下古生界烃源岩成熟度研究进展及存在问题

Research progress and challenges in thermal maturity evalution of Lower Paleozoic source rocks

  • 摘要: 中国下古生界海相烃源岩普遍处于高—过成熟阶段,且由于缺乏镜质体,下古生界地层的成熟度评价一直是深地油气勘探的技术难点。对基于有机岩石学、地球化学及光谱的有机质成熟度评价方法进行系统归纳,探讨各类成熟度参数在下古生界高—过成熟烃源岩中的适用性,以期为深地油气资源勘探提供指导。重点分析了笔石表皮体反射率、芳烃分子标志物参数、拉曼光谱参数,并指出存在的问题与发展趋势:(1)笔石表皮体反射率因其热敏感性而被广泛应用于表征下古生界地层成熟度,但不同类型的笔石表皮体具有不同的反射率升高速率,并在生气窗出现“反射率异常”现象;(2)芳烃化合物(如菲系列和二苯并噻吩系列)及相关参数(如甲基菲指数MPI-1和甲基二苯并噻吩中的4-MDBT/1-MDBT)的热稳定性表现敏感,可成为有效的成熟度评价参数,但也受初始有机质类型及环境的影响;(3)拉曼光谱可通过D1峰和G峰的相关参数来表征分子结构和成熟度变化,但由于不同实验室的仪器、采用波长和解谱方式的差异,不利于通用对比。通过进一步总结成熟度参数的理论基础和适用范围,指出矿物催化、辐射效应和热模拟实验对参数适用性的影响,提出多参数联合分析可提升成熟度评价的准确性,但校准方法仍需优化。

     

    Abstract: Marine source rocks in China's Lower Paleozoic are predominantly in the highly to over-mature stage. The lack of vitrinite in these strata has made thermal maturity evaluation a persistent technical challenge in deep hydrocarbon exploration. This study systematically summarizes organic matter maturity evaluation methods based on organic petrology, geochemistry, and spectroscopy, with the goal of assessing the applicability of various maturity parameters for highly to over-mature source rocks in the Lower Paleozoic, thereby providing insights for deep hydrocarbon resource exploration. Special emphasis is placed on analyzing graptolite reflectance, aromatic hydrocarbon molecular marker parameters, and Raman spectroscopy parameters, highlighting current challenges and future research directions. (1) Owing to its excellent thermal sensitivity, graptolite reflectance is extensively employed to characterize the maturity of Lower Paleozoic source rocks. Nevertheless, different graptolite types exhibit varying rates of reflectance increase, with "reflectance anomalies" observed within the gas window. (2) Aromatic hydrocarbon compounds (e.g., phenanthrene series and dibenzothiophenes) and their derived parameters (e.g., methylphenanthrene index MPI-1, and 4-MDBT/1-MDBT in methyldibenzothiophene) exhibit sensitive thermal stability responses, rendering them effective maturity evaluation parameters. However, their applicability might be constrained by the initial organic matter type and depositional environment. (3) Raman spectroscopy can effectively characterize molecular structure evolution and thermal maturity, through parameters derived from the D1 and G peaks. However, variations in laboratory instruments, wavelength selection, and spectral interpretation methods might limit comparability across studies. Finally, this study summarizes the theoretical foundations and practical applicability of these parameters, highlighting the impacts of mineral catalysis, radiation effects, and thermal simulation experiments on their suitability. The results demonstrate that a multi-parameter integrated approach significantly improves the accuracy of maturity evaluation. However, current calibration methodologies still require refinement to achieve optimal performance.

     

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