic evolution of the Tan-Lu fault zone[J].Science China Earth Sciences,2018,61(4):386-405.
[19] MERCIER J L,HOU Minjing,VERGÉLY P,et al.Structural and stratigraphical constraints on the kinematics history of the southern Tan-Lu fault zone during the Mesozoic Anhui Province,China[J].Tectonophysics,2007,439(1/4):33-66.
[20] OKAY A I,CELAL ŞENGOÖR A M.Evidence for intracontinental thrust-related exhumation of the ultra-high-pressure rocks in China[J].Geology,1992,20(5):411-414.
[21] 张文正,杨华,解丽琴,等.湖底热水活动及其对优质烃源岩发育的影响——以鄂尔多斯盆地长7烃源岩为例[J].石油勘探与开发,2010,37(4):424-429.ZHANG Wenzheng,YANG Hua,XIE Liqin,et al.Lake-bottom hydrothermal activities and their influences on the high-quality source rock development:a case from Chang 7 source rocks in Ordos Basin[J]. Petroleum Exploration and Development,2010,37(4): 424-429.
[22] ZHANG Kun,LIU Rong,LIU Zhaojun,et al.Influence of palaeoclimate and hydrothermal activity on organic matter accumulation in lacustrine black shales from the Lower Cretaceous Bayingebi Formation of the Yin’e Basin,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2020,560:110007.
[23] 侯中帅,陈世悦,刘惠民,等.东营凹陷热液流体活动及其油气地质意义[J].中国矿业大学学报,2019,48(5):1090-1101.HOU Zhongshuai,CHEN Shiyue,LIU Huimin,et al.Hydrothermal fluid activity and its hydrocarbon geological significance in Dongying depression[J].Journal of China University of Mining & Technology,2019,48(5):1090-1101.
[24] 储呈林,陈强路,张博,等.热液活动对东二沟剖面玉尔吐斯组烃源岩形成的影响[J].沉积学报,2016,34(4):803-810.CHU Chenglin,CHEN Qianglu,ZHANG Bo,et al.Influence on formation of Yuertusi source rock by hydrothermal activities at Dongergou section,Tarim Basin[J].Acta Sedimentologica Sinica,2016,34(4):803-810.
[25] 柳益群,周鼎武,焦鑫,等.一类新型沉积岩:地幔热液喷积岩——以中国新疆三塘湖地区为例[J].沉积学报,2013,31(5): 773-781.LIU Yiqun,ZHOU Dingwu,JIAO Xin,et al.A new type of sedimentary rocks:mantle-originated hydroclastites and hydrothermal exhalites,Santanghu area,Xinjiang,NW China[J].Acta Sedimentologica Sinica,2013,31(5):773-781.
[26] 常海亮,郑荣才,郭春利,等.准噶尔盆地西北缘风城组喷流岩稀土元素地球化学特征[J].地质论评,2016,62(3):550-568. CHANG Hailiang,ZHENG Rongcai,GUO Chunli,et al.Characteristics of rare earth elements of exhalative rock in Fengcheng Formation,northwestern margin of Jungger Basin[J].Geological Review,2016,62(3):550-568.
[27] 文华国,郑荣才,QING Hairuo,等.酒泉盆地青西凹陷下沟组湖相热水沉积岩流体包裹体特征[J].地质学报,2010,84(1):106-116. WEN Huaguo,ZHENG Rongcai,QING Hairuo,et al.Characteristics of fluid inclusions in the lacustrine hydrothermal sedimentary rock from the Xiagou Formation,Lower Cretaceous in Qingxi sag,Jiuquan Basin [J].Acta Geologica Sinica,2010,84(1):106-116.
[28] 钟大康,苏琛,杨喆,等.内蒙古二连盆地白音查干凹陷下白垩统腾格尔组热水沉积过程中矿物沉淀顺序及其控制因素[J].古地理学报,2019,21(5):695-708.ZHONG Dakang,SU Chen,YANG Zhe,et al.Precipitation sequence of hydrothermal minerals and their controlling factors during the sedimentation:a case study of the Lower Cretaceous Tenggeer Formation in Baiyinchagan sag of Erlian Basin,Inner Mongolia[J].Journal of Palaeogeography (Chinese Edition),2019,21(5):695-708.
[29] GAO Ping,HE Zhiliang,LI Shuangjian,et al.Volcanic and hydrothermal activities recorded in phosphate nodules from the Lower Cambrian Niutitang Formation black shales in South China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2018,505:381-397.
[30] MCKIBBEN M A,WILLIAMS A E,HALL G E M.Solubility and transport of plantinum-group elements and Au in saline hydrothermal fluids:constraints from geothermal brine data[J].Economic Geology,1990,85(8):1926-1934.
