A petrophysically driven seismic inversion method for TOC content of hydrocarbon source rocks

Zhangbo Xiao, Heming Lin, Weiwei Zhang, Ming Luo, Xudong Wang, Zhiwei Zhang
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Abstract

The organic carbon content is the main index for evaluating organic matter abundance of source rocks, and it is still difficult to quantitatively predict TOC in source rocks based on seismic data. The study of seismic fluid identification driven by petrophysics can help to understand the fluid characteristics and distribution patterns of subsurface oil and gas reservoirs. This paper, first of all, clarified the sweet spot parameters (parameters characterizing hydrocarbon enrichment) and sensitive elastic parameters (a parameter characterizing the nature of an ideal elastic body) of source rocks through theoretical petrophysical modeling, and established the relationship between sensitive elastic parameters and sweet spot parameters TOC, and construct a statistical petrophysical model that can characterize the relationship between the two on this basis. And then construct the joint distribution of TOC and elastic impedance through the Bayesian theoretical framework to obtain the maximum posterior probability estimate as the final TOC inversion results of source rocks. Our method successfully predicts the spreading of high-quality source rocks in the Wen4 Section of Lufeng 13 Subsag, and the inversion results are within an uncertainty range of ±14 m for well data, which proves the reliability of the method. The prediction results show that the organic matter abundance of source rocks in the Wen4 Section is high and the organic carbon content is generally higher than 2%, which provides a reliable basis for the further implementation of the resource scale of the depression and the clarification of the hydrocarbon rich area, which provides technical support for the evaluation of the source rocks of the new depression in the new area.
烃源岩 TOC 含量的岩石物理驱动地震反演方法
有机碳含量是评价源岩有机质丰度的主要指标,而根据地震资料定量预测源岩中的总有机碳含量仍有一定难度。岩石物理驱动的地震流体识别研究有助于了解地下油气藏的流体特征和分布规律。本文首先通过岩石物理理论建模,明确了源岩的甜点参数(表征油气富集的参数)和敏感弹性参数(表征理想弹性体性质的参数),建立了敏感弹性参数与甜点参数TOC之间的关系,并在此基础上构建了能够表征二者关系的统计岩石物理模型。然后通过贝叶斯理论框架构建 TOC 和弹性阻抗的联合分布,得到最大后验概率估计值,作为最终的源岩 TOC 反演结果。我们的方法成功地预测了禄丰 13 子囊文 4 段优质源岩的展布情况,反演结果在油井数据±14 m 的不确定范围内,证明了该方法的可靠性。预测结果表明,文4段源岩有机质丰度较高,有机碳含量普遍高于2%,为进一步落实凹陷资源规模、明确富烃区提供了可靠依据,为新区凹陷源岩评价提供了技术支撑。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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