Seismic Versus Sonic Revisited

S. Munadi
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Abstract

The sonic log enables all features along the depth scale can be correlated with all features in the ime scale as found in the seismic section. However, this sonic log must beThe sonic log enables all atures along the depth scale can be correlated with all features in the time scale as found in the seismic section. However, this sonic log must be corrected to the time-depth curve obtained from the check shot survey. The problem arises when some zones around the borehole such as the invaded zones or the flushed zones exhibit dispersive properties. This dispersive properties causes discrepancies between integrated sonic transit time and the time-depth curve. As a result, the synthetic seismogram generated from the sonic log will not match with the corresponding seismic section. To solve this problem, a practical method for correcting the discrepancies is presented in this paper. Although the method is inspired by paper published in the seventies, but the way to approach the problem is different. This problem looks simple, but its effect on mapping top and bottom of the reservoir is important. An example of implementation from the real field is also given. corrected to the time-depth curve obtained from the check shot survey. The problem arises when some zones around the borehole such as the invaded zones or the flushed zones exhibit dispersive properties. This dispersive properties causes discrepancies between integrated sonic transit time and the time-depth curve. As a result, the synthetic seismogram generated from the sonic log will not match with the corresponding seismic section. To solve this problem, a practical method for correcting the discrepancies is presented in this paper. Although the method is inspired by paper published in the seventies, but the way to approach the problem is different. This problem looks simple, but its effect on mapping top and bottom of the reservoir is important. An example of implementation from the real field is also given.
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地震vs声波重访
声波测井可以将地震剖面中深度尺度上的所有特征与时间尺度上的所有特征进行对比。声波测井可以将地震剖面中时间尺度上的所有特征与深度尺度上的所有特征相关联。然而,这种声波测井必须校正为从回井测量中得到的时间-深度曲线。当井眼周围的一些区域,如侵入带或冲刷带表现出分散性时,问题就出现了。这种色散特性导致了综合声波传递时间和时间-深度曲线之间的差异。因此,声波测井生成的合成地震记录与相应的地震剖面不匹配。为了解决这一问题,本文提出了一种实用的校正方法。虽然该方法受到了七十年代发表的论文的启发,但处理问题的方式不同。这个问题看起来很简单,但它对绘制水库顶部和底部的影响是重要的。最后给出了一个实际应用的实例。校正后的时间-深度曲线是由检井测量得到的。当井眼周围的一些区域,如侵入带或冲刷带表现出分散性时,问题就出现了。这种色散特性导致了综合声波传递时间和时间-深度曲线之间的差异。因此,声波测井生成的合成地震记录与相应的地震剖面不匹配。为了解决这一问题,本文提出了一种实用的校正方法。虽然该方法受到了七十年代发表的论文的启发,但处理问题的方式不同。这个问题看起来很简单,但它对绘制水库顶部和底部的影响是重要的。最后给出了一个实际应用的实例。
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