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合川-潼南地区茅口组一段泥灰岩总有机碳含量测井评价方法OA

Research on Log Evaluation Method for TOC Content of Marlstone in the First Member of Maokou Formation in Hechuan-Tongnan Area

中文摘要英文摘要

为解决四川盆地合川-潼南地区茅口组一段(简称茅一段)泥灰岩岩性复杂、取心资料有限、总有机碳含量(TOC)精准评价难度大、优质烃源岩分布规律认识不清的问题,分析了研究区测井、岩心及地球化学实测数据,优选出电阻率、声波时差、自然伽马等烃源岩敏感测井参数,验证了改进Δlog R法、自然伽马法两类传统测井评价方法的适用性,构建岩性指示曲线划分岩性单元,运用 Δlog R—GR分岩性权重法建立TOC预测模型,并剖析了区域烃源岩纵向与平面展布特征.研究结果表明:①研究区茅一段泥灰岩TOC为0.04%~3.32%,平均值为0.78%,镜质体反射率平均为2.45%,整体属于中等有机质丰度、高演化程度的海相烃源岩;②改进Δlog R法、自然伽马法计算TOC平均绝对误差分别为0.26%、0.21%,两类方法计算结果具备互补性;③Δlog R—GR分岩性权重法有效规避岩性、滑石等特殊矿物带来的干扰,模型计算TOC平均绝对误差降至0.14%,预测精度显著提升;④区域内茅一段有效烃源岩厚度为 29.0~51.0 m,平均厚度 42.9 m,纵向上茅一 a亚段烃源岩品质优于下部亚段,平面上东南部烃源岩厚度最大,整体自东南向西北方向逐渐减薄,烃源岩厚度与单井试气产能呈现良好对应关系.结论认为,Δlog R—GR 分岩性权重法适用于研究区复杂岩性泥灰岩TOC定量评价,研究成果可为茅一段有利区带优选、井位部署与储层综合评价提供可靠技术支撑.

To address the complex lithology,limited core data,difficulty in accurately evaluating total organic carbon(TOC)content,and unclear understanding of the distribution law of high-quality hydrocarbon source rocks in marlstone of the First Member of Maokou formation(Mao1 member)in the Hechuan-Tongnan Area,Sichuan Basin,logging,core and geochemical test data from the study area.Select the logging information sensitive to source rock such as resistivity,sonic and natural gamma ray,verify the applicability of two conventional logging evaluation methods:the modified Δlog R method and the natural gamma method.A lithology indicator curve is constructed to divide lithologic units,and the lithology-weighted ΔlogR-GR method is adopted to establish the TOC prediction model.The vertical and areal distribution characteristics of regional source rocks are also analyzed.The results show that:①TOC content in the Mao1 member marlstone ranges from 0.04%to 3.32%,with an average of 0.78%;the average vitrinite reflectance is 2.45%,indicating a marine source rock with moderate organic richness and high thermal maturity.②The average absolute errors of TOC calculated by the modified Δlog R method and the natural gamma method are 0.26%and 0.21%,respectively,demonstrating complementary accuracy between the two methods.③The lithology-weighted Δlog R—GR method effectively reduces interference caused by lithology and special minerals such as talc,reducing the average absolute error of TOC calculation to 0.14%,significantly improving prediction accuracy.④The effective thickness of source rocks in the Mao1 member ranges from 29.0 to 51.0 m,averaging 42.9 m.Vertically,source rock quality in the Mao1a submember is superior to that in the lower submembers.Horizontally,the thickest source rocks occur in the southeastern part of the region,gradually thinning from southeast to northwest,with a good correspondence between source rock thickness and single-well gas testing productivity.It is concluded that the lithology-weighted Δlog R—GR method is suitable for quantitative TOC evaluation in complex lithology marlstone in the study area.The achievement provides reliable technical support for favorable zone selection,well placement and comprehensive reservoir evaluation in the Mao1 member.

金雪英;周鹏林;王春燕;温琴

大庆油田有限责任公司勘探开发研究院,黑龙江 大庆 163712大庆油田有限责任公司勘探开发研究院,黑龙江 大庆 163712大庆油田有限责任公司勘探开发研究院,黑龙江 大庆 163712大庆油田有限责任公司勘探开发研究院,黑龙江 大庆 163712

天文与地球科学

茅口组一段泥灰岩TOC测井评价自然伽马法分岩性权重法合川-潼南地区

the first member of Maokou formationmarlstoneTOClog evaluationnatural gamma methodlithology-weighted methodHechuan-Tongnan area

《测井技术》 2026 (4)

684-691,8

国家科技重大专项课题"多物理场测井岩石物理智能建模与分析系统"(2025ZD1401103)

10.16489/j.issn.1004-1338.2026.04.012

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