[31] SCOTT C,LYONS T W.Contrasting molybdenum cycling and isotopic properties in euxinic versus non-euxinic sediments and sedimentary rocks:refining the paleoproxies[J].Chemical Geology,2012,324-325:19-27.
[32] QIU Xinwei,LIU Chiyang,MAO Guangzhou,et al.Major,trace and platinum-group element geochemistry of the Upper Triassic nonmarine hot shales in the Ordos Basin,central China[J].Applied Geochemistry,2015,53:42-52.
[33] WANG Ren,SHI Wanzhong,XIE Xiangyang,et al.Hydrothermal indications of Early Cretaceous red beds in lacustrine successions,North Yellow Sea Basin,eastern China[J].Marine and Petroleum Geology,2017,88:739-755.
[34] HE Taohua,LU Shuangfang,LI Wenhao,et al.Paleoweathering,hydrothermal activity and organic matter enrichment during the formation of Earliest Cambrian black strata in the northwest Tarim Basin,China[J].Journal of Petroleum Science and Engineering,2020,189:106987.
[35] ZHANG Wenzheng,YANG Weiwei,XIE Liqin.Controls on organic matter accumulation in the Triassic Chang 7 lacustrine shale of the Ordos Basin,central China[J].International Journal of Coal Geology,2017,183:38-51.
[36] HE Cong,JI Liming,WU Yuandong,et al.Characteristics of hydrothermal sedimentation process in the Yanchang Formation,South Ordos Basin,China:evidence from element geochemistry[J].Sedimentary Geology,2016,345:33-41.
[37] ZHU Chenxi,JIANG Fujie,ZHANG Pengyuan,et al.Identification of effective source rocks in different sedimentary environments and evaluation of hydrocarbon resources potential:a case study of Paleogene source rocks in the Dongpu depression,Bohai Bay Basin[J].Journal of Petroleum Science and Engineering,2021,201:108477.
[38] 胡涛,庞雄奇,姜福杰,等.陆相断陷咸化湖盆有机质差异富集因素探讨——以东濮凹陷古近系沙三段泥页岩为例[J].沉积学报,2021,39(1):140-152. HU Tao,PANG Xiongqi,JIANG Fujie,et al.Factors controlling differential enrichment of organic matter in saline lacustrine rift basin:a case study of third Member Shahejie Fm in Dongpu depression[J].Acta Sedimentologica Sinica,2021,39(1):140-152.
[39] 韩国猛,王丽,肖敦清,等.渤海湾盆地枣园油田古近系孔店组沸石矿物的岩浆热液成因[J].石油勘探与开发,2021,48(5):950-961.HAN Guomeng,WANG Li,XIAO Dunqing,et al.Magmatic hydrothermal fluid genesis of zeolite in the Paleogene Kongdian Formation of Zaoyuan oilfield,Bohai Bay Basin,China[J].Petroleum Exploration and Development,2021,48(5):950-961.
[40] 吴和源,汪建国,王培玺,等.渤海湾盆地南堡凹陷中—下寒武统白云岩成因及储层形成机理[J].石油学报,2018,39(4):416-426. WU Heyuan,WANG Jianguo,WANG Peixi,et al.Genesis of dolomite reservoir of Middle-Lower Cambrian in Nanpu sag,Bohai Bay Basin[J].Acta Petrolei Sinica,2018,39(4):416-426.
[41] 李继岩,王永诗,刘传虎,等.热液流体活动及其对碳酸盐岩储集层改造定量评价——以渤海湾盆地东营凹陷西部下古生界为例[J].石油勘探与开发,2016,43(3):359-366.LI Jiyan,WANG Yongshi,LIU Chuanhu,et al.Hydrothermal fluid activity and the quantitative evaluation of its impact on carbonate reservoirs:a case study of the Lower Paleozoic in the west of Dongying sag,Bohai Bay Basin,East China[J].Petroleum Exploration and Development,2016,43(3):359-366.
[42] YIN Jie,XU Changgui,HAO Fang,et al.Controls on organic matter enrichment in source rocks of the Shahejie Formation in the southwestern Bozhong sag,Bohai Bay Basin,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2020,560:110026.
[43] 池英柳,赵文智.渤海湾盆地新生代走滑构造与油气聚集[J].石油学报,2000,21(2):14-20.CHI Yingliu,ZHAO Wenzhi.Strike-slip deformation during the cenozoic and its influence on hydrocarbon accumulation in the Bohai Bay Basin[J].Acta Petrolei Sinica,2000,21(2):14-20.
