泥页岩沉积特征与生烃能力——以东营凹陷沙河街组三段中亚段-沙河街组四段上亚段为例

doi:10.7623/syxb201701004

石油学报 ›› 2017, Vol. 38 ›› Issue (1): 31-43.DOI: 10.7623/syxb201701004

泥页岩沉积特征与生烃能力——以东营凹陷沙河街组三段中亚段-沙河街组四段上亚段为例

曾翔¹, 蔡进功¹, 董哲^1,2, 王学军³, 郝运轻³

1. 同济大学海洋地质国家重点实验室上海 200092;
2. 中海石油(中国)有限公司上海分公司上海 200335;
3. 中国石油化工股份有限公司胜利油田分公司勘探开发研究院山东东营 257015

收稿日期:2016-05-19 修回日期:2016-09-23 出版日期:2017-01-25 发布日期:2017-01-23
通讯作者: 蔡进功,男,1961年12月生,1983年获南京大学学士学位,2003年获同济大学博士学位,现为同济大学教授、博士生导师,主要从事海洋沉积学和石油地质学方面的科研和教学工作。Email:jgcai@tongji.edu.cn
作者简介:曾翔,男,1987年10月生,2010年获西安石油大学学士学位,2013年获中国石油大学(华东)硕士学位,现为同济大学博士研究生,主要从事细颗粒沉积学和石油地质学研究。Email:2013zengxiang@tongji.edu.cn
基金资助:
国家自然科学基金项目（No.41372130，No.41672115）和国家重大科技专项（2016ZX05006-001-003）资助。

Sedimentary characteristics and hydrocarbon generation potential of mudstone and shale: a case study of Middle Submember of Member 3 and Upper Submember of Member 4 in Shahejie Formation in Dongying sag

Zeng Xiang¹, Cai Jingong¹, Dong Zhe^1,2, Wang Xuejun³, Hao Yunqing³

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;
2. Shanghai Branch, CNOOC China Limited, Shanghai 200335, China;
3. Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong Dongying 257015, China

Received:2016-05-19 Revised:2016-09-23 Online:2017-01-25 Published:2017-01-23

摘要/Abstract

摘要：

泥页岩的沉积环境与形成方式都将控制其矿物、有机质特征并影响岩石的生烃潜力。选取东营凹陷古近系沙河街组泥页岩，开展岩石薄片观察、X射线衍射和热解等检测，研究岩石的矿物学特征和有机质特征，解析各类泥页岩成因与生烃能力的差异。研究发现，研究区的块状、纹层状和含石膏构造泥页岩中构造特征各异，矿物成分（碎屑、黏土、碳酸盐矿物和石膏类矿物等）含量变化大，有机质特征也各不相同。综合分析矿物与有机质的特征及组合关系，发现细纹层页岩和断续纹层页岩是以生物作用为主导形成的沉积产物，生烃能力最强；宽纹层页岩和均匀块状泥岩属化学沉积作用的产物，具有较强的生烃能力；含碎屑块状泥岩主要通过机械作用沉积而成，含石膏构造泥岩则在蒸发环境下通过化学沉淀形成，两者的生烃能力较弱。比较东营凹陷沙河街组三段中亚段-沙河街组四段上亚段的泥页岩类型，发现沙河街组三段中亚段和沙河街组四段纯下次亚段以机械和化学作用形成的含碎屑块状和含石膏构造泥岩为主，导致2个层段的生烃能力较弱；沙河街组三段下亚段和沙河街组四段纯上次亚段以生物或化学沉积作用形成的纹层状页岩为主，导致2个层段的生烃能力较强。因此，关注泥页岩矿物和有机质组合关系，从机械、化学和生物等沉积方式差异的角度探讨各类泥页岩的成因和生烃能力的变化，能够为非常规油气勘探提供新的思路。

关键词: 泥页岩, 沉积特征, 生烃能力, 沙河街组, 东营凹陷

Abstract:

