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    珠江口盆地惠州凹陷恩平组“扇-辫”复合体发育规律及有利储层主控因素

    彭光荣 刘培 宋朋霖 高翔 熊万林 向巧维 韩博

    彭光荣, 刘培, 宋朋霖, 高翔, 熊万林, 向巧维, 韩博, 2025. 珠江口盆地惠州凹陷恩平组“扇-辫”复合体发育规律及有利储层主控因素. 地球科学, 50(8): 3199-3212. doi: 10.3799/dqkx.2023.190
    引用本文: 彭光荣, 刘培, 宋朋霖, 高翔, 熊万林, 向巧维, 韩博, 2025. 珠江口盆地惠州凹陷恩平组“扇-辫”复合体发育规律及有利储层主控因素. 地球科学, 50(8): 3199-3212. doi: 10.3799/dqkx.2023.190
    Peng Guangrong, Liu Pei, Song Penglin, Gao Xiang, Xiong Wanlin, Xiang Qiaowei, Han Bo, 2025. Characteristics of the 'Fan-Braid' Complex and Main Controlling Factors of Favorable Reservoir in the Enping Formation, Huizhou 26 Sag, Pearl River Mouth Basin. Earth Science, 50(8): 3199-3212. doi: 10.3799/dqkx.2023.190
    Citation: Peng Guangrong, Liu Pei, Song Penglin, Gao Xiang, Xiong Wanlin, Xiang Qiaowei, Han Bo, 2025. Characteristics of the "Fan-Braid" Complex and Main Controlling Factors of Favorable Reservoir in the Enping Formation, Huizhou 26 Sag, Pearl River Mouth Basin. Earth Science, 50(8): 3199-3212. doi: 10.3799/dqkx.2023.190

    珠江口盆地惠州凹陷恩平组“扇-辫”复合体发育规律及有利储层主控因素

    doi: 10.3799/dqkx.2023.190
    基金项目: 

    中国海洋石油有限公司“十四五”科技重大项目“陆缘裂谷盆地深层/超深层油气成藏条件与成藏机制研究——珠江口盆地珠一坳陷” KJGG2022-0403

    中国海洋石油有限公司科研项目“惠州19构造带三角洲-滩坝复合沉积形成机制及展布规律” SCKY-2024-YJYKT-01

    中国海洋石油有限公司三年基础地质研究项目“高温背景下不同流体环境“岩-流”相互作用研究” SCKY-2024-SZ-YJYKT12

    中国海洋石油有限公司科研项目“珠江口盆地浅水区陡坡砂砾岩带油气富集规律及勘探方向” KJZH-2024-2106

    详细信息
      作者简介:

      彭光荣(1978-),男,高级工程师,主要从事油气地质与油气勘探综合研究工作. ORCID: 0009-0009-1437-5878. E-mail: penggr@cnooc.com.cn

    • 中图分类号: P624

    Characteristics of the "Fan-Braid" Complex and Main Controlling Factors of Favorable Reservoir in the Enping Formation, Huizhou 26 Sag, Pearl River Mouth Basin

    • 摘要: 珠江口盆地惠州凹陷惠州26洼恩平组发育“扇三角洲-辫状河三角洲”复合沉积体系,并在不同构造的不同沉积演化阶段均发生了典型的“扇-辫”体系转换,转换前后的储层物性条件差异较大,亟需开展深入研究.基于三维地震资料以及岩心分析资料,综合分析了惠州26洼恩平组“扇-辫”复合体系储层差异展布特征及其主控因素,并明确了该区域“南扇北辫、早扇晚辫”的扇-辫演化关系;同时,深入揭示了“优相-改造-火山”为该复合体系有利储层发育的三大主控因素,其中:优质沉积相带是有利储层发育的物质基础,多级断阶搬运改造以及古隆背景下的湖浪淘洗是改善储层物性的关键,而火山物质差异化成岩演化对储层物性起着调控作用.相对而言,惠州26洼恩平组辫状河三角洲相储层物性整体较好,但仍需在埋深下限之上寻找受火山物质影响小的有利储层发育区带;而扇三角洲前缘亚相,还需加强对改造作用的研究并优选强改造作用下的储层.

