The Cabuérniga Fault System (CFS) extends for 150 km in E–W trend along the northern divide of Cantabrian Mountains, near Sea. This fault system was reactivated several times since Paleozoic, and displays hydrothermal activity nowadays. We present here a detailed geological map whole CFS six cross-sections distributed strike, which allowed us to unravel kinematic history individual segments com...

The northeastern region (NER) of India has several complex regional geological structures, out which the Dauki fault (DF) is a prominent one. E–W trending reverse DF, inferred to go through southern margin Shillong Plateau (SP), played major role in deformation adjoining areas and was believed be active during Late Quaternary time. Previous paleoseismological studies conducted on eastern wester...