S-wave anisotropy from two dipole sonic data processing methods, confronted with fracture permeability, logs and cores | Science and Technology for Energy Transition (STET)

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Fig. 19

GPF-Ardèche, MM1 borehole: Dipole sonic anisotropy results from both birefringence detection methods, in depth interval 173–225 m. The regional N30° E fault strike direction is drawn as a red line over the FSA/fast S-wave azimuth curve results from both detection methods.

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