Fault zone head waves (FZHW) are seismic waves that travel along the boundary between two rock bodies with different speeds. They can reveal contrasts in fault-zone structure that are hard to see with other methods. In a recent paper we
Fault zone head waves (FZHW) are seismic waves that travel along the boundary between two rock bodies with different speeds. They can reveal contrasts in fault-zone structure that are hard to see with other methods. In a recent paper we