Sedimentary environment and formation mode of mudstone and shale are able to control its mineral and organic matter characteristics as well as influence the hydrocarbon generation potential of rocks. The Paleogene mudstone and shale in Shanghejie Formation, Dongying sag was selected to carry out rock thin-section observation, X-ray diffusion, thermal decomposition and other detection methods, so as to study the mineral and organic matter characteristics of rocks as well as analyze the differences in genesis and hydrocarbon generation potential of various mudstone and shales. Results show that massive, layered and gypsum-bearing mudstone and shale have diversified laminated characteristics in the study area, where the content of mineral components (including clastics, clay, carbonate and gypsum minerals) show great changes and organic matter characteristics have also been diversified. Through comprehensive analysis on mineral and organic matter characteristics as well as their assemblage relationships, it was found that the fine-laminated shale and discontinuously-laminated shale were the products mainly formed by biological deposition with the highest hydrocarbon generation potential. The wide-laminated shale and homogenous-massive mudstone were the products of chemical deposition with higher hydrocarbon generation potential. The clastic-massive mudstone was mainly formed by mechanic deposition, while the gypsum-bearing mudstone was generated by chemical deposition in an evaporitic environment, and both showed weaker hydrocarbon generation potential. Comparing the mudstone and shale types in the Middle Submember of Member 3 and the Upper Submember of Member 4 of Shahejie Formation, Dongying sag, it was detected that the Middle Submember of Member 3 and Chunxia Submember of Member 4 were dominated by clastic-massive and gypsum-bearing mudstone and shale formed due to mechanic and chemical effect, leading to weaker hydrocarbon generation potential. The Lower Submember of Member 3 and Chunshang Submember of Member 4 of Shahejie Formation, Dongying sag were dominated by laminated mudstone and shale formed due to biological or chemical deposition, leading to higher hydrocarbon generation potential. Therefore, the focus on mineral-organic matter assemblage relationships of mudstone and shale as well as the changes in the genesis and hydrocarbon generation potential of various mudstone and shales from the perspectives of mechanic, chemical and biological deposition modes is able to provide a new idea for unconventional hydrocarbon exploration.

Key words: mudstone and shale, sedimentary characteristics, hydrocarbon generation potential, Shahejie Formation, Dongying sag

中图分类号:

TE122.1

曾翔, 蔡进功, 董哲, 王学军, 郝运轻. 泥页岩沉积特征与生烃能力——以东营凹陷沙河街组三段中亚段-沙河街组四段上亚段为例[J]. 石油学报, 2017, 38(1): 31-43.

Zeng Xiang, Cai Jingong, Dong Zhe, Wang Xuejun, Hao Yunqing. Sedimentary characteristics and hydrocarbon generation potential of mudstone and shale: a case study of Middle Submember of Member 3 and Upper Submember of Member 4 in Shahejie Formation in Dongying sag[J]. Acta Petrolei Sinica, 2017, 38(1): 31-43.

