等时格架下陆相页岩多尺度岩相精细识别及控制因素分析——以渤海湾盆地东营凹陷为例

曹冰; 杜学斌; 陆永潮; 刘惠民; 刘占红; 马义权; 王勇; 赵珂; 杨盼; 彭丽

doi:10.11781/sysydz201905752

等时格架下陆相页岩多尺度岩相精细识别及控制因素分析——以渤海湾盆地东营凹陷为例

doi: 10.11781/sysydz201905752

曹冰¹,
杜学斌^2,3, ,,
陆永潮³,
刘惠民⁴,
刘占红^2,3,
马义权^2,3,
王勇⁴,
赵珂^2,3,
杨盼^2,3,
彭丽³

1. 中国海油(中国)有限公司上海分公司, 上海 200335;
2. 中国地质大学(武汉) 海洋学院, 武汉 430074;
3. 中国地质大学(武汉) 构造与油气资源教育部重点实验室, 武汉 430074;
4. 中国石化胜利油田分公司地质科学研究院, 山东东营 257015

基金项目:

国家科技重大专项（2016ZX05034002，2016ZX05060004，2016ZX05027001）资助。

详细信息

作者简介:
曹冰(1967-),男,高级工程师,从事非常规储层沉积学研究。E-mail:caobing@cnooc.com.cn。

通讯作者:
杜学斌(1977-),男,副教授,博士生导师,能源地质专业。E-mail:xbdu@cug.edu.cn。

中图分类号: TE122.1
计量
- 文章访问数: 875
- HTML全文浏览量: 134
- PDF下载量: 128
- 被引次数: 0
出版历程
- 收稿日期: 2019-03-27
- 修回日期: 2019-07-25
- 刊出日期: 2019-09-28

Identification and controlling factors of multi-scale lithofacies for continental shale under an isochronous stratigraphic framework: a case study in Dongying Sag, Bohai Bay Basin

CAO Bing¹,
DU Xuebin^{2,3
, ,},
LU Yongchao³,
LIU Huimin⁴,
LIU Zhanhong^2,3,
MA Yiquan^2,3,
WANG Yong⁴,
ZHAO Ke^2,3,
YANG Pan^2,3,
PENG Li³

1. CNOOC Shanghai Company, Shanghai, 200335, China;
2. College of Marine Science and Technology, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China;
3. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China;
4. Geological Scientific Research Institute, SINOPEC Shengli Oilfield Branch Company, Dongying, Shandong 257015, China

摘要

摘要: 由于陆相页岩控制因素的多样性与复杂性，使得页岩岩相的精细识别及预测具有一定的难度，同时，页岩岩相发育的控制因素也一直没有明确。通过近年来对渤海湾盆地东营凹陷泥页岩岩相及控制因素的持续研究，总结了不同级次等时地层格架下陆相页岩岩相多尺度精细识别标志与发育特征，提出了2种尺度的控制因素。岩相可分为层耦、层耦组、岩相域和岩相层序4个尺度，其中层耦受古生产力、季风、氧化—还原条件联合控制，层耦组—岩相域—岩相层序受物源、气候、构造联合控制，多种因素叠合造就了陆相页岩岩相的复杂性与多样性。研究成果对于系统刻画中国陆相页岩岩相特征、深入理解不同尺度岩相形成机理具有重要意义。
- 陆相页岩 /
- 等时格架 /
- 岩相 /
- 控制因素 /
- 东营凹陷 /
- 渤海湾盆地
Abstract: At present, due to the diversity and complexity of terrestrial shales, it is difficult to identify and predict the shale facies precisely. At the same time, the controlling factors for shale development are not well understood. The study of shale facies and controlling factors in the Dongying Sag has allowed the identification of features of multi-scale lithofacies in lacustrine shale of different grades, and further identified two controlling factors. Lithofacies can be divided into layer coupling, layer coupling group, lithofacies domain and lithofacies sequence. The layer coupling is controlled jointly by paleoproductivity, monsoon and oxidation-reduction, while the layer coupling group-lithofacies domain-lithofacies sequence are controlled jointly by material source, climate and structure, thus resulting in the complexity and diversity of continental shale lithofacies. The results can be used to systematically understand the multi-scale characterization and research of lacustrine shale lithofacies.
- terrestrial shale /
- isochronous stratigraphic framework /
- lithofacies /
- controlling factors /
- Dongying Sag /
- Bohai Bay Basin

