The main objective of this research is to recognize several geological structures associated with the shear zones of the MFFS(Magallanes-Fagnano fault system) by the analysis and interpretation of gra
The analysis of space-time surface deformation during earthquakes reveals the variable state of stress that occurs at deep crustal levels, and this information can be used to better understand the sei
The study region is seismically and tectonically characterized by the angle variations in the subduction of the Nazca plate. The results obtained from earthquakes location between 32° and 36°S latitud