Tanner, David C.; Lohr, Tina; Krawczyk, Charlotte M.; Oncken, Onno; Endres, Heike; Samiee, Ramin; Trappe, Henning; Kukla, Peter A. (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
Movement on fault planes causes a large
amount of smaller-scale deformation,
ductile or brittle, in the area surrounding
the fault. Much of this deformation
is below the resolution of reflection
seismics (i.e. sub-seismic, ...