[44] 朱光,刘国生,牛漫兰,等.郯庐断裂带的平移运动与成因[J].地质通报,2003,22(3):200-207.ZHU Guang,LIU Guosheng,NIU Manlan,et al.Transcurrent movement and genesis of the Tan-Lu fault zone[J].Geological Bulletin of China,2003,22(3):200-207.
[45] 朱光,牛漫兰,刘国生,等.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件[J].地质学报,2002,76(3):325-334.ZHU Guang,NIU Manlan,LIU Guosheng,et al.Structural,magmatic and sedimentary events of the Tan-Lu fault belt during its Early Cretaceous strike-slip movement[J].Acta Geologica Sinica,2002,76(3):325-334.
[46] 朱日祥,徐义刚,朱光,等.华北克拉通破坏[J].中国科学:地球科学,2012,42(8):1135-1159.ZHU Rixiang,XU Yigang,ZHU Guang,et al.Destruction of the North China craton[J].Science China Earth Sciences,2012,55(10):1565-1587.
[47] 陈印,朱光,胡召齐,等.华北克拉通东部盆地白垩—古近纪构造沉降的时空变化及其与克拉通破坏的关系[J].地质科学,2009,44(3):836-854. CHEN Yin,ZHU Guang,HU Zhaoqi,et al.Temporal-spatial changes of tectonic subsidence for Cretaceous-Paleogene basins in the eastern North China craton and their relations with the craton destruction[J].Chinese Journal of Geology,2009,44(3):836-854.
[48] 漆家福,邓荣敬,周心怀,等.渤海海域新生代盆地中的郯庐断裂带构造[J].中国科学D辑:地球科学,2008,38(增刊1):19-29. QI Jiafu,DENG Rongjing,ZHOU Xinhuai,et al.Structural characteristics of the Tan-Lu fault zone in Cenozoic basins offshore the Bohai Sea[J].Science in China Series D:Earth Sciences,2008,51(S2):20-31.
[49] CAO Yingchang,YUAN Guanghui,XU Jinjun,et al.The Bohai Bay Basin:a super basin in eastern China[R].SEG 3742256,2022.
[50] 张功成,佟殿君,陈凯,等.渤海湾超级油盆构造演化及其烃源岩发育[J].石油勘探与开发,2024,51(5):1008-1023.ZHANG Gongcheng,TONG Dianjun,CHEN Kai,et al.Tectonic evolution and source rocks development of the super oil-rich Bohai Bay Basin,East China[J].Petroleum Exploration and Development,2024,51(5):1008-1023.
[51] 李三忠,索艳慧,戴黎明,等.渤海湾盆地形成与华北克拉通破坏[J].地学前缘,2010,17(4):64-89.LI Sanzhong,SUO Yanhui,DAI Liming,et al.Development of the Bohai Bay Basin and destruction of the North China craton[J].Earth Science Frontiers,2010,17(4):64-89.
[52] GILDER S A,LELOUP P H,COURTILLOT V,et al.Tectonic evolution of the Tancheng-Lujiang (Tan-Lu)fault via Middle Triassic to Early Cenozoic paleomagnetic data[J].Journal of Geophysical Research:Solid Earth,1999,104(B7):15365-15390.
[53] 朱日祥,徐义刚.西太平洋板块俯冲与华北克拉通破坏[J].中国科学:地球科学,2019,49(9):1346-1356.ZHU Rixiang,XU Yigang.The subduction of the West Pacific plate and the destruction of the North China craton[J].Science China Earth Sciences,2019,62(9):1340-1350.
[54] 朱光,刘国生,DUNLAP W J,等.郯庐断裂带同造山走滑运动的⁴⁰Ar/³⁹Ar年代学证据[J].科学通报,2004,49(2):190-198. ZHU Guang,LIU Guosheng,DUNLAP W J,et al.⁴⁰Ar/³⁹Ar geochronological constraints on syn-orogenic strike-slip movement of Tan-Lu fault zone[J].Chinese Science Bulletin,2004,49(5):499-508.
[55] 郑永飞,吴福元.克拉通岩石圈的生长和再造[J].科学通报,2009,54(14):1945-1949.ZHENG Yongfei,WU Fuyuan.Growth and reworking of cratonic lithosphere[J].Chinese Science Bulletin,2009,54(19):3347-3353.
[56] REN Jianye,TAMAKI K,LI Sitian,et al.Late Mesozoic and Cenozoic rifting and its dynamic setting in eastern China and adjacent areas[J].Tectonophysics,2002,344(3/4):175-205.
[57] ZHU Guang,JIANG Dazhi,ZHANG Bilong,et al.Destruction of the eastern North China craton in a backarc setting:evidence from crustal deformation kinematics[J].Gondwana Research,2012,22(1):86-103.