参考文献

[1] BLATT H,TRACY R J.Petrology:igneous,sedimentary and metamorphic[M].2nd ed.San Francisco:Freeman,1996:281-292.
[2] YOUNGQUIST W.SHALE oil-The elusive energy[R].Hubbert Center Newsletter # 98/4,1998.
[3] 张林晔,李政,朱日房,等.济阳坳陷古近系存在页岩气资源的可能性[J].天然气工业,2008,28(12):26-29.
ZHANG Linye,LI Zheng,ZHU Rifang,et al.Resource potential of shale gas in Paleogene in Jiyang depression[J].Natural Gas Industry,2008,28(12):26-29.
[4] 张林晔,孔祥星,张春荣,等.济阳坳陷下第三系优质烃源岩的发育及其意义[J].地球化学,2003,32(1):35-42.
ZHANG Linye,KONG Xiangxing,ZHANG Chunrong,et al.High-quality oil-prone source rocks in Jiyang depression[J].Geochimica,2003,32(1):35-42.
[5] 张林晔.湖相烃源岩研究进展[J].石油实验地质,2008,30(6):591-595.
ZHANG Linye.The progress on the study of lacustrine source rocks[J].Petroleum Geology & Experiment, 2008,30(6):591-595.
[6] 党伟,张金川,黄潇,等.陆相页岩含气性主控地质因素——以辽河西部凹陷沙河街组三段为例[J].石油学报,2015,36(12):1516-1530.
DANG Wei,ZHANG Jinchuan,HUANG Xiao,et al.Main-controlling geological factors of gas-bearing property of continental shale gas:a case study of Member 3rd of Shahejie Formation in western Liaohe sag[J].Acta Petrolei Sinica, 2015,36(12):1516-1530.
[7] 朱光有,金强,张水昌,等.济阳坳陷东营凹陷古近系沙河街组深湖相油页岩的特征及成因[J].古地理学报,2005,7(1):59-69.
ZHU Guangyou,JIN Qiang,ZHANG Shuichang,et al.Characteristics and origin of deep lake oil shale of the Shahejie Formation of Paleogene in Dongying sag,Jiyang depression[J].Journal of Palaeogeography,2005,7(1):59-69.
[8] 朱光有,金强,周建林.东营凹陷旋回式深湖相烃源岩研究[J].地质科学,2003,38(2):254-262.
ZHU Guangyou,JIN Qiang,ZHOU Jianlin.Source rock characters of cyclic deep-lake facies in the Dongying depression[J].Chinese Journal of Geology,2003,38(2):254-262.
[9] 姜福杰,庞雄奇,姜振学,等.东营凹陷沙四上亚段烃源岩排烃特征及潜力评价[J].地质科技情报,2007,26(2):69-74.
JIANG Fujie,PANG Xiongqi,JIANG Zhenxue,et al.Hydrocarbon-expulsion characters and the potential resource evaluation of hydrocarbon source rocks from the upper section of 4th Member of Shahejie Formation in Dongying depression[J].Geological Science and Technology Information,2007,26(2):69-74.
[10] 蔡希源.湖相烃源岩生排烃机制及生排烃效率差异性——以渤海湾盆地东营凹陷为例[J].石油与天然气地质,2012,33(3):329-334.
CAI Xiyuan.Hydrocarbon generation-expulsion mechanisms and efficiencies of lacustrine source rocks:a case study from the Dongying sag,Bohai Bay Basin[J].Oil & Gas Geology,2012,33(3):329-334.
[11] SEVILLE J P K,WILLETT C D,KNIGHT P C.Interparticle forces in fluidisation:a review[J]. Powder Technology,2000,113(3):261-268.
[12] BENNETT R H,BRYANT W R,HULBERT M H,et al.Microstructure of fine-grained sediments:from mud to shale[M].New York:Springer,2012:123-229.
[13] 张顺,陈世悦,鄢继华,等.东营凹陷西部沙三下亚段——沙四上亚段泥页岩岩相及储层特征[J].天然气地球科学,2015,26(2):320-332.
ZHANG Shun,CHEN Shiyue,YAN Jihua,et al.Characteristics of shale lithofacies and reservoir space in the 3rd and 4th members of Shahejie Formation,the west of Dongying sag[J].Natural Gas Geoscience,2015,26(2):320-332.
[14] 刘传联,舒小辛,刘志伟.济阳坳陷下第三系湖相生油岩的微观特征[J].沉积学报,2001,19(2):293-298.
LIU Chuanlian,SHU Xiaoxin,LIU Zhiwei.Micro-characteristics of Paleogene lacustrine petroleum source rocks in Jiyang depression[J].Acta Sedimentologica Sinica,2001,19(2):293-298.
[15] LIU Chuanlian,WANG Pinxian.The role of algal blooms in the formation of lacustrine petroleum source rocks-evidence from Jiyang depression,Bohai Gulf Rift Basin,eastern China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2013,388:15-22.
[16] 姜在兴,张文昭,梁超,等.页岩油储层基本特征及评价要素[J].石油学报,2014,35(1):184-196.
JIANG Zaixing,ZHANG Wenzhao,LIANG Chao,et al.Characteristics and evaluation elements of shale oil reservoir[J].Acta Petrolei Sinica,2014,35(1):184-196.
