伊朗西南部某油田地震资料反演用于层速度建模

Pooria Kianoush , Ghodratollah Mohammadi , Seyed Aliakbar Hosseini , Nasser Keshavarz Faraj Khah , Peyman Afzal
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引用次数: 0

摘要

地震速度被认为是与地层压力变化相关的最佳属性。通过地震反演将地震属性和测井数据相结合,以最高的精度预测整个油田的储层特征。本研究特别介绍了伊朗西南部整个南阿扎德甘油田碳酸盐岩地层的地震速度。所考虑的数据集包括三维地震数据、垂直地震剖面(VSP)、23口井的测井数据和地质信息。在这里,我们使用叠后偏移速度、地震反演以及声阻抗(AI)模型和声波测井之间的关系来估计层速度,以预测地层压力。结果表明,相关系数为0.71,反演精度高(相对误差8.76%)。使用AI地震属性,实际和预测的P波(Vp)相关系数计算为0.74,所有七个相关系数计算均为0.79。因此,估计的Vp与原始测井值一致。油田较深地层中的倒置AI立方体约为8000-15000[(m/s)*(g/cm3)],可称为钙质地层。考虑协同克里格的序列高斯模拟(SGS)产生的Vp立方体与AI的相关性,其中使用逆距离加权(IDW)方法的初始速度立方体为0.54,大于在协同克里格中应用区间偏移速度趋势的相同方法。垂直变差函数范围的最终Vp立方体的各向异性为96m,主方向和次方向的各向异性均为11850m。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Inversion of seismic data to modeling the Interval Velocity in an Oilfield of SW Iran

Seismic velocity is considered the best attribute related to formation pressure changes. Integrating seismic attributes and well-logging data through seismic inversion predicts the reservoir characteristics across the field with the highest accuracy. This study especially presents seismic velocity for the whole south Azadegan Field in SW Iran for carbonate formations. The considered dataset includes 3D seismic data, vertical seismic profiling (VSP), logging data of 23 wells, and geological information. Here, we estimated the interval velocity using post-stack migration velocity, seismic inversion, and the relationship between the acoustic impedance (AI) model and the sonic log to predict formation pressure. As a result, the correlation coefficient of 0.71 and a high inversion accuracy (8.76% relative error) is concluded. The actual and predicted P-wave (Vp) correlation coefficient is calculated as 0.74 and all sevens as 0.79 using an AI seismic attribute. Thus, the estimated Vp agrees with the original well-log values. Inverted AI cubes in the deeper formations of the field are about 8000-15000 [(m/s)*(g/cm3)], which could be referred to as calcareous formations. The correlation of the Vp cube resulting from the Sequential Gaussian simulation (SGS) considering co-kriging with the AI, with the initial velocity cube using the inverse distance weighted (IDW) method being 0.54 is more than the same method applied with interval migration velocity trend in co-kriging. The anisotropy of the final Vp cube for the vertical variogram range is 96m, and for major and minor directions is 11850 m.

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