西南石油大学学报(自然科学版) ›› 2023, Vol. 45 ›› Issue (4): 55-71.DOI: 10.11885/j.issn.1674-5086.2022.03.11.03

• 地质勘探 • 上一篇    下一篇

珠三拗陷优质烃源岩地震相特征及分布预测

游君君1, 雷明珠2, 刘亿2, 翟亚楠2, 江黎1   

  1. 1. 中海石油(中国)有限公司湛江分公司, 广东 湛江 524057;
    2. 中海石油(中国)有限公司海南分公司, 海南 海口 570312
  • 出版日期:2023-08-10 发布日期:2023-07-18
  • 通讯作者: 游君君,E-mail:youjj@cnooc.com.cn
  • 作者简介:游君君,1981年生,男,汉族,湖南新化人,高级工程师,硕士,主要从事地球化学与成藏综合研究。E-mail:youjj@cnooc.com.cn;雷明珠,1987年生,女,汉族,湖北咸宁人,工程师,硕士,主要从事石油地质方面的研究。E-mail:leimzh@cnooc.com.cn;刘亿,1988年生,男,汉族,四川武胜人,工程师,硕士,主要从事油气勘探方面的研究。E-mail:liuyi23@cnooc.com.cn;翟亚楠,1992年生。女,汉族,河南焦作人,工程师,硕士,主要从事油气地球化学及成藏方面的研究。E-mail:zhaiyn2@cnooc.com.cn;江黎,1996年生,女,汉族,山东潍坊人,助理工程师,主要从事油气地化成藏方面的研究。E-mail:jiangli12@cnooc.com.cn
  • 基金资助:
    国家重点研发计划(2019YFA0708504)

Characteristics of Seismic Facies of High-quality Source Rocks and Prediction of Their Distributions in the Zhu III Depression, Pearl River Mouth Basin

YOU Junjun1, LEI Mingzhu2, LIU Yi2, ZHAI Yanan2, JIANG Li1   

  1. 1. CNOOC China Limited, Zhanjiang Branch, Zhangjiang, Guangdong 524057, China;
    2. CNOOC China Limited, Hainan Branch, Haikou, Hainan 570312, China
  • Online:2023-08-10 Published:2023-07-18

摘要: 珠三拗陷不同沉积环境发育的烃源岩地球化学特征及成藏贡献差异较大,各相带烃源岩的空间分布尚不明确,制约了下一步油气勘探工作。通过综合分析岩屑、测井、地球化学和地震资料,对珠三拗陷优质烃源岩分布开展了系统研究。研究结果表明: 1)文昌B凹陷文昌组中深湖相烃源岩、滨浅湖相烃源岩和文昌A凹陷恩平组浅湖相烃源岩地震相特征分别为强振幅-低频-平行-中连续反射、弱振幅-低频-平行-弱连续反射(或空白反射)和中弱振幅-低频-平行-中连续反射(或杂乱反射)。2)文昌B凹陷中深湖相优质源岩广泛分布于凹陷中心和陡坡带,滨浅湖相烃源岩分布于中心边缘和缓坡带。但文昌A凹陷中深湖相烃源岩仅分布于凹陷中心,滨浅湖相烃源岩大面积分布于凹陷周缘。因此,文昌B凹陷文昌组中深湖相和浅湖相烃源岩以及文昌A凹陷滨浅湖相烃源岩为主力烃源岩。

关键词: 珠三拗陷, 恩平组, 文昌组, 优质烃源岩, 地震相

Abstract: The source rocks developed in different sedimentary environments have different geochemical characteristics and contributions to petroleum accumulation. However, the spatial distribution of the source rocks of different facies is unknow, which restricts the following petroleum exploration. Based on the comprehensive analysis of rock debris, well logging, geochemistry and seismic data, the characteristics of seismic facies of high-quality sources within the Enping Formation and Wenchang Formation as well as their distribution modes are systematically investigated. The results demonstrate that: 1) the seismic facies of the source rocks of the Wenchang Formation deposited in the semi-deep and shallow lake in the Wenchang B Sag as well as the source rocks of Enping Formation deposited in the shallow lake are featured by strong amplitude-low frequency-parallel-moderately continuous reflection, weak amplitude-low frequency-parallel-weakly continuous reflection, and moderate and weak amplitude-low frequency-parallel-moderately continuous reflection (or chaotic reflection). 2) the highquality source rocks deposited in the semi-deep lake in the Wenchang B Sag are widely distributed in the sag center and steep slope zone, whereas the source rocks deposited in shallow lake are primarily distributed in the sag center and gentle slope; however, the source rocks deposited in the semi-deep lake are only located in the sag center in the Wenchang A Sag, and the source rocks deposited in the shallow lake are well developed around the sag. Thus, source rocks deposited in the semi-deep lake and shallow lake within the Wenchang Formation in the Wenchang B Sag and that deposited in the shallow lake in the Wenchang A Sag are the primary source rocks.

Key words: Zhu III Depression, Enping Formation, Wenchang Formation, high-quality source rocks, seismic facies

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