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- W2017337227 abstract "Sonic full waveforms were recorded in a shale‐limestone interval with an experimental 12-channel acoustic logging device. Well-defined shear (pseudo‐Rayleigh) waves were observed throughout most of the 142 m interval and were used to distinguish lithologic boundaries and zones of fracturing as interpreted by logs. The high signal‐to‐noise ratio of the waveforms permitted meaningful shear velocities to be obtained by intervals in this well. A correlation of changes in the [Formula: see text] ratio with depth aided in identifying some compositional changes in the well, but such a correlation could not be used to distinguish fracturing in the limestone. Shear‐wave amplitudes, however, were effective for identifying lithologic changes, as well as fractures, from the sonic log. Shear amplitudes were lower in the shale than in the limestone, and shear‐wave attenuation increased in fractured zones. There was no strong correlation between the degree of fracturing and the attenuation of Stoneley waves. In general, shear‐wave processing of sonic logs is recommended for interpretation of lithology and fracturing in any well in which full waveforms are recorded and shear waves propagate." @default.
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- W2017337227 title "Shear‐wave processing of sonic log waveforms in a limestone reservoir" @default.
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- W2017337227 doi "https://doi.org/10.1190/1.1442501" @default.
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