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Book Chapter
Torbahn L, Huhn K.  2014.  Submarine Mass Movements and Their Consequences. Submarine Mass Movements and Their Consequences. 37:85–94.
Mosher D.C, Moscardelli L., Shipp R.C, Chaytor J.D, Baxter C.DP, Lee H.J, Urgeles R..  2010.  Submarine mass movements and their consequences. Submarine Mass Movements and Their Consequences, Advances in Natural and Technological Hazards Research. :1–8.
Gràcia E., Bartolome R., Perea H., Moreno X., L. de la Peña G, Ranero C.R, C. Iacono L, Martinez-Loriente S., Diez S., Masana E. et al..  2014.  Seismic hazard of active faults in the Alboran Sea inferred from submarine paleosismology. Una aproximación multidisciplinar al estudio de fallas activas, los terremotos y el riesgo sísmico. :101–104.
Rebesco M, Pedrosa MT, Camerlenghi A, Lucchi RG, Sauli C, De Mol B, Madrussani G, Urgeles R, Rossi G, Böhm G.  2012.  One million years of climatic generated landslide events on the northwestern Barents Sea continental margin.. Submarine Mass Movement and Their Consequences, Advances in Natural and Technological Hazards Research. :747–756.
Iacono CLo, Gràcia EG, Bartolomé R, Coiras E, Dañobeitia JJose, Acosta J.  2012.  The habitats of the Chella Bank. Eastern Alboran Sea (Western Mediterranean). Seafloor Geomorphology as Benthic Habitat: GeoHAB Atlas of Seafloor Geomorphic Features and Benthic Habitats.. :681–690.
, Ferrater M., Perea H., Baize S., Echeverria A., Pallàs R., E. Meléndez G, -Díaz M, .J. J, Rockwell T..  2014.  Fine grained bodies as evidence of “dusty” paleoearthquakes in the Alhama de Murcia Fault geological record. Una aproximación multidisciplinar al estudio de fallas activas, los terremotos y el riesgo sísmico. :23–26.
Perea H, Gràcia E., Bartolomé R, L. de la Peña G, Martinez-Loriente S., Moreno X., De Mol B., Tello O., Ballesteros M., Party EVENT-DEEPcruise.  2014.  Evidences of quaternary active faults across the Djibouti high and the Adra Ridge (Alboran Sea). Una aproximación multidisciplinar al estudio de fallas activas, los terremotos y el riesgo sísmico. :97–100.
Perea H, Gràcia E., Bartolomé R, L. de la Peña G, Martinez-Loriente S., Moreno X., De Mol B., Tello O., Ballesteros M., Party EVENT-DEEPcruise.  2014.  Evidences of quaternary active faults across the Djibouti high and the Adra Ridge (Alboran Sea). Una aproximación multidisciplinar al estudio de fallas activas, los terremotos y el riesgo sísmico. :97–100.
Ranero C.R, von Huene R., Weinrebe W., Barckhausen U..  2007.  Convergent margin tectonics of Middle America: A marine perspective. Central America, Geology, Hazards and Resources. :239–265.
Masana E., Grácia E, Moreno X, Bartolomé R, Dañobeitia JJosé.  2013.  Characterizing the seismic potential of the Eastern Betics Shear Zone (EBSZ), a major source of earthquakes in Southeastern Iberia. Contribución de la Geología al Análisis de la Peligrosidad Sísmica. :101–104.
Martinez-Loriente S., Gràcia E, Bartolomé R, SALLARES V, Perea H.  2014.  Active faulting in the Mesozoic oceanic lithosphere offshore the SW Iberian margin. Significance for earthquake and tsunami hazard. Una aproximación multidisciplinar al estudio de fallas activas, los terremotos y el riesgo sísmico. :81–84.

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