Reactivation (long-term evolution) of silvia-pijao fault along the “quebrada la maizena “western flank of central cordillera, quindio- colombia.

The macro and microstructural characteristics of rocks along the lower portion of the “Quebradala Maizena”, in the influence zone of the Silvia- Pijao Fault, one of the major faults related to theRomeral Fault Zone (RFZ), allow to interpet a long history of deformation. These rocks belong tothe Queb...