Investigador

Subdirector de CIGIDEN. Geólogo de la Universidad Católica del Norte y Doktor rer Natur, de la Universidad Libre de Berlín. Actualmente es profesor del Departamento de Ciencias Geológicas de la Universidad Católica del Norte, y se especializa en deformación dúctil, análisis de fallas, interacción entre fallas y morfologías, terremotos y remociones en masa, procesos tectónicos en general, análisis de fallas e interacción entre fallas y morfología.
Ha participado en proyectos internacionales relacionados con el estudio de procesos de deformación en zonas de subducción.
Subdirector Cigiden e Investigador principal
ggonzale@ucn.cl
Splay fault slip during the Mw 8.8 2010 Maule Chile earthquake: COMMENT
Permanent fore-arc extension and seismic segmentation: Insights from the 2010 Maule earthquake, Chile
Normal upper plate fault reactivation in northern Chile and the subduction earthquake cycle: From geological observations and static Coulomb Failure Stress (CFS) change
Upper plate reverse fault reactivation and the unclamping of the megathrust during the 2014 northern Chile earthquake sequence
Near-field co-seismic ionospheric response due to the northern Chile Mw 8.1 Pisagua earthquake on April 1, 2014 from GPS observations
The 1 April 2014 Pisagua tsunami: Observations and modeling
The 16 September 2015 Chile tsunami from the post-tsunami survey and numerical modeling perspectives
Accelerated late Quaternary uplift revealed by 10 Be exposure dating of marine terraces, Mejillones Peninsula, northern Chile
Coseismic extension from surface cracks reopened by the 2014 Pisagua earthquake sequence
Geomorpholohy and Structural devepelopment of the nested summit crater of Lascar Volcano studied with terrestrial Laser Scanner data and Analogue Modelling
A climatic trigger for catastrophic Pleistocene–Holocene debris flows in the Eastern Andean Cordillera of Colombia
Slip distribution of the 2014 MW=8.1 Pisagua, northern Chile, earthquake sequence estimated from coseismic fore- arc surface cracks
Structural characteristics of an active fold-and-thrust system in the southeastern Atacama Basin, northern Chile