[58] 王小凤.郯庐断裂带[M].北京:地质出版社,2000:1-200.WANG Xiaofeng.Tanlu fault zone[M].Beijing:Geological Publishing House,2000:1-200.
[59] 徐杰,宋长青,高战武.营口-潍坊断裂带新生代活动的特征[J].地震地质,1999,21(4):289-300.XU Jie,SONG Changqing,GAO Zhanwu.Active characters of the Yingkou Weifang fault zone in the Cenozoic era[J].Seismology and Geology,1999,21(4):289-300.
[60] 刘池洋,黄雷,张东东,等.石油贫富悬殊的成因:来自华北克拉通东部南北新生代盆地的启示[J].中国科学:地球科学,2018,48(11):1506-1526.LIU Chiyang,HUANG Lie,ZHANG Dongdong,et al.Genetic causes of oil-rich and oil-poor reservoirs:implications from two Cenozoic basins in the eastern North China craton[J].Science China Earth Sciences,2018,61(12):1910-1931.
[61] 高祥林.渤海中部郯庐断裂带的近期活动与渤海新近纪新生断裂[J].地质科学,2006,41(2):355-364.GAO Xianglin.Recent activities of the Tan-Lu fault zone in the central Bohai Sea and newly generated faults during Neogene in Bohai[J].Chinese Journal of Geology,2006,41(2):355-364.
[62] 邓运华.渤海湾盆地上第三系油藏形成与勘探[J].中国海上油气(地质),2000,14(3):163-167.DENG Yunhua.Neogene oil accumulations and their exploration in Bohai Bay Basin[J].China Offshore Oil and Gas (Geology),2000,14(3):163-167.
[63] 田立新,王清斌,刘晓健,等.渤海海域莱州湾凹陷沙河街组硅化碎屑岩地质特征及其储层意义[J].石油与天然气地质,2020,41(5):1073-1082.TIAN Lixin,WANG Qingbin,LIU Xiaojian,et al.Geological features and their participation in the formation of silicified clastic reservoirs in the Shahejie Formation of Laizhouwan sag,Bohai Sea[J].Oil & Gas Geology,2020,41(5):1073-1082.
[64] 刘晓健,王清斌,代黎明,等.莱州湾凹陷火山岩-湖相碳酸盐岩混积岩储层特征和成因[J].地球科学,2020,45(10):3579-3588. LIU Xiaojian,WANG Qingbin,DAI Liming,et al.Reservoir characteristics and formation mechanisms of lacustrine carbonate and volcanics mixing sediments,Laizhouwan sag[J].Earth Science,2020,45(10):3579-3588.
[65] 王航,杨海风,黄振,等.走滑强控型盆缘洼陷控洼机制及主烃灶预测——以渤海盆地庙西南洼为例[J].成都理工大学学报(自然科学版),2021,48(1):53-62.WANG Hang,YANG Haifeng,HUANG Zhen,et al.The depression-controlled mechanism and prediction of hydrocarbon kitchen in the strike slip fault-controlled marginal sag:a case study of the Miaoxi sag,Bohai Basin,China[J].Journal of Chengdu University of Technology (Science & Technology Edition),2021,48(1):53-62.
[66] 杨海风,涂翔,赵弟江,等.渤海湾盆地莱州湾凹陷沙河街组第三、第四段烃源岩有机相特征[J].成都理工大学学报(自然科学版),2021,48(1):72-81. YANG Haifeng,TU Xiang,ZHAO Dijiang,et al.Organic facies characteristics of source rocks on the 3rd and 4th Member of Shahejie Formation in the southern Laizhouwan depression,Bohai Bay Basin,China[J].Journal of Chengdu University of Technology (Science & Technology Edition),2021,48(1):72-81.
[67] MENG Qingren,ZHOU Zhonghe,ZHU Rixiang,et al.Cretaceous Basin evolution in northeast Asia:tectonic responses to the paleo-Pacific plate subduction[J].National Science Review,2022,9(1):nwab088.
[68] 徐长贵,杨海风,王德英,等.渤海海域莱北低凸起新近系大面积高丰度岩性油藏形成条件[J].石油勘探与开发,2021,48(1): 12-25.XU Changgui,YANG Haifeng,WANG Deying,et al.Formation conditions of Neogene large-scale high-abundance lithologic reservoir in the Laibei low uplift,Bohai Sea,East China[J].Petroleum Exploration and Development,2021,48(1):12-25.
[69] 中国石油天然气总公司.陆相烃源岩地球化学评价方法:SY/T 5735—1995[S].北京:石油工业出版社,1996.China National Petroleum Company.Geochemical evaluation standard of terrestrial hydrocarbon source rock:SY/T 5735-1995[S].Beijing:Petroleum Industry Press,1996.
