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- W2897626165 abstract "Abstract Unusually high compressional ( P ) to shear ( S ) wave velocity ratios ( V p / V s ) were measured at different subduction zones and interpreted as fluid‐pressurized regions. Because no laboratory data reported such high values in isotropic rocks, mineralogical or anisotropic constrains were assumed. However, fluid‐saturated rocks' V p / V s is a frequency‐dependent property so that standard laboratory measurements cannot be directly upscaled to the field. Using a new methodology, we measured the property in the elastic regime relevant to field measurements for diverse lithologies. We obtained extreme V p / V s values, consistent with those reported at seismic frequency in the field. Consistently with a model, it shows that if high fluid pressure is a key factor, anomalous V p / V s values could evidence intense degrees of microfracturation in isotropic rocks, whichever its mineralogical content. The permeability of these regions could be larger than 10 −16 m 2 ." @default.
- W2897626165 created "2018-10-26" @default.
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- W2897626165 date "2018-11-20" @default.
- W2897626165 modified "2023-09-30" @default.
- W2897626165 title "Anomalous <i>V</i><sub><i>p</i></sub>/<i>V</i><sub><i>s</i></sub> Ratios at Seismic Frequencies Might Evidence Highly Damaged Rocks in Subduction Zones" @default.
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- W2897626165 doi "https://doi.org/10.1029/2018gl080132" @default.
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