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首页> 外文期刊>Journal of Geoscience, Engineering, Environment and Technology >Rock Physics Formula and RMS Stacking Velocity Calculation to Assist Acoustic Impedance Inversion that Constrain Well Data
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Rock Physics Formula and RMS Stacking Velocity Calculation to Assist Acoustic Impedance Inversion that Constrain Well Data

机译:岩石物理公式和rms堆叠速度计算,以帮助解释限制井数据的声阻抗反演

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This research ilustrate the generation of acoustic impedance inversion in the absence of well log using stacking velocity input in Salawati Basin, Papua, Indonesia using data obtained from seismic lines and stacking velocity section. Initial acoustic impedance modelswere first before the inversion process and were created by spreading the value of well log data to the all seismic CDP. The calculated acoustic impedance logs from standard sonic and density logs were used to build the initial model of acoustic impedance.First, the stacking velocities was first interpolated on a grid that has the same size as the seismic data using by means of Polynomial algorithm. This was closely followed by the conversion of the stacking velocities to interval velocities using Dix’s equation. The matrix densities were estimated by simple rock physics approach i.e. Gardner’s equation as a velocity function. The initial model of acoustic impedance was calculated by multiplying the densities section and interval velocities section. The resulting initial model of acoustic impedance was inverted to obtain the best of acoustic impedance section based on reflectivity.
机译:本研究Ilustrate在使用堆积速度输入,印度尼西亚巴布亚,印度尼西亚的堆积速度输入,使用从地震线和堆叠速度部分获得的数据,在缺乏日志中产生声学阻抗反转的产生。初始声阻抗模型首先在反转过程之前,并通过将井日志数据的值传播到所有地震CDP来创建。来自标准Sonic和密度日志的计算的声阻抗日志用于构建声阻抗的初始模型。首先将堆叠速度在具有与多项式算法使用与地震数据具有相同尺寸的网格上的内插。这是密切的,然后使用Dix等式将堆叠速度转换为间隔速度。矩阵密度通过简单的岩石物理方法估计,即加德纳的等式作为速度函数。通过乘以密度部分和间隔速度部分来计算声阻抗的初始模型。所得到的声阻抗初始模型被反转以基于反射率获得最佳的声阻抗部分。

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