[70] 邬立言,顾信章,盛志纬,等.生油岩热解快速定量评价[M].北京:科学出版社,1986.WU Liyan,GU Xinzhang,SHENG Zhiwei,et al.Rapid quantitative evaluation of oil source rocks with pyrolysis method[M].Beijing:Science Press,1986.
[71] ALDERTON D H M,PEARCE J A,POTTS P J.Rare earth element mobility during granite alteration:evidence from southwest England[J]. Earth and Planetary Science Letters,1980,49(1):149-165.
[72] EXLEY R A.Microprobe studies of REE-rich accessory minerals:implications for Skye granite petrogenesis and REE mobility in hydrothermal systems[J].Earth and Planetary Science Letters,1980,48(1):97-110.
[73] MICHARD A,ALBARōDE F,MICHARD G,et al.Rare-earth elements and uranium in high-temperature solutions from East Pacific Rise hydrothermal vent field (13°N)[J].Nature,1983,303(5920):795-797.
[74] JAMES R H,ELDERFIELD H,PALMER M R.The chemistry of hydrothermal fluids from the Broken Spur site,29°N Mid-Atlantic ridge [J].Geochimica et Cosmochimica Acta,1995,59(4):651-659.
[75] MILLS R A,ELDERFIELD H.Rare earth element geochemistry of hydrothermal deposits from the active TAG Mound,26°N Mid-Atlantic ridge[J].Geochimica et Cosmochimica Acta,1995,59(17):3511-3524.
[76] 丁振举,刘丛强,姚书振,等.海底热液系统高温流体的稀土元素组成及其控制因素[J].地球科学进展,2000,15(3):307-312.DING Zhenju,LIU Congqiang,YAO Shuzhen,et al.Rare earth elements compositions of high-temperature hydrothermal fluids in sea floor and control factors[J].Advance in Earth Sciences,2000,15(3):307-312.
[77] LIU Weihua,ETSCHMANN B,MIGDISOV A,et al.Revisiting the hydrothermal geochemistry of europium (II/III)in light of new in-situ XAS spectroscopy results[J].Chemical Geology,2017,459:61-74.
[78] DANIELSON A,MÖLLER P,DULSKI P.The europium anomalies in banded iron formations and the thermal history of the oceanic crust[J]. Chemical Geology,1992,97(1/2):89-100.
[79] 赵振华.某些常用稀土元素地球化学参数的计算方法及其地球化学意义[J].地质地球化学,1985(增刊1):11-14.ZHAO Zhenhua.Calculating methods geochemical parameters of some commonly used rare earth elements and their geochemical significance[J].Geology-Geochemistry,1985(S1):11-14.
[80] TAYLOR S R,MCLENNAN S M.The continental crust:its composition and evolution[M].Oxford:Blackwell Scientific Publications,1985:311.
[81] 王中刚,于学元,赵振华,等.稀土元素地球化学[M].北京:科学出版社,1989.WANG Zhonggang,YU Xueyuan,ZHAO Zhenhua,et al.Rare earth element geochemistry[M].Beijing:Science Press,1989.
[82] KLINKHAMMER G P,ELDERFIELD H,EDMOND J M,et al.Geochemical implications of rare earth element patterns in hydrothermal fluids from mid-ocean ridges[J].Geochimica et Cosmochimica Acta,1994,58(23):5105-5113.
[83] BOYNTON W V.Cosmochemistry of the rare earth elements:meteorite studies[J].Developments in Geochemistry,1984,2:63-114.
[84] CHOI J H,HARIYA Y.Geochemistry and depositional environment of Mn oxide deposits in the Tokoro belt,northeastern Hokkaido,Japan[J]. Economic Geology,1992,87(5):1265-1274.
[85] BOSTRÖM K,KRAEMER T,GARTNER S.Provenance and accumulation rates of opaline silica,Al,Ti,Fe,Mn,Cu,Ni and Co in Pacific pelagic sediments[J].Chemical Geology,1973,11(2):123-148.
[86] DILLON P J,RIGLER F H.The phosphorus-chlorophyll relationship in lakes 1,2[J].Limnology and Oceanography,1974,19(5):767-773.
[87] TRIBOVILLARD N,ALGEO T J,LYONS T,et al.Trace metals as paleoredox and paleoproductivity proxies:an update[J].Chemical Geology,2006,232(1/2):12-32.
[88] DYMOND J,SUESS E,LYLE M.Barium in deep-sea sediment:a geochemical proxy for paleoproductivity[J].Paleoceanography,1992,7(2):163-181.
