Gudmundsson, Agust; Geyer, Adelina (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
When viewed as ideal elastic cracks,
seismogenic faults are often modeled as
decreases from the host rock to the
boundary between the core and the damage
zone.
mode II or mode III cracks in semiinfinite
elastic bodies or ...