中国石油勘探 ›› 2012, Vol. 17 ›› Issue (6): 23-27,5.

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廊固凹陷烃源岩精细评价研究及应用

金凤鸣,师玉雷,罗强,董雄英,钟雪梅   

  • 出版日期:2012-12-15 发布日期:2012-12-15
  • 基金资助:
    中国石油天然气股份有限公司科技项目“成熟探区油气分布规律与精细勘探技术研究”(2011D-0703)部分成果

Research and Application of Detailed Assessment on Hydrocarbon Source Rock of Langgu Depression

Jin Fengming,Shi Yulei,Luo Qiang,Dong Xiongying and Zhong Xuemei   

  1. Jin Fengming, Shi Yulei, Luo Qiang, Dong Xiongying, Zhong Xuemei//Exploration and Development Research Institute of PetroChina Huabei Oilfield Company, Renqiu City, Hebei Province 062552
  • Online:2012-12-15 Published:2012-12-15

摘要: 烃源岩测井评价利用纵向连续高分辨率测井信息估算地层的泥岩有机碳含量,弥补了因地球化学数据不足在区域范围识别烃源岩空间展布的困难,为资源量估算及油气勘探决策提供依据。研究采用了主要利用ΔlogR方法并结合地质统计分析及不同地质条件下校正的测井信息评价烃源岩方法,对廊固凹陷191口井进行评价,并结合区域地层及沉积资料,精细刻画不同层系优质、中等、差烃源岩在空间的展布。廊固凹陷烃源岩主要发育在沙三段、沙四段,总体上为巨厚的中等—差烃源岩,厚达700~3000m,而优质烃源岩在区域上具有分布面积小、但厚度薄的特点,厚度仅为30~70m。优质烃源岩主要发育在湖侵体系域,且烃源岩中心在变化,沙四段优质烃源岩主要分布于曹家务—永清一带,而沙三段优质烃源岩主要分布于旧州—固安一带。

关键词: 廊固凹陷, 测井, 烃源岩, 有机碳

Abstract: Vertical continuous high-resolution logging information is used in logging assessment of hydrocarbon source rock to evaluate the content of organic carbon in mudstone of the formation. This will solve the bottleneck of identifying space distribution of regional hydrocarbon source rock owing to inadequate geochemical data and provide the basis for calculation of reserves and making decisions on oil and gas exploration. The study adopts Δ logR method and is combined with geological statistical analysis and logging information corrected under different geological conditions to assess hydrocarbon source rock. This method used to appraise 191 wells in Langgu Depression. Based on regional and stratigraphic sediment data, it make detailed description of space distribution of high-quality, medium-quality and poor hydrocarbon rock in different stratum series. In Langgu Depression, hydrocarbon source rock developed mainly in Es3 and Es4 with the thickness mainly reaching 700 meters to 3000 meters at the medium and low quality. High-quality hydrocarbon source rock is distributed in small area with short thickness, only 30 meters to 70 meters. High-quality source rock developed mainly in the lake invasion system. With the center of source rock changing, high-quality source rock of Es4 is mainly distributed in the Caojiawu-Yongqing zone while high-quality source rock of Es3 is distributed in Jiuzhou-Gu?an zone.

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