[89] LI Wenhao,LU Shuangfang,TAN Zhaozhao,et al.Lacustrine source rock deposition in response to coevolution of the paleoenvironment and formation mechanism of organic-rich shales in the Biyang depression,Nanxiang Basin[J].Energy & Fuels,2017,31(12):13519-13527.
[90] SONG Yu,LI Shuifu,HU Shouzhi.Warm-humid paleoclimate control of salinized lacustrine organic-rich shale deposition in the Oligocene Hetaoyuan Formation of the Biyang depression,East China[J].International Journal of Coal Geology,2019,202:69-84.
[91] XU Chuan,SHAN Xuanlong,HE Wentong,et al.The influence of paleoclimate and a marine transgression event on organic matter accumulation in lacustrine black shales from the Late Cretaceous,southern Songliao Basin,northeast China[J].International Journal of Coal Geology,2021,246:103842.
[92] XU Chuan,SHAN Xuanlong,LIN Heming,et al.The formation of Early Eocene organic-rich mudstone in the western Pearl River Mouth Basin,South China:insight from paleoclimate and hydrothermal activity[J].International Journal of Coal Geology,2022,253:103957.
[93] DAVIES G R,SMITH JR L B.Structurally controlled hydrothermal dolomite reservoir facies:an overview[J].AAPG Bulletin,2006,90(11):1641-1690.
[94] OREN A.Life at high salt concentrations,intracellular KCl concentrations,and acidic proteomes[J].Frontiers in Microbiology,2013,4:315.
[95] OREN A.Microbial life at high salt concentrations:phylogenetic and metabolic diversity[J].Saline Systems,2008,4(1):2.
[96] WARREN J K.Evaporites:a geological compendium[M].2nd ed.Cham:Springer,2016.
[97] 夏刘文,曹剑,边立曾,等.准噶尔盆地玛湖大油区二叠纪碱湖生物-环境协同演化及油源差异性[J].中国科学:地球科学,2022,52(4):732-746. XIA Liuwen,CAO Jian,BIAN Lizeng,et al.Co-evolution of paleo-environment and bio-precursors in a Permian alkaline lake,Mahu mega -oil province,Junggar Basin:implications for oil sources[J].Science China Earth Sciences,2022,65(3):462-476.
[98] VAN DOVER C L.The ecology of deep-sea hydrothermal vents[M].Princeton:Princeton University Press,2000.
[99] KOSCHINSKY A,GARBE-SCHÖNBERG D,SANDER S,et al.Hydrothermal venting at pressure-temperature conditions above the critical point of seawater,5°S on the Mid-Atlantic ridge[J].Geology,2008,36(8):615-618.
[100] LÓPEZ-GARCÍA P,LÓPEZ-LÓPEZ A,MOREIRA D,et al.Diversity of free-living prokaryotes from a deep-sea site at the Antarctic Polar Front[J].FEMS Microbiology Ecology,2001,36(2/3):193-202.
[101] 邱欣卫,刘池洋,毛光周,等.鄂尔多斯盆地延长组火山灰沉积物岩石地球化学特征[J].地球科学,2011,36(1):139-150.QIU Xinwei,LIU Chiyang,MAO Guangzhou,et al.Petrological- geochemical characteristics of volcanic ash sediments in Yanchang Formation in Ordos Basin [J].Earth Science,2011,36(1):139-150.
[102] JØRGENSEN B B.Mineralization of organic matter in the Sea bed—the role of sulphate reduction[J].Nature,1982,296(5858):643-645.
[103] CANFIELD D E,JØRGENSEN B B,FOSSING H,et al.Pathways of organic carbon oxidation in three continental margin sediments[J].Marine Geology,1993,113(1/2):27-40.
[104] 李鹏,刘全有,毕赫,等.火山活动与海侵影响下的典型湖相页岩有机质保存差异分析[J].地质学报,2021,95(3):632-642.LI Peng,LIU Quanyou,BI He,et al.Analysis of the difference in organic matter preservation in typical lacustrine shale under the influence of volcanism and transgression[J].Acta Geologica Sinica,2021,95(3):632-642.
[105] LIU Quanyou,LI Peng,JIN Zhijun,et al.Preservation of organic matter in shale linked to bacterial sulfate reduction (BSR)and volcanic activity under marine and lacustrine depositional environments[J].Marine and Petroleum Geology,2021,127:104950.
[106] STUIVER M.The sulfur cycle in lake waters during thermal stratification[J]. Geochimica et Cosmochimica Acta,1967,31(11):2151-2167.
[107] BERNER R A,RAISWELL R.C/S method for distinguishing freshwater from marine sedimentary rocks[J].Geology,1984,12(6):365-368.
