N.1 Allmendinger, R. W., González, G., G.., Yu, J., Isacks, B.L. (2003). The east-west faults scarps of northern Chile: Tectonics significance and climates clues. Congreso(?)

       N.2  Allmendinger, R. W., & González, G. (2009). Neogene to Quaternary tectonics of the coastal Cordillera, northern Chile. Tectonophysics,495(1), 93-110.

       N.3 Allmendinger, R. W., González, G., Yu, J., Hoke, G., & Isacks, B. (2005). Trench-parallel shortening in the Northern Chilean Forearc: Tectonic and climatic implications. Geological Society of America Bulletin, 117(1-2), 89-104.

       N.4 Allmendinger, R. W., & González, G. (2010). Invited review paper: Neogene to Quaternary tectonics of the coastal Cordillera, northern Chile. Tectonophysics,495(1), 93-110.

       N.5 Armijo, R., & Thiele, R. (1990). Active faulting in northern Chile: ramp stacking and lateral decoupling along a subduction plate boundary. Earth and Planetary Science Letters, 98(1), 40-61.

        N.6 Becerra, A., Podestá, L., Monetta, R., Sáez, E., Leyton, F., & Yañez, G. (2015). Seismic microzoning of Arica and Iquique, Chile. Natural Hazards,79(1), 567-586.

       N.7 Carrizo, D., & González, G. (2003). Modelo de crecimiento de la Falla Salar del Carmen,Sistema de Fallas de Atacama, Cordillera de la Costa, norte de Chile. In Congreso Geológico Chileno (No. 10, pp. 578-582). 

       N.8 Carrizo, D., Gonzalez, G., Cembrano, J., Yañez, G., Jensen, A., Espina, J., & Andrónico,J. (2005). Reverse fault geometry of the Chuculay system, northern Chilean outer forearc, using morphotectonical and numerical approach.

       N.9 Carrizo, D., González, G., & Dunai, T. (2008). Constricción neógena en la Cordillera de la Costa,norte de Chile: neotectónica y datación de superficies con 21Ne cosmogónico.Revista geológica de Chile, 35(1), 01-38.

       N.10 Cortes-Aranda, J., Gonzalez, G., Rémy, D., & Martinod, J. (2015). Normal upper plate fault reactivation in northern Chile and the subduction earthquake cycle: From geological observations and static Coulomb Failure Stress (CFS) change.
Tectonophysics, 639, 118-131.

       N.11 Cortés, A., González, L., Binnie, S. A., Robinson, R., Freeman, S. P. H. T., & Vargas, E. (2012). Paleoseismology of the Mejillones Fault, northern Chile: Insights from cosmogenic 10Be and optically stimulated luminescence determinations. Tectonics, 31(2).

       N.12 Delouis, B., Cisternas, A., Dorbath, L., Rivera, L., & Kausel, E. (1996). The Andean subduction zone between 22 and 25 S (northern Chile): precise geometry and state of stress. Tectonophysics, 259(1), 81-100.

       N.13 Delouis, B., Monfret, T., Dorbath, L., Pardo, M., Rivera, L., Comte, D., … & Cisternas, A. (1997). The Mw= 8.0 Antofagasta (northern Chile) earthquake of 30 July 1995: A precursor to the end of the large 1877 gap. Bulletin of the Seismological Society of America, 87(2), 427-445.

       N.14 Delouis, B., Philip, H., Dorbath, L., & Cisternas, A. (1998). Recent crustal deformation in the Antofagasta region (northern Chile) and the subduction process. Geophysical Journal International, 132(2), 302-338.

       N.15 Ewiak, O., Victor, P., & Oncken, O. (2015). Investigating multiple fault rupture at the Salar del Carmen segment of the Atacama Fault System (northern Chile): Fault scarp morphology and knickpoint analysis. Tectonics, 34(2), 187-212.

       N.16 Farías, M., Charrier, R., Comte, D., Martinod, J., & Hérail, G. (2005). Late Cenozoic deformation and uplift of the western flank of the Altiplano: Evidence from the depositional, tectonic, and geomorphologic evolution and shallow seismic activity (northern Chile at 19 30′ S). Tectonics, 24(4).

       N.17 González, G., & Carrizo, D. (2003). Segmentación, cinemática y cronología relativa de la deformación tardía de la Falla Salar del Carmen, Sistema de Fallas de Atacama,(23° 40’S), norte de Chile. Revista geológica de Chile,30(2), 223-244.

       N18 González, G., Carrizo, D., Cembrano, J., Allmendinger, R., Espina, J., & Loveless, J. (2005). Fracture propagation in the Central Andes forearc, Coastal Cordillera, Northern Chile: Insight from IKONOS data and surfaces topographic modelling.

