地球科学进展 doi: 10.11867/j.issn.1001-8166.2025.090

   

松辽盆地西南部奈曼凹陷烃源岩地球化学特征及资源前景
朱必清1,古团2,李朋朋1,李福来3,魏永波4,刘全有1*   
  1. (1. 北京大学 能源研究院,北京 100871;2. 中国石油辽河油田分公司勘探开发研究院,辽宁 盘锦 124010;3. 中国石油大学(华东)地球科学与技术学院,山东 青岛 266580;4. 中国科学院地质与地球物理研究所深层油气理论与智能勘探开发重点实验室,北京 100029)
  • 基金资助:
    国家自然科学基金基础科学中心项目(编号:42488101)资助.

Geochemical Signatures of Source Rocks and Resource Potential in the Naiman Sag, Southwestern Songliao Basin

ZHU Biqing1, Gu Tuan2, LI Pengpeng1, LI Fulai3, WEI Yongbo4, LIU Quanyou1*   

  1. (1. Institute of Energy, School of Earth and Space Sciences, Peking University, Beijing 100871, China; 2. Exploration & Development Research Institute of Liaohe Oilfield Branch Company, PetroChina, Panjin Liaoning 124010, China; 3. School of Geosciences in China University of Petroleum (East China), Qingdao 266580, China; 4. Key Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China)
  • About author:ZHU Biqing, research areas include petroleum geochemistry and multi-sphere interactions. E-mail: zhubq@stu.pku.edu.cn
  • Supported by:
    Project supported by the National Natural Science Foundation of China (Grant No. 42488101).
奈曼凹陷位于松辽盆地西南缘,整体勘探程度较低,其油气成藏条件和主控因素尚不明 确。在系统梳理前人研究成果的基础上,结合钻井、地震及储层岩性和物性等资料,综合分析了奈 曼凹陷的石油地质特征、成藏主控因素及资源潜力。结果表明,区内主要发育沙海组、九佛堂组下 段和义县组3 套烃源岩,集中分布于凹陷北部,整体处于低熟—成熟阶段。其中,九佛堂组下段发 育半深湖—深湖相泥页岩,有机质丰度较高(总有机碳平均为2.79%),类型以Ⅰ型和Ⅱ1型为主,为该 区主要烃源岩。生物标志物特征显示,其形成于高盐度、强还原的湖相环境,母质来源为低等水生 生物与高等陆生植物的混合。区内油气以稠油和湿气为主,其中稠油未经历明显生物降解,主要 受低成熟度控制;天然气属于低熟—成熟阶段腐泥型气,直接来自干酪根裂解。油气富集受良好 源—储配置、优势沉积相带和有利岩性共同控制,整体呈现“相带—岩性—构造”三元耦合特征。 此外,深部流体活动可能在成藏过程中发挥重要作用,不仅促进有机质再生烃作用,还可能引起伴 生稀贵气体(如H2和He)富集。总体上,凹陷中心及深层“甜点区”具备烃源充足、圈闭近源和流体 活跃等有利条件,具有较高的油气勘探潜力。未来研究应关注多因素耦合下的成藏机理,以深化 对奈曼凹陷油气系统的整体认识。
Abstract:The Naiman Sag, located in the southwestern part of the Songliao Basin, remains underexplored, and the conditions for hydrocarbon accumulation and the main controlling factors are not yet well understood. Based on a comprehensive review of previous studies and an integration of data from drilling, seismic profiles, and reservoir lithology and petrophysics, this study analyzes the petroleum geological characteristics, controlling factors for hydrocarbon accumulation, and resource potential of the Naiman Sag. The results indicate that the primary hydrocarbon source rocks in the region are the Shahai, lower Jiufotang, and Yixian formations, which are mainly concentrated in the northern part of the sag and are generally in the low-to-mature stage (Ro% <1.0). Among them, the lower Jiufotang Formation, developed in semi-deep lake to deep lake facies, contains highquality source rocks with high organic matter abundance (average TOC of 2.79%) and a predominance of Type I and Type II₁ kerogen. These source rocks are the primary contributors to hydrocarbons in the region. Biomarker characteristics indicate that the source rocks formed in a high-salinity, strongly reducing lacustrine environment, with mixed contributions from lower aquatic organisms and higher terrestrial plants. The hydrocarbons in the region are primarily heavy oil and wet gas, with heavy oils not undergoing significant biodegradation and mainly controlled by low maturity. The natural gas is characterized as sapropelic kerogen-derived gas in the low-tomature stage, directly resulting from kerogen cracking. Hydrocarbon accumulation is primarily controlled by favorable source-reservoir configurations, dominant depositional facies, and advantageous lithology, demonstrating a trinity of "facies – lithology– structure" coupling. Additionally, deep fluid activities may play an important role in the accumulation process by not only promoting secondary hydrocarbon generation but also contributing to the enrichment of associated noble gases such as hydrogen and helium. Overall, the central and deeper “sweet-spot” zones of the sag, with abundant hydrocarbon supply, proximal traps, and active fluid movement, show significant exploration potential. Future studies should focus on the unconventional accumulation mechanisms under multi-factor coupling to deepen the understanding of the petroleum system in the Naiman Sag.

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[1] 夏柳青, 张敏, 吴喻祥. 煤系烃源岩中高丰度三环萜烷的组成特征及其成因探讨[J]. 地球科学进展, 2025, 40(4): 424-438.
[2] 鲍园, 唐佳阳, 琚宜文, 安超. 鄂尔多斯盆地东南缘黄陵矿区中生代煤系烃源层构造—热演化过程与生物气生成[J]. 地球科学进展, 2021, 36(10): 993-1003.
[3] 蔡郁文, 王华建, 王晓梅, 何坤, 张水昌, 吴朝东. 铀在海相烃源岩中富集的条件及主控因素[J]. 地球科学进展, 2017, 32(2): 199-208.
[4] 汪少勇, 李建忠, 郭秋麟, 李登华. 层次分析法在致密油有利区优选中的应用——以川中侏罗系大安寨段为例[J]. 地球科学进展, 2015, 30(6): 715-723.
[5] 吉利明,李林涛,吴涛,张晓宝,周世新. 柴达木盆地始新统沟鞭藻及其油源意义[J]. 地球科学进展, 2007, 22(3): 221-226.
[6] 陈启林;周洪瑞;李相博;. 蒙甘青地区早白垩世原型盆地特征及其对烃源岩分布的控制[J]. 地球科学进展, 2005, 20(6): 656-663.
[7] 陈中红;查明. 烃源岩排烃作用研究现状及展望[J]. 地球科学进展, 2005, 20(4): 459-466.
[8] 腾格尔;刘文汇;徐永昌;陈践发. 无机地球化学参数与有效烃源岩发育环境的相关研究[J]. 地球科学进展, 2005, 20(2): 193-200.
[9] 郑军卫;刘文汇;史斗. 塔里木盆地深层气勘探潜势[J]. 地球科学进展, 2004, 19(5): 802-807.
[10] 涂建琪,金奎励. 表征海相烃源岩有机质成熟度的若干重要指标的对比与研究[J]. 地球科学进展, 1999, 14(1): 18-23.
[11] 刘大锰. 有机岩石学的研究现状与进展[J]. 地球科学进展, 1994, 9(3): 18-23.
[12] 肖贤明. 有机岩石学及其在油气评价中的应用[J]. 地球科学进展, 1992, 7(2): 39-.
[13] 关德师,王岑红,洪峰,边玉平. 我国油气形成模拟实验概述[J]. 地球科学进展, 1990, 5(4): 19-22.
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