Advances in Earth Science

   

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).

ZHU Biqing, Gu Tuan, LI Pengpeng, LI Fulai, WEI Yongbo, LIU Quanyou. Geochemical Signatures of Source Rocks and Resource Potential in the Naiman Sag, Southwestern Songliao Basin[J]. Advances in Earth Science, DOI: 10.11867/j.issn.1001-8166.2025.090.

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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