       

    • 图  1  惠州凹陷区域位置及综合地层柱状图(a),惠州26洼恩平组二段沉积古地貌图(b)

      Fig.  1.  Location and Comprehensive Stratigraphic Histogram of Huizhou Depression (a), Sedimentary Paleogeomorphology Map of the Second Member of Enping Formation in Huizhou 26 Depression (b)

      图  2  惠州26洼恩平组区域连井(a)及地震相(b)剖面

      Fig.  2.  Profile of Well Connection (a) and Seismic Facies (b) in the Enping Formation of Huizhou 26 depression

      图  3  惠州26洼恩平组恩三四段沉积相(a)、恩二段早期沉积相(b)、恩二段晚期沉积相(c)

      Fig.  3.  Late sedimentary facies of the second member (a), early sedimentary facies of the second member (b), and sedimentary facies of the third and fourth members (c) of the Enping Formation in the Huizhou 26 depression

      图  4  惠州26洼恩平组实测渗透率与埋深关系散点图

      Fig.  4.  Scatter plot of the relationship between measured permeability and burial depth in the Enping Formation in the Huizhou 26 depression

      图  5  惠州26洼恩平组重点井位镜下储层特征

      a. A6-2井,3 155.00 m,砂泥混杂近源堆积,成分成熟度低,孔隙发育极差;b. A6-5井,3 132.46 m,分选好,孔隙发育好,K=2 206 mD,φ=17.4%;c. A6-1井,3 235.00 m,长石粒内溶蚀孔隙;d. A6-5井,3 359.50 m,泥质含量较丰富,见少量高岭石等自生粘土矿物,孔隙发育差,K=2.9 mD,φ=11.56%;e. A6-1井,3 234.50 m,见大量高龄石(A)充填粒间,见微孔;f. A6-1井,3 184.00 m,方解石呈连晶状胶结颗粒产出;g. A6-1,3 306.50 m,见粒状黄铁矿,蜂窝状-片状绿/蒙混层以及手风琴状高岭石充填粒间孔隙产出;h. A6-1,3 415.20 m,针叶状绿泥石和次生加大石英夹杂共生并充填粒间孔隙产出;i. A6-7井,3 660.00 m,有机质充填粒间孔隙;j. B5-2井,3 836.00 m,见有机质条带,粗粒为主,凹凸-线接触,孔隙发育差;k. B5-2井,3 770.00 m,凝灰质充填粒间,并见溶蚀;l. B5-2井,3 815.00 m,填隙物凝灰质含量10%,火山岩岩屑相对含量55%;m. A6-1井,3 234.50 m,半塑性安山岩岩屑;n. A6-4井,3 220.00 m,可见玻屑;o. B5-1井,安山岩砾石见磨圆

      Fig.  5.  Microscopic reservoir characteristics of key well locations in the Enping Formation of Huizhou 26 depression

      图  6  恩平组不同沉积相带井壁心实测物性

      Fig.  6.  Measured physical properties of wellbore cores in different sedimentary facies zones of the Enping Formation

      图  7  惠州26-A构造恩平组下段实测孔隙度(a)、实测渗透率(b)及成分成熟度图(c)

      Fig.  7.  Measured porosity (a), permeability (b), and compositional maturity map (c) of the lower section of the Enping Formation in Huizhou 26-A structure

      图  8  惠州26-A构造EP23层沉积古地貌图(位置见图 1b

      Fig.  8.  Sedimentary Paleogeomorphology Map of EP23 Layer in Huizhou 26-A Structure (see Fig.1b for location)

      图  9  惠州26-A构造单砂体组(EP221、EP231、EP233)微古地貌图(位置见图 1b

      Fig.  9.  Micropaleogeomorphic map of Huizhou 26-A structure single sand body group (EP221, EP231, EP233) (see Figure 1b for location)

      图  10  惠州26-A、27-B构造火山物质的井震特征(a)惠州27-B构造火山物质含量变化规律(b)(位置见图 1b

      Fig.  10.  Well seismic characteristics of volcanic material in Huizhou 26-A and 27-B structures (a) Changes in volcanic material content in Huizhou 27-B structures (b) (see Figure 1b for location)

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    出版历程
    • 收稿日期:  2023-12-23
    • 刊出日期:  2025-08-25

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