[108] OHMOTO H.A seawater-sulfate origin for early Earth’s volcanic sulfur[J].Nature Geoscience,2020,13(8):576-583.
[109] 刘全有,李鹏,金之钧,等.湖相泥页岩层系富有机质形成与烃类富集——以长7为例[J].中国科学:地球科学,2022,52(2):270-290.LIU Quanyou,LI Peng,JIN Zhijun,et al.Organic-rich formation and hydrocarbon enrichment of lacustrine shale strata:a case study of Chang 7 Member[J].Science China Earth Sciences,2022,65(1):118-138.
[110] 刘全有,李鹏,金之钧,等.火山活动对海相和淡水湖相页岩形成的影响[J].地球化学,2022,51(5):556-569.LIU Quanyou,LI peng,JIN Zhijun,et al.Effect of volcanic activity on the formation of marine shale and freshwater lacustrine shale[J].Geochimica,2022,51(5):556-569.
[111] LALLIER-VERGōS E,BERTRAND P,DESPRAIRIES A.Organic matter composition and sulfate reduction intensity in Oman margin sediments[J].Marine Geology,1993,112(1/4):57-69.
[112] BOHACS K M,CARROLL A R,NEAL J E,et al.Lake- basin type,source potential,and hydrocarbon character:an integrated sequence-stratigraphic-geochemical fram ework[M]// GIERLOWSKI-KORDESCH E H,KELTS K R.Lake basins through space and time.AAPG,2000.
[113] 丁修建,柳广弟,黄志龙,等.有机质供给和保存在烃源岩形成中的控制作用[J].地球科学,2016,41(5):832-842. DING Xiujian,LIU Guangdi,HUANG Zhilong,et al.Controlling function of organic matter supply and preservation on formation of source rocks [J].Earth Science,2016,41(5):832-842.
[114] 王磊.鄂尔多斯盆地延长组长7期湖盆古生产力恢复及其控制因素[D].西安:西北大学,2015.WANG Lei.The recovery of the paleoproductivity in the period of Chang 7 in Ordos Basin and its control factors[D].Xi’an:Northwest University,2015.
[115] YANG Hua,ZHANG Wenzheng,WU Kai,et al.Uranium enrichment in lacustrine oil source rocks of the Chang 7 Member of the Yanchang Formation,Erdos Basin,China[J].Journal of Asian Earth Sciences,2010,39(4):285-293.
[116] KOOPMANS M P,RIJPSTRA W I C,KLAPWIJK M M,et al.A thermal and chemical degradation approach to decipher pristane and phytane precursors in sedimentary organic matter[J].Organic Geochemistry,1999,30(9):1089-1104.
[117] BROOKS J D,GOULD K,SMITH J W.Isoprenoid hydrocarbons in coal and petroleum[J].Nature,1969,222(5190):257-259.
[118] POWELL T G,MCKIRDY D M.Relationship between ratio of pristane to phytane,crude oil composition and geological environment in Australia[J].Nature Physical Science,1973,243(124):37-39.
[119] PETERS K E,WALTERS C C,MOLDOWAN J M.The biomarker guide[M].2nd ed.Cambridge:Cambridge University Press,2005.
[120] DING Xiujian,LIU Guangdi,ZHA Ming,et al.Relationship between total organic carbon content and sedimentation rate in ancient lacustrine sediments,a case study of Erlian Basin,northern China[J].Journal of Geochemical Exploration,2015,149:22-29.
[121] TYSON R V.Sedimentation rate,dilution,preservation and total organic carbon:some results of a modelling study[J].Organic Geochemistry,2001,32(2):333-339.
[122] 张慧芳,吴欣松,王斌,等.陆相湖盆沉积有机质富集机理研究进展[J].沉积学报,2016,34(3):463-477. ZHANG Huifang,WU Xinsong,WANG Bin,et al.Research progress of the enrichment mechanism of sedimentary organics in lacustrine basin [J].Acta Sedimentologica Sinica,2016,34(3):463-477.
[123] DEMAISON G J,MOORE G T.Anoxic environments and oil source bed genesis[J].Organic Geochemistry,1980,2(1):9-31.
[124] CALVERT S E,PEDERSEN T F,NAIDU P D,et al.On the organic carbon maximum on the continental slope of the eastern Arabian Sea[J]. Journal of Marine Research,1995,53(2):269-296.
[125] FILIPPELLI G M,SIERRO F J,FLORES J A,et al.A sediment-nutrient-oxygen feedback responsible for productivity variations in Late Miocene sapropel sequences of the western Mediterranean[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2003,190:335-348.
