
1.页岩油气富集机理与高效开发全国重点实验室,北京 102206
2.中国石化石油勘探开发研究院,北京 102206
3.中国石化石油勘探开发研究院无锡石油地质研究所,江苏 无锡 214126
Received:09 January 2026,
Online First:30 July 2026,
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赵培荣, 李楚雄, 申宝剑, 等. 中国咸化湖盆页岩生烃特征与分析技术研究进展[J]. 油气藏评价与开发, XXXX, XX(XX): 1-14.
ZHAO Peirong, LI Chuxiong, SHEN Baojian, et al. Research Progress on Hydrocarbon Generation Characteristics and Analytical Techniques of Shale in Saline Lacustrine Basins in China[J]. Petroleum Reservoir Evaluation and Development, XXXX, XX(XX): 1-14.
赵培荣, 李楚雄, 申宝剑, 等. 中国咸化湖盆页岩生烃特征与分析技术研究进展[J]. 油气藏评价与开发, XXXX, XX(XX): 1-14. DOI: 10.13809/j.cnki.cn32-1825/te.20260005.
ZHAO Peirong, LI Chuxiong, SHEN Baojian, et al. Research Progress on Hydrocarbon Generation Characteristics and Analytical Techniques of Shale in Saline Lacustrine Basins in China[J]. Petroleum Reservoir Evaluation and Development, XXXX, XX(XX): 1-14. DOI: 10.13809/j.cnki.cn32-1825/te.20260005.
咸化湖盆页岩油作为陆相页岩油气资源的重要类型,其成烃过程受到沉积、成岩等多重调控,表现出显著的复杂性与差异性。通过对中国典型咸化湖盆页岩地质特征的资料调研,结合密闭体系、半开放体系生烃模拟及有机硫分析等实验技术研究成果,系统探讨了中国咸化湖盆页岩差异生烃成因机理。研究表明:咸化湖盆页岩岩相、有机相类型丰富且非均质性较强,主力烃源岩层系普遍具有中-高有机质丰度、Ⅰ-Ⅱ
2
型为主的干酪根类型和0.7%~1.3%(
R
o
)的热演化程度。部分典型页岩生烃过程呈现“双峰生油”分异特征:硫酸盐型湖盆页岩为“低熟油-成熟油”双峰,碱性碳酸盐型湖盆页岩为“成熟油-高熟油”双峰。沉积环境控制下的成烃生物类型主导了烃源岩物质基础与生烃过程。有机硫通过低键能C—S键结构降低干酪根生烃活化能,促使页岩生烃门限前移。盐类矿物、黏土矿物、火山矿物、碱类矿物通过催化反应、氢源供给、皂化反应等有机-无机相互作用调控了生烃路径与产物组成。通过实验技术创新与机理深化,实现了从微观化合物到宏观地质过程的生烃动态模拟,为咸化湖盆页岩生烃动力学建模、资源潜力评价及“甜点”层段预测提供了关键技术支撑。本研究对完善陆相页岩生烃理论、指导陆相页岩油气高效勘探开发具有重要意义。
As an important type of continental shale oil and gas resources
shale oil in saline lacustrine basins is subject to multiple controls such as sedimentation and diagene
sis during its hydrocarbon generation process
showing remarkable complexity and heterogeneity. Based on data investigation of the geological characteristics of shales in typical saline lacustrine basins in China
combined with research results from experimental techniques including closed-system and semi-open-system hydrocarbon generation simulations and organic sulfur analysis
this study systematically discusses the genetic mechanism of differential hydrocarbon generation of shales in saline lacustrine basins in China. The results show that shales in saline lacustrine basins are rich in lithofacies and organic facies types with strong heterogeneity
and the major source rock intervals generally have moderate to high organic matter abundance
kerogen types dominated by Type Ⅰ-Ⅱ
2
and thermal maturity ranging from 0.7% to 1.3% vitrinite reflectance (
R
o
). Some typical shales exhibit a bimodal oil generation characteristic during hydrocarbon generation: bimodal distribution of low-mature oil and mature oil for shales in sulfate-type lacustrine basins
and bimodal distribution of mature oil and high-mature oil for shales in alkaline carbonate-type lacustrine basins. The types of hydrocarbon-generating organisms controlled by sedimentary environments dominate the material basis and hydrocarbon generation process of source rocks. Organic sulfur reduces the hydrocarbon generation activation energy of kerogen through low-bond-energy C-S bonds
leading to an earlier hydrocarbon generation threshold of shales. Salt minerals
clay minerals
volcanic minerals and alkaline minerals regulate hydrocarbon generation pathways and product compositions through organo-mineral interactions such as catalytic reactions
hydrogen supply and saponification. Through innovative experimental techniques and in-depth mechanism analysis
dynamic simulation of hydrocarbon generation from microscopic compounds to macroscopic geological processes has been realized
providing key technical support for kinet
ic modeling of hydrocarbon generation
resource potential evaluation and “sweet spot” interval prediction of shales in saline lacustrine basins. This study is of great significance for improving the theory of continental shale hydrocarbon generation and guiding the efficient exploration and development of continental shale oil and gas.
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