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    塔西南地区二叠系普斯格组烃源岩地质特征及TOC测井定量预测

    Source rocks in the Permian Pusige Formation, Southwest Tarim Basin: Geological characteristics, well logging evaluation and hydrocarbon potential analysis

    • 摘要:
      研究目的 烃源岩是油气成藏的物质基础,然而受钻井取心样品数量限制,地球化学分析化验难以实现全井段烃源岩特征的系统性评价。因此,利用测井资料结合人工智能开展烃源岩TOC的连续定量评价与烃源岩预测,对于全面深入分析油气成藏条件尤为重要。
      研究方法 本文利用塔西南坳陷二叠系普斯格组重点井的岩样地球化学分析资料和测井资料,对烃源岩地质特征和总有机碳含量(TOC)的测井评价方法和智能预测方法进行了综合研究。
      研究结果 普斯格组烃源岩以暗色泥岩为主,其TOC处于0.01%~20.6%,平均为1.13%,热解生烃潜量(Pg)为0.02~23.31 mg/g,平均为2.76 mg/g。干酪根类型以Ⅱ2型和Ⅲ型为主,镜质体反射率(Ro)值主体分布于0.55%~2.55%,处于成熟阶段,属于一般—好烃源岩。受灰质泥岩等异常高电阻率影响,传统ΔlgR法适用性较差。本文由此选取自然伽马(GR)、深探测电阻率(M2Rx)、补偿中子(CNC)、补偿密度(DEN)等测井曲线数据采用多元回归分析和随机森林机器学习方法建立了TOC含量定量预测模型,其中随机森林方法效果明显优于多元回归方法,通过随机森林方法实现了研究区单井烃源岩TOC的连续定量评价。
      结论 塔西南坳陷二叠系普斯格组发育一般—好烃源岩。相较于ΔlgR法、多元回归方法,随机森林方法可更为精准地实现本区烃源岩TOC全井段连续定量预测。研究区普斯格组具备充足生烃物质基础、优良储盖组合与有利构造运聚条件,油气勘探潜力可观。

       

      Abstract:
      This paper is the result of oil and gas exploration engineering.
      Objective Source rocks are the fundamental material basis for hydrocarbon accumulation. However, due to the limited number of drilling core samples, geochemical analyses alone are often insufficient to provide a systematic evaluation of source rock characteristics throughout the entire well interval. Therefore, utilizing well-log data combined with artificial intelligence to conduct continuous quantitative evaluation of total organic carbon (TOC) in source rocks and source rock prediction is of great significance for a comprehensive and in-depth analysis of hydrocarbon accumulation conditions.
      Methods This paper comprehensively investigated the geological characteristics of source rocks, as well as logging-based evaluation and intelligent prediction methods for total organic carbon (TOC), using geochemical analysis data of rock samples and logging data from key wells in the Permian Pusige Formation of the Southwestern Tarim Basin.
      Results The source rocks of the Pusige Formation are mainly composed of dark mudstones, with TOC values ranging from 0.01% to 20.6% (average 1.13%). The hydrocarbon generation potential (Pg) varies from 0.02 mg/g to 23.31 mg/g (average 2.76 mg/g). The kerogen types are predominantly Type Ⅱ2 and Type Ⅲ, while vitrinite reflectance (Ro) values are mainly distributed between 0.55% to 2.55%, indicating a mature stage of thermal evolution. Overall, the source rocks are classified as fair to good source rocks. Due to the influence of argillaceous limestones and other lithologies with abnormally high resistivity, the conventional ΔlgR method exhibits poor applicability. To overcome this limitation, this study employed gamma ray (GR), deep resistivity (M2Rx), compensated neutron porosity (CNC), and compensated density (DEN) logging curves to establish a quantitative TOC prediction model using multiple linear regression and random forest machine learning methods. The random forest model performed significantly better than the multiple regression model, enabling continuous quantitative evaluation of source rock TOC in single-wells of the study area.
      Conclusions The Permian Pusige Formation in the Southwestern Tarim Depression develops fair-to-good hydrocarbon source rocks. Compared with the ΔlgR method and multiple regression algorithm, the random forest algorithm can achieve more accurate continuous quantitative prediction of total organic carbon (TOC) content of source rocks along the full well interval in the study area. The Pusige Formation within the research block is characterized by sufficient hydrocarbon-generating material foundation, favorable reservoir-cap rock assemblages and advantageous structural migration and accumulation conditions, demonstrating considerable hydrocarbon exploration potential.

       

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