The Maghlaq Fault is a large, left-stepping normal fault (displacement >210 m) cutting the Oligo-Miocene pre- to syn-rift carbonates of SW Malta. Two principal slip zones separate the deformed rocks of the fault zone from ...
The distinct element method is used for modeling the growth of normal faults in
layered sequences. The models consist of circular particles that can be bonded together with breakable cement. Size effects of the model ...