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- W2034750078 abstract "Knowledge of shear-wave velocity structure, when used with compressional-wave velocity, can help constrain interpretations of composition from seismic refraction results. We present shear-velocity (vs) models from high-quality S-wave data from Southwest Germany, which combine with existing P-wave velocity (vp) models to give Poisson's ratio in the crust and uppermost mantle. In general, Poisson's ratio is 0.25 in the uppermost crust, 0.22-0.23 in the mid-crust, and varies laterally from 0.24-0.30 in the lower crust; the average Poisson’s ratio for the whole crust is everywhere about 0.25. The laminated signature of the lower crust prominent on reflection and P-wave refraction data is absent on the S-wave refraction data, suggesting strong vertical variations of Poisson's ratio within the lower crust. No shear-wave refractions from the upper mantle are present, even where strong P-wave refractions are observed, possibly indicating an increase of Poisson's ratio with depth in the upper mantle. We interpret these results to indicate a high quartz content or fluid phases at low pore pressure in the mid-crust, a high feldspar content in the lower crust, and an increase in depletion of basaltic components with depth in the upper mantle." @default.
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- W2034750078 date "1987-03-01" @default.
- W2034750078 modified "2023-10-14" @default.
- W2034750078 title "Shear-wave velocity and Poisson's ratio structure of the upper lithosphere in southwest Germany" @default.
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- W2034750078 doi "https://doi.org/10.1029/gl014i003p00231" @default.
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