       N.19 González, L., Dunai, T., Carrizo, D., & Allmendinger, R. (2006). Young displacements on the Atacama Fault System, northern Chile from field observations and cosmogenic 21Ne concentrations. Tectonics, 25(3).

       N.20 González, G., Cembrano, J., Aron, F., Veloso, E. E., & Shyu, J. B. H. (2009). Coeval compressional deformation and volcanism in the central Andes, case studies from northern Chile (23 S–24 S). Tectonics, 28(6).

       N.21 González, G., Cembrano, J., Carrizo, D., Macci, A., & Schneider, H. (2003). The link between forearc tectonics and Pliocene–Quaternary deformation of the Coastal Cordillera, northern Chile. Journal of South American Earth Sciences,16(5), 321-342. 

        N.22 González, G., Gerbault, M., Martinod, J., Cembrano, J., Carrizo, D., Allmendinger, R.,& Espina, J. (2008). Crack formation on top of propagating reverse faults of the Chuculay Fault System, northern Chile: Insights from field data and numerical modelling. Journal of Structural Geology, 30(6), 791-808.

       N.23 González, G., Salazar, P., Loveless, J. P., Allmendinger, R. W., Aron, F., & Shrivastava, M. (2015). Upper plate reverse fault reactivation and the unclamping of the megathrust during the 2014 northern Chile earthquake sequence. Geology, 43(8), 671-674.

       N.24 Hartley, A. J., May, G., Chong, G., Turner, P., Kape, S. J., & Jolley, E. J. (2000). Development of a continental forearc: A Cenozoic example from the Central Andes, northern Chile. Geology, 28(4), 331-334.

       N.25 Heinze, B., 2003. Active intraplate faulting in the forearc of north central Chile (30°S): implications from neotectonic field studies, GPS data, and elastic dislocation modeling. Scientifical Technical report, Geoforschungszentrum, Potsdam, Germany. 134 p

       N.26 Hervé, M. (2013). Movimiento sinistral en el Cretácico Inferior de la Zona de Falla de Atacama al Norte de Paposo (24ºS), Chile. Andean Geology, (31), 37-42.

       N.27 Legrand, et.al  (2007). Source parameters of the M w= 6.3 Aroma crustal earthquake of July 24, 2001 (northern Chile), and its aftershock sequence.Journal of south American earth sciences, 24(1), 58-68.

       N.28 Loveless, J. P., Allmendinger, R. W., Pritchard, M. E., & González, G. (2010). Normal and reverse faulting driven by the subduction zone earthquake cycle in the northern Chilean  fore-arc. Tectonics, 29(2).

       N.29 Marquardt et al., 2002. Late Quaternary slip rates of the Mejillones Fault, Northern Chile (23°S), using 10Be dates. 5th ISAG, Toulouse (France) (2002), pp. 409–412.

       N.30 Marquardt, C., Lavenu, A., Ortlieb, L., Godoy, E., & Comte, D. (2004). Coastal neotectonics in Southern Central Andes: uplift and deformation of marine terraces in Northern Chile (27 S). Tectonophysics, 394(3), 193-219.

       N.31 Naranjo, J. A. (1987). Interpretación de la actividad cenozoica superior a lo largo de la Zona de Falla Atacama, Norte de Chile. Andean Geology, (31), 43-55.

       N.32 Niemeyer, H., González, G., & Martinez-De Los Rios, E. (1996). Evolución tectónica cenozoica del margen continental activo de Antofagasta, norte de Chile. Andean Geology, 23(2), 165-186.

       N.33 Niemeyer, H., & Urrutia, C. (2010). Strike-slip along the Sierra de Varas Fault (Cordillera de Domeyko Fault-System), northern Chile. Andean Geology, 36(1), 37-50.

       N.34 Opazo Castro, E. A. (2014). Evaluación y zonificación de peligro de remociones en masa en la Ruta A-16, vía de acceso principal a la ciudad de Iquique (Región de Tarapacá).

       N.35 Pinto Morales, L. R. (2016). Determinación de efectos de sitio en las estaciones sismológicas de la región de Tarapacá.

       N.36 Santibanez, I., Cembrano, J. M., Gonzalez, G., Aron, F., & Yanez, G. A. (2013, December).Crustal Faults in the Chilean Andes: Tectonic significance and implications for geologic hazard. In AGU Fall Meeting Abstracts (Vol. 1, p. 2614).

       N.37 Shirzaei, M., Bürgmann, R., Oncken, O., Walter, T. R., Victor, P., & Ewiak, O. (2012). Response of forearc crustal faults to the megathrust earthquake cycle: InSAR evidence from Mejillones Peninsula, Northern Chile. Earth and Planetary Science Letters, 333, 157-164.