录井工程 ›› 2023, Vol. 34 ›› Issue (2): 103-108.doi: 10.3969/j.issn.1672-9803.2023.02.017
杨毅①, 郭东明①, 程乐利②, 袁胜斌①, 陈恭洋②, 印森林②
YANG Yi①, GUO Dongming①, CHENG Leli②, YUAN Shengbin①, CHEN Gongyang②, YIN Senlin②
摘要: 渤中凹陷东营组地层普遍发育超压,对其超压地质成因仍有争议。前人通过声波速度与有效应力图板法分析,认为东营组超压以欠压实成因为主,而东营组发育大段泥岩地层,其中的高有机碳含量对于声波时差的影响不容忽视。基于地化录井资料对重点井的声波时差曲线进行了有机碳含量校正,重新分析了东营组超压层特征,并探讨了烃源岩超压成因分类。结果表明:渤中凹陷东营组超压层普遍具有高有机碳含量特征,声波时差经过校正后明显减小,平均降低幅度16.8%,将校正后的资料进行重新投点,表现为流体膨胀特征,这一结论与地层响应特征相符,有助于提高区域地层压力预监测精度,对其他地区烃源岩层系超压成因研究具有借鉴意义。
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