摘要
西湖凹陷M气田区块泥岩超压为欠压实和生烃共同作用的结果,目的层砂岩具有低孔渗特征,导致流体孔隙压力预测难度大,为此,基于测井资料分析,建立了适用区块低孔渗地层和多压力异常成因特点的纵波速度压力预测模型,基于非欠压实成因异常压力对总孔隙压力的贡献程度的参数来表征多压力异常成因的压力预测,基于层控和断控多约束层速度反演的低频地震速度建模和叠前AVO反演的精细三维地震速度场的构建策略获得用于地震压力预测所需的三维高精度速度场。实际区块三维地层孔隙压力场的预测结果表明,在工区实测点深度处的孔隙压力预测值与实测值之间的平均误差小于6%,验证了多压力异常成因情形下的压力预测的可靠性。
The mudstone overpressure at M Gas Field in Xihu Sag is formed by a combination of undercompaction and hydrocarbon generation. The low porosity and permeability of the sandstone in the target zone makes it difficult to predict the pore-pressure. Therefore, the P-wave velocity pore-prediction model for the low porosity and permeability strata and multiple overpressure mechanisms is established based on well logging data analysis. The pore-pressure prediction with multiple overpressure mechanisms is characterized by the parameter of the contribution of abnormal pressure caused by non-undercompaction to the total pore pressure. The high-precision seismic velocity field is built based on modelling of the velocity with low-frequency component by multi-constrained velocity inversion under strata bound and fault-controlled and pre-stack AVO inversion. The prediction of three-dimensional pore pressure field in this area shows that the average error between the estimated pore pressures and the measured pore pressures is less than 6%. This verified the reliability of the pressure prediction for the case of multi-pressure abnormality.
引文
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