[126] INGALL E,JAHNKE R.Influence of water-column anoxia on the elemental fractionation of carbon and phosphorus during sediment diagenesis [J].Marine Geology,1997,139(1/4):219-229.

渤海湾盆地沙河街组—东营组深部热液对有机质富集的影响及模式

Influence of deep hydrothermal fluid on organic matter enrichment and its activity mode in Shahejie Formation and Dongying Formation of Bohai Bay 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]	王茂云, 曾溅辉, 王小娟, 陈冬霞, 吴长江, 潘珂, 张欢乐, 崔虎旺. 源-储分离型致密砂岩气藏中气水分布控制因素——以四川盆地中部地区沙溪庙组致密砂岩气为例[J]. 石油学报, 2024, 45(8): 1187-1201,1218.
[2]	赵波, 丁寒生, 尹淑敏, 张永成, 李忠权, 孙国昕, 刘筝. 松辽盆地北部中央隆起带基岩潜山天然气成藏主控因素与成藏模式[J]. 石油学报, 2024, 45(12): 1783-1799.
[3]	党伟, 张金川, 聂海宽, 王凤琴, 唐玄, 蒋恕, 魏晓亮, 刘秋波, 李沛, 李菲, 孙江涛. 页岩油微观赋存特征及其主控因素——以鄂尔多斯盆地延安地区延长组7段3亚段陆相页岩为例[J]. 石油学报, 2022, 43(4): 507-523.
[4]	唐勇, 宋永, 郭旭光, 赵靖舟, 吴涛, 黄立良, 何文军, 吴伟涛, 吴和源. 准噶尔盆地玛湖凹陷源上致密砾岩油富集的主控因素[J]. 石油学报, 2022, 43(2): 192-206.
[5]	刘翰林, 邹才能, 邱振, 潘松圻, 张文正, 荆振华, 郝记华, 尹帅, 吴松涛, 李士祥, 郭秋雷. 鄂尔多斯盆地延长组7段3亚段异常高有机质沉积富集因素[J]. 石油学报, 2022, 43(11): 1520-1541.
[6]	刘凯旋, 陈践发, 付娆, 汪华, 罗冰, 戴鑫, 师肖飞, 董勍伟. 富氦天然气藏成藏特征及主控因素[J]. 石油学报, 2022, 43(11): 1652-1663.
[7]	李婷婷, 朱光有, 赵坤, 王鹏举. 华南地区南华系大塘坡组黑色岩系地质地球化学特征与有机质富集机制[J]. 石油学报, 2021, 42(9): 1142-1162.
[8]	吴建发, 赵圣贤, 范存辉, 夏自强, 季春海, 张成林, 曹埒焰. 川南长宁地区龙马溪组富有机质页岩裂缝发育特征及其与含气性的关系[J]. 石油学报, 2021, 42(4): 428-446.
[9]	刘春, 陈世加, 赵继龙, 陈戈, 苏洲, 高乔. 远源油气成藏条件与富集主控因素——以库车坳陷南部斜坡带中生界-新生界油气藏为例[J]. 石油学报, 2021, 42(3): 307-318.
[10]	赵贤正, 李宏军, 付立新, 崔宇, 韩国猛, 楼达, 蒲秀刚, 刘国全, 姜文亚, 董雄英, 邹磊落. 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.
[11]	冯林杰, 蒋裕强, 刘菲, 谷一凡, 王占磊, 钟克修, 廖义沙. 川东地区开江—梁平海槽南段飞仙关组鲕滩储层特征及主控因素[J]. 石油学报, 2021, 42(10): 1287-1298.
[12]	王家豪, 王华, 肖敦清, 蒲秀刚, 韩文忠, 张伟. 陆相断陷湖盆异重流与滑塌型重力流沉积辨别[J]. 石油学报, 2020, 41(4): 392-402,411.
[13]	代一丁, 牛子铖, 汪旭东, 王小龙, 肖张波, 张凯迪, 赵璇. 珠江口盆地陆丰凹陷古近系与新近系油气富集规律的差异及其主控因素[J]. 石油学报, 2019, 40(s1): 41-52.
[14]	朱筱敏, 葛家旺, 吴陈冰洁, 张向涛, 汪旭东, 李晓燕, 黎明. 珠江口盆地陆丰凹陷深层砂岩储层特征及主控因素[J]. 石油学报, 2019, 40(s1): 69-80.
[15]	操应长, 杨田, 宋明水, 王艳忠, 马奔奔, 王健, 远光辉, 葸克来. 陆相断陷湖盆低渗透碎屑岩储层特征及相对优质储层成因——以济阳坳陷东营凹陷古近系为例[J]. 石油学报, 2018, 39(7): 727-743.