[17] 张海峰,刘庆,张林晔,等.山东东营凹陷古近系沙河街组湖盆演化及烃源岩赋存相带[J].古地理学报,2005,7(3):383-397.
ZHANG Haifeng,LIU Qing,ZHANG Linye,et al.Lacustrine basin evolution and favorable sedimentary facies belt for source rocks abounding in the Shahejie Formation of Paleogene in Dongying sag,Shandong province[J].Journal of Palaeogeography,2005,7(3):383-397.
[18] 杨田,操应长,王艳忠,等.深水重力流类型、沉积特征及成因机制——以济阳坳陷沙河街组三段中亚段为例[J].石油学报,2015,36(9):1048-1059.
YANG Tian,CAO Yingchang,WANG Yanzhong,et al.Types,sedimentary characteristics and genetic mechanisms of deep-water gravity flows:a case study of the middle submember in Member 3 of Shahejie Formation in Jiyang depression[J].Acta Petrolei Sinica,2015,36(9):1048-1059.
[19] 石油地质勘探专业标准化委员会.SY/T 5163-2010沉积岩中黏土矿物和常见非黏土矿物X射线衍射分析方法[S].北京:石油工业出版社,2010.
Standardization Committee of Petroleum Geological Exploration.SY/T 5163-2010 Analysis method for clay minerals and ordinary non-clay minerals in sedimentary rocks by the X-ray diffraction[S].Beijing:Petroleum Industry Press,2010.
[20] 石油地质勘探专业标准化委员会.GB/T 18602-2001岩石热解分析[S].北京:中国标准出版社,2001.
Standardization Committee of Petroleum Geological Exploration.GB/T 18602-2001 Rock pyrolysis analysis[S].Beijing:China Standard Press,2001.
[21] SCHIEBER J,BOSE P K,ERIKSSON P,et al.Atlas of microbial mat features preserved within the siliciclastic rock record[M].Amsterdam:Elsevier,2007:117-262.
[22] GERDES G.Structures left by modern microbial mats in their host sediments[M]//SCHIEBER J,BOSE P K,ERIKSSON P G,et al.Atlas of Microbial Mat Features Preserved within the Clastic Rock Record.Amsterdam:Elsevier,2007.
[23] 梅冥相.微生物席的特征和属性:微生物席沉积学的理论基础[J].古地理学报,2014,16(3):285-304.
MEI Mingxiang.Feature and nature of microbial-mat:theoretical basis of microbial-mat sedimentology[J].Journal of Palaeogeography,2014,16(3):285-304.
[24] 王冠民,任拥军,钟建华,等.济阳坳陷古近系黑色页岩中纹层状方解石脉的成因探讨[J].地质学报,2005,79(6):834-838.
WANG Guanmin,REN Yongjun,ZHONG Jianhua,et al.Genetic analysis on lamellar calcite veins in Paleogene black shale of the Jiyang depression[J].Acta Geologica Sinica, 2005,79(6):834-838.
[25] WEAVER C E.Clays,muds,and shales[M].New York:Elsevier,1989:60-205.
[26] POTTER P E,MAYNARD J B,DEPETRIS P J.Mud and mudstones:introduction and overview[M].Berlin Heidelberg:Springer,2005:10-53.
[27] SCHIEBER J,SOUTHARD J B,SCHIMMELMANN A.Lenticular shale fabrics resulting from intermittent erosion of water-rich muds-interpreting the rock record in the light of recent flume experiments[J].Journal of Sedimentary Research,2010,80(1):119-128.
[28] TURNER J T.Zooplankton fecal pellets,marine snow,phytodetritus and the ocean's biological pump[J].Progress in Oceanography,2015,130:205-248.
[29] TURNER J T.Zooplankton fecal pellets,marine snow and sinking phytoplankton blooms[J].Aquatic Microbial Ecology,2002,27(1):57-102.
[30] 刘传联,徐金鲤,汪品先.藻类勃发——湖相油源岩形成的一种重要机制[J].地质论评,2001,47(2):207-210.
LIU Chuanlian,XU Jinli,WANG Pinxian.Algal blooms:the primary mechanism in the formation of lacustrine petroleum source rocks[J].Geological Review,2001,47(2):207-210.
[31] 冯增昭.碳酸盐岩岩相古地理学[M].北京:石油工业出版社,1989:84-90.
FENG Zengzhao.Lithofacies paleogeography of carbonate rocks[M].Beijing:Petroleum Industry Press,1989:84-90.
[32] FlÜGEL E.MICROFACIES of carbonate rocks:analysis,interpretation and application[M].Berlin Heidelberg:Springer-Verlag,2010:101-203.
[33] SCHOLLE P A,ULMER-Scholle D S.A color guide to the petrography of carbonate rocks:grains,textures,porosity,diagenesis[M].AAPG Memoir 77.Tulsa,OK:The American Association of Petroleum Geologists,2003:316-430.
