M

MAGGI M

Last name: MAGGI M

2013 (v1)

Publication

Metadata-only

The role of fault surface geometry in the evolution of the fault deformation zone: comparing modeling with field example from the Vignanotica normal fault (Gargano, Southern Italy)

MAGGI M Cianfarra P Salvini F.

Faults have a (brittle) deformation zone that can be described as the presence of two distintive zones: an internal Fault core (FC) and an external Fault Damage Zone (FDZ). The FC is characterized by grinding processes that comminute the rock grains to a final grain-size distribution characterized by the prevalence of smaller grains over...

Uploaded on: April 14, 2023