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Estimation Of Formation Parameters Using Full Waveform Acoustic and Shear Wave Logs

机译:利用全波形声波和剪切波测井估算地层参数

摘要

A combination of borehole Stoneley waves from full waveform acoustic logs and directshear wave logs was used to estimate formation permeability and shear wave velocity.Data sets used here were collected by Area's array full waveform acoustic logging tooland shear wave logging tool. The P- and S-wave velocities of the formation are determinedby threshold detection with cross-correlation correction from the full waveformand the shear wave log, respectively. The full waveform acoustic logging data are alsoprocessed using the Extended Prony's method to estimate the borehole Stoneley wavephase velocity and attenuation as a function of frequency. Two different borehole modelsare considered for the inversion of Stoneley wave velocity and attenuation data. Theyare the isotropic elastic and the porous isotropic borehole models. Inversion parametersinclude shear wave velocity and formation permeability. Inverted shear wave velocitiesand permeabilities are compared with the shear wave log and the core permeabilitymeasurements, respectively, for an integrated interpretation and possible identificationof shear wave anisotropy.
机译:结合全波形声波测井和直接剪切波测井的钻孔斯通利波来估算地层渗透率和剪切波速度。这里使用的数据集是由Area的阵列全波形声波测井仪和剪切波测井仪收集的。地层的P波和S波速度分别通过阈值检测和互相关校正从全波形和横波测井中确定。还使用扩展Prony方法处理完整的波形声波测井数据,以估计钻孔Stoneley波相速度和衰减随频率的变化。考虑两种不同的井眼模型来进行斯通利波速度和衰减数据的反演。它们是各向同性弹性模型和多孔各向同性钻孔模型。反演参数包括剪切波速度和地层渗透率。分别将反演的横波速度和渗透率与横波测井曲线和岩心渗透率测量值进行比较,以便对横波各向异性进行综合解释和识别。

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  • 作者

    Cheng N. Y.; Cheng C. H.;

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  • 年度 1992
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