[34] 熊毅.土壤胶体[M].北京:科学出版社,1983:62-68.
XIONG Yi.Soil colloid:Material basis of soil colloid[M].Beijing:Science Press,1983:62-68.
[35] STOW D A,PIPER D J W.Fine-grained sediments:deep-water processes and facies[M].Oxford:Geological Society, Special Publications,1984:110-223.
[36] 蔡进功.泥质沉积物和泥岩中有机黏土复合体[M].北京:科学出版社,2004:5-130.
CAI Jingong.Organo-clay complexes in muddy sediments and mudstones[M].Beijing:Science Press,2004:5-130.
[37] PAMUKCU S,TUNCAN M.Influence of some physicochemical activities on mechanical behavior of clays[M]//BENNETT R H,BRYANT W R,HULBERT M H,et al.Microstructure of Fine-Grained Sediments.New York:Springer,1991:241-253.
[38] 孙致安,卢寿慈.钙、镁离子对石英、赤铁矿凝聚与絮凝的作用[J].矿冶工程,1992,12(2):19-22.
SUN Zhi'an,LU Shouci.Effect of calcium and magnesium ions on aggregation and floculation of quartz and hematite[J].Mining and Metallurgical Engineering,1992,12(2):19-22.
[39] Homewood P.Fine-grained turbidite systems[J].Basin Research, 2001,13(3):377.
[40] 蒋有录,查明.石油天然气地质与勘探[M].北京:石油工业出版社,2006:43-95.
JIANG Youlu,ZHA Ming.Geology and exploration of oil and gas[M].Beijing:Petroleum Industry Press,2006:43-95.
[41] TYSON R.Sedimentary organic matter:organic facies and palynofacies[M]. Netherlands:Springer,1995:50-250.
[42] PETERS K E,CASSA M R.Applied source-rock geochemistry[M]//MAGOON L B,DOW W G.The Petroleum System.From Source to Trap.Tulsa:American Association of Petroleum Geologists,1994.
[43] VANDENBROUCKE M,LARGEAU C.Kerogen origin,evolution and structure[J]. Organic Geochemistry,2007,38(5):719-833.
[44] BJORLYKKE K.Petroleum geoscience:from sedimentary environments to rock physics[M].Berlin Heidelberg:Springer,2010:31-118.
[45] PETERS K.Guidelines for evaluating petroleum source rock using programmed pyrolysis[J].AAPG Bulletin,1986,70(3):318-329.
[46] 陈中红,查明,金强.东营凹陷古近系中深层湖盆演化中的无机元素响应[J].沉积学报,2008,26(6):925-932.
CHEN Zhonghong,ZHA Ming,JIN Qiang.Mineral elemental response to the evolution of terrestrial brine faulted-basin:a case study in the Paleogene of Well Haoke-1,Dongying sag[J].Acta Sedimentologica Sinica,2008,26(6):925-932.
[47] 陈中红,查明,刘太勋.东营凹陷古近系古湖盆演化与水化学场响应[J].湖泊科学,2008,20(6):705-714.
CHEN Zhonghong,ZHA Ming,LIU Taixun.Response and evolution of formation water chemical fields of the paleogene in Dongying sag[J].Journal of Lake Scienc es,2008,20(6):705-714.
[48] 李文俊.东营凹陷南坡沙河街组沙四段-沙三下亚段沉积体系研究[D].青岛:中国石油大学(华东),2012:5-92.
LI Wenjun.The sedimentary system of Es₄-Es₃^x member of Shahejie Formation on the southern slope of Dongying sag[D].Qingdao:China University of Petroleum (East China),2012:5-92.
[49] 周祺盛.烃源岩有机质赋存与热解参数关系研究[D].上海:同济大学,2015:35-83.
ZHOU Qisheng.Study on the relationship of occurrence of organic matter and pyrolysis parameters in source rocks[D].Shanghai:Tongji University,2015:35-83.

泥页岩沉积特征与生烃能力——以东营凹陷沙河街组三段中亚段-沙河街组四段上亚段为例

Sedimentary characteristics and hydrocarbon generation potential of mudstone and shale: a case study of Middle Submember of Member 3 and Upper Submember of Member 4 in Shahejie Formation in Dongying sag

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[10]	赵贤正, 周立宏, 蒲秀刚, 时战楠, 韩国猛, 吴佳朋, 韩文中, 张伟, 高欢欢, 马建英, 汪虎. 歧口凹陷歧北次凹沙河街组三段页岩油地质特征与勘探突破[J]. 石油学报, 2020, 41(6): 643-657.
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[14]	杜学斌, 刘晓峰, 陆永潮, 刘惠民, 张守鹏, 马义权, 赵珂, 魏巍. 陆相细粒混合沉积分类、特征及发育模式——以东营凹陷为例[J]. 石油学报, 2020, 41(11): 1324-1333.
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