HTML全文

参考文献(32)

[1]	马新华.四川盆地南部页岩气富集规律与规模有效开发探索[J].天然气工业,2018,38(10):1-10. MA Xinhua.Enrichment laws and scale effective development of shale gas in the southern Sichuan Basin[J].Natural Gas Industry,2018,38(10):1-10.
[2]	刘洪林,郭伟,刘德勋,等.海相页岩成岩过程中的自生脆化作用[J].天然气工业,2018,38(5):17-25. LIU Honglin,GUO Wei,LIU Dexun,et al.Authigenic embrittlement of marine shale in the process of diagenesis[J].Natural Gas Industry,2018,38(5):17-25.
[3]	雷丹凤,李熙喆,位云生,等.海相页岩有效产气储层特征:以四川盆地五峰组-龙马溪组页岩为例[J].中国矿业大学学报,2019,48(2):333-343. LEI Danfeng,LI Xizhe,WEI Yunsheng,et al.Characteristics of effective gas-producing reservoir in marine shale:a case study of the Wufeng-Longmaxi shales in Sichuan Basin[J].Journal of China University of Mining & Technology,2019,48(2):333-343.
[4]	JIANG Zaixing,GUO Ling,LIANG Chao.Lithofacies and sedimentary characteristics of the Silurian Longmaxi shale in the southeastern Sichuan Basin,China[J].Journal of Palaeogeography,2013,2(3):238-251.
[5]	TANG Xianglu,JIANG Zaixing,HUANG Hexin,et al.Lithofacies characteristics and its effect on gas storage of the Silurian Longmaxi marine shale in the southeast Sichuan Basin,China[J].Journal of Natural Gas Science and Engineering,2016,28:338-346.
[6]	刘惠民,孙善勇,操应长,等.东营凹陷沙三段下亚段细粒沉积岩岩相特征及其分布模式[J].油气地质与采收率,2017,24(1):1-10. LIU Huimin,SUN Shanyong,CAO Yingchang,et al.Lithofacies characteristics and distribution model of fine-grained sedimentary rock in the lower Es₃ member,Dongying Sag[J].Petroleum Geo-logy and Recovery Efficiency,2017,24(1):1-10.
[7]	ABOUELRESH M O,SLATT R M.Lithofacies and sequence stratigraphy of the Barnett shale in east-central Fort Worth Basin,Texas[J].AAPG Bulletin,2012,96(1):1-22.
[8]	王勇,王学军,宋国奇,等.渤海湾盆地济阳坳陷泥页岩岩相与页岩油富集关系[J].石油勘探与开发,2016,43(5):696-704. WANG Yong,WANG Xuejun,SONG Guoqi,et al.Genetic connection between mud shale lithofacies and shale oil enrichment in Jiyang Depression,Bohai Bay Basin[J].Petroleum Exploration and Development,2016,43(5):696-704.
[9]	刘庆,曾翔,王学军,等.东营凹陷沙河街组沙三下-沙四上亚段泥页岩岩相与沉积环境的响应关系[J].海洋地质与第四纪地质,2017,37(3):147-156. LIU Qing,ZENG Xiang,WANG Xuejun,et al.Lithofacies of mudstone and shale deposits of the Es³z-Es⁴s formation in Dongying Sag and their depositional environment[J].Marine Geology & Quaternary Geology,2017,37(3):147-156.
[10]	马义权,杜学斌,刘惠民,等.东营凹陷沙四上亚段陆相页岩岩相特征、成因及演化[J].地球科学,2017,42(7):1195-1208. MA Yiquan,DU Xuebin,LIU Huimin,et al.Characteristics,depositional processes,and evolution of shale lithofaceis of the upper submember of Es₄ in the Dongying Depression[J].Earth Science,2017,42(7):1195-1208.
[11]	WANG Pengfei,JIANG Zhenxue,YIN Lishi,et al.Lithofacies classification and its effect on pore structure of the Cambrian marine shale in the Upper Yangtze Platform,South China:evidence from FE-SEM and gas adsorption analysis[J].Journal of Petroleum Science and Engineering,2017,156:307-321.
