东营凹陷沙河街组四段上亚段细粒沉积岩岩相特征及与沉积环境的关系

doi:10.7623/syxb201710002

石油学报 ›› 2017, Vol. 38 ›› Issue (10): 1110-1122.DOI: 10.7623/syxb201710002

东营凹陷沙河街组四段上亚段细粒沉积岩岩相特征及与沉积环境的关系

吴靖^1,2, 姜在兴³, 梁超⁴

1. 中国石油化工股份有限公司石油勘探开发研究院北京 100083;
2. 中国石油化工集团公司页岩油气勘探开发重点实验室北京 100083;
3. 中国地质大学能源学院北京 100083;
4. 中国石油大学地球科学与技术学院山东青岛 266580

收稿日期:2017-03-20 修回日期:2017-07-28 出版日期:2017-10-25 发布日期:2017-11-02
通讯作者: 吴靖,女,1988年6月生,2010年获中国地质大学(武汉)资源学院学士学位,2015年获中国地质大学(北京)能源学院博士学位,现为中国石油化工股份有限公司石油勘探开发研究院高级工程师,主要从事沉积学研究.Email:wujing6524982@163.com
作者简介:吴靖,女,1988年6月生,2010年获中国地质大学(武汉)资源学院学士学位,2015年获中国地质大学(北京)能源学院博士学位,现为中国石油化工股份有限公司石油勘探开发研究院高级工程师,主要从事沉积学研究.Email:wujing6524982@163.com
基金资助:
国家自然科学基金项目（No.41602142）、国家重大科技专项（2016ZX05036-004-001）、中国博士后基金项目（No.2017T100523，2015M582465）、山东省自然科学基金项目（ZR2016DB16）及中国石油化工股份有限公司科技攻关项目（P16043）资助。

Lithofacies characteristics of fine-grained sedimentary rocks in the upper submember of Member 4 of Shahejie Formation,Dongying sag and their relationship with sedimentary environment

Wu Jing^1,2, Jiang Zaixing³, Liang Chao⁴

1. Sinopec Petroleum Exploration and Production Research Institute, Beijing 100083, China;
2. Sinopec Key Laboratory of Shale Gas/Oil Exploration & Production, Beijing 100083, China;
3. Faculty of Energy Resources, China University of Geosciences, Beijing 100083, China;
4. School of Geosciences, China University of Petroleum, Shandong Qingdao 266580, China

Received:2017-03-20 Revised:2017-07-28 Online:2017-10-25 Published:2017-11-02

摘要/Abstract

摘要：

细粒沉积岩的岩相特征影响泥页岩的生烃能力与储集性能，与沉积环境的相互关系分析亦可丰富细粒沉积的研究。然而目前针对陆相细粒沉积岩岩相的研究较为薄弱，基于岩相成因，与沉积环境相结合的岩相特征分析较少。基于大量岩心、薄片、X射线衍射及地球化学数据，以成分为第一要素，以东营凹陷沙河街组四段上亚段细粒沉积岩为例，划分出4大类、12种岩相类型，分析每一种岩相的宏观、微观、成分及成因特征。通过矿物成分、地球化学等多参数的分析发现，沙河街组四段上亚段沉积环境分为4个阶段。沉积环境通过控制岩相主要成分而控制了岩相的类别与发育；沉积环境的旋回性与阶段性变化导致岩相的旋回性与阶段性变化；沉积环境控制岩相发育，岩相亦能反应沉积环境的变化。在细粒沉积分析中，不能排除突发事件（海侵、浊流等）对岩相及沉积环境的影响。

关键词: 细粒沉积岩, 岩相特征, 沉积环境, 东营凹陷, 沙河街组四段上亚段

Abstract:

Lithofacies characteristics of fine-grained sedimentary rocks (FGSR)have impact on the hydrocarbon generation ability and reserving property of shale, and their relationship with sedimentary environment can be analyzed to enrich the research on fine-grained sediment.However, there are insufficient studies regarding the lithofacies of lacustrine FGSR. The lithofacies characteristics are less analyzed based on lithofacies genesis in combination with sedimentary environment. Accordingly, based on massive well cores, thin sections, X-ray diffraction and geochemical data, and the component as the first element, FGSR in the upper submember of Member 4 of Shahejie Formation in Dongying sag was divided into four categories and 12 lithofacies types, so as to analyze the macro, micro, component and genesis characteristics of each lithofacies type. Through analyzing mineral compositions, geochemical indexes and other parameters, it is found that the sedimentary environment in the upper submember of Member 4 of Shahejie Formation can be classified into four stages.The sedimentary environment controls the types and development of lithofacies through controlling the main components of lithofacies;the cyclicity and periodic changes of lithofacies are caused by those in sedimentary environment; the sedimentary environment controls the lithofacies development, and the lithofacies reflects the change of sedimentary environment. During the FGSR analysis, the influences of sudden events (such as transgression and turbidity flow)on lithofacies and sedimentary environment cannot be excluded.

Key words: fine-grained sedimentary rocks, lithofacies characteristics, sedimentary environment, Dongying sag, the upper submember of Member 4 of Shahejie Formation

中图分类号:

TE121

吴靖, 姜在兴, 梁超. 东营凹陷沙河街组四段上亚段细粒沉积岩岩相特征及与沉积环境的关系[J]. 石油学报, 2017, 38(10): 1110-1122.

Wu Jing, Jiang Zaixing, Liang Chao. Lithofacies characteristics of fine-grained sedimentary rocks in the upper submember of Member 4 of Shahejie Formation,Dongying sag and their relationship with sedimentary environment[J]. Acta Petrolei Sinica, 2017, 38(10): 1110-1122.

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东营凹陷沙河街组四段上亚段细粒沉积岩岩相特征及与沉积环境的关系

Lithofacies characteristics of fine-grained sedimentary rocks in the upper submember of Member 4 of Shahejie Formation,Dongying sag and their relationship with sedimentary environment

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