Leg 200: Drilling at the Hawaii-2 Observatory (H2O) and the Nuuanu Landslide
Figure 7.
Cross-dipole sonic waveforms recorded at depths of 60 and 153 mbsf. They can be used to detect shear wave anistropy for fracture and stress analyses.
Cross-dipole sonic waveforms recorded at depths of 60 and 153 mbsf. They can be used to detect shear wave anistropy for fracture and stress analyses.