[12]	YAN Jianping,HE Xu,HU Qinhong,et al.Lower Es₃ in Zhanhua Sag,Jiyang Depression:a case study for lithofacies classification in lacustrine mud shale[J].Applied Geophysics,2018,15(2):151-164.
[13]	陈少伟,刘伟,梁康.页岩气成藏富集主控因素研究[J].中国石油和化工标准与质量,2017,37(16):104-105. CHEN Shaowei,LIU Wei,LIANG Kang.Study on main controlling factors of shale gas accumulation and enrichment[J].China Petroleum and Chemical Standard and Quality,2017,37(16):104-105.
[14]	王超,张柏桥,陆永潮,等.焦石坝地区五峰组-龙马溪组一段页岩岩相展布特征及发育主控因素[J].石油学报,2018,39(6):631-644. WANG Chao,ZHANG Baiqiao,LU Yongchao,et al.Lithofacies distribution characteristics and main development controlling factors of shale in Wufeng Formation-Member 1 of Longmaxi Formation in Jiaoshiba area[J].Acta Petrolei Sinica,2018,39(6):631-644.
[15]	贾承造,邹才能,杨智,等.陆相油气地质理论在中国中西部盆地的重大进展[J].石油勘探与开发,2018,45(4):546-560. JIA Chengzao,ZOU Caineng,YANG Zhi,et al.Significant progress of continental petroleum geology theory in basins of Central and Western China[J].Petroleum Exploration and Development,2018,45(4):546-560.
[16]	KONG Xianxin,JIANG Zaixing,HAN Chao,et al.Sedimentary characteristics and depositional models of two types of homoge-nites in an Eocene continental lake basin,Shulu Sag,Eastern China[J].Journal of Asian Earth Sciences,2019,179:165-188.
[17]	朱红涛,刘可禹,朱筱敏,等.陆相盆地层序构型多元化体系[J].地球科学,2018,43(3):770-785. ZHU Hongtao,LIU Keyu,ZHU Xiaomin,et al.Varieties of sequence stratigraphic configurations in continental basins[J].Earth Science,2018,43(3):770-785.
[18]	谭先锋,王萍,王佳,等.早始新世极热气候时期咸化湖盆混合沉积作用:以渤海湾盆地东营凹陷孔店组为例[J].石油与天然气地质,2018,39(2):340-354. TAN Xianfeng,WANG Ping,WANG Jia,et al.Mixed sedimentation in saline lacustrine basins during initial Eocene thermal maximum period:a case study on Kongdian Formation in Dong-ying Sag,Bohai Bay Basin[J].Oil & Gas Geology,2018,39(2):340-354.
[19]	ZHAO Ke,DU Xuebin,LU Yongchao,et al.Are light-dark coupled laminae in lacustrine shale seasonally controlled? a case study using astronomical tuning from 42.2 to 45.4 Ma in the Dongying Depression,Bohai Bay Basin,Eastern China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2019,528:35-49.
[20]	李彦泽,王志坤,商琳,等.小湖盆浅水三角洲沉积特征及其等时格架划分方案:以南堡4-3区东二段为例[J].沉积学报,2019.DOI:10.14027/j.issn.1000-0550.2019.017. LI Yanze,WANG Zhikun,SHANG Lin,et al.Study on sedimentary characteristics of shallow-water deltas and isochronous straigraphic framework:an example of Ed₂ of 4-3 zone of Nanpu oil field[J].Acta Sedimentologica Sinica,2019.DOI:10.14027/j.issn.1000-0550.2019.017.
[21]	MA Yiquan,FAN Majie,LU Yongchao,et al.Climate-driven paleo-limnological change controls lacustrine mudstone depositional process and organic matter accumulation:constraints from lithofacies and geochemical studies in the Zhanhua Depression,Eastern China[J].International Journal of Coal Geology,2016,167:103-118.
[22]	杜学斌,陆永潮,刘惠民,等.细粒沉积物中不同级次高频层序划分及其地质意义:以东营凹陷沙三下-沙四上亚段泥页岩为例[J].石油实验地质,2018,40(2):244-252. DU Xuebin,LU Yongchao,LIU Huimin,et al.Division of high-frequency sequences of different orders in fine-grained deposits and its geologic significance:a case study of mud shale from the lower section of the third member to the upper section of the fourth member of Shahejie Formation in Dongying Sag,Bohai Bay Basin[J].Petroleum Geology & Experiment,2018,40(2):244-252.
[23]	刘津.陆相层序地层学的研究现状与发展趋势[J].长江大学学报(自然科学版),2013,10(32):55-58. LIU Jin.Research status and development trend of continental sequence stratigraphy[J].Journal of Yangtze University (Natural Science Edition),2013,10(32):55-58.
[24]	吴孔友,秦磊,谭明友,等.构造对东营凹陷深层砂体发育的控制作用[J].沉积学报,2014,32(5):893-900. WU Kongyou,QIN Lei,TAN Mingyou,et al.Research on structures controlling the development of deep sand bodies in Dong-ying Depression[J].Acta Sedimentologica Sinica,2014,32(5):893-900.
[25]	陈树光.东营凹陷古近纪构造体制转换及其动力学背景分析[D].武汉:中国地质大学,2015. CHEN Shuguang.Paleogene structure systems transformation and its analysis of dynamic background,Dongying Sag[D].Wuhan:China University of Geosciences,2015.
[26]	王苗,陆建林,左宗鑫,等.纹层状细粒沉积岩特征及主控因素分析:以渤海湾盆地东营凹陷沙四上-沙三下亚段为例[J].石油实验地质,2018,40(4):470-478. WANG Miao,LU Jianlin,ZUO Zongxin,et al.Characteristics and dominating factors of lamellar fine-grained sedimentary rocks:a case study of the upper Es₄ member-lower Es₃ member,Dongying Sag,Bohai Bay Basin[J].Petroleum Geology & Experiment,2018,40(4):470-478.
[27]	杨万芹,王学军,蒋有录,等.湖泊古气候的量化恢复及其对细粒沉积的影响:以东营凹陷沙四段上亚段-沙三段下亚段为例[J].油气地质与采收率,2018,25(2):29-36. YANG Wanqin,WANG Xuejun,JIANG Youlu,et al.Quantitative reconstruction of paleoclimate and its effects on fine-grained lacustrine sediments:a case study of the upper Es₄ and lower Es₃ in Dongying Sag[J].Petroleum Geology and Recovery Efficiency,2018,25(2):29-36.
[28]	MA Yiquan,FAN Majie,LU Yongchao,et al.Middle Eocene paleohydrology of the Dongying Depression in Eastern China from sedi-mentological and geochemical signatures of lacustrine mudstone[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2017,479:16-33.
[29]	ZACHOS J C,SHACKLETON N J,PEVENAUGH J S,et al.Climate response to orbital forcing across the Oligocene-Miocene boundary[J].Science,2001,292:274-278.
[30]	ZACHOS J C,PAGANI M,SLOAN L, et al.Trends,rhythms,and aberrations in global climate 65 Ma to present[J].Science,2001,292:686-693.
[31]	ZACHOS J C,DICKENS G R,ZEEBE R E.An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics[J].Nature,2008,451:279-283.
[32]	MA Yiquan,FAN Majie,LU Yongchao,et al.Stable isotope record of Middle Eocene summer monsoon and its instability in Eastern China[J].Global and Planetary Change,2019,175:103-112.