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Garcia X, Pavlidis D, Gorman GJ, Gomes JLMA, Piggott MD, Aristodemou E, Mindel J, Latham J-P, Pain CC, ApSimon H.  2011.  A two-phase adaptive finite element method for solid-fluid coupling in complex geometries. International Journal for Numerical Methods in Fluids. 66:82–96.
Goldfinger C, C. Nelson H, Morey AE, Johnson JE, Patton J, Karabanov E, Gutiérrez-Pastor J, Eriksson AT, Grácia E, Dunhill G et al..  2012.  Turbidite Event History—Methods and Implications for Holocene Paleoseismicity of the Cascadia Subduction Zone.
a Institut M, Ciències D, V De Ciències SInstitut, Icrea CRRanero.  2013.  Tu-02-13 TOMO3D - A New 3-D Joint Refraction and Reflection Travel-time Tomography Code for Active-source Seismic Data. Eage '13. :10–13.
Bartolomé R, , -Cornú N, , Alonso J.L., Cameselle A.L., Castellon A., Estrada F., Perea H., Prada M..  2014.  TSUJAL project and marine survey: Crustal characterization of the Rivera Plate-Jalisco Block boundary and its implications for seismic and tsunami hazard assessment5) TSUJAL Working Group: D. 2nd Iberian meeting on active faults and paleoseismology – IBERFAULT 2014.
Garcia X, Escribano E, Colom H, Domenech J, Queralt J.  2011.  Tricyclic Antidepressants-loaded Biodegradable PLGA Nanoparticles: In Vitro Characterization and In Vivo Analgesic and Anti-Allodynic Effect. Current Nanoscience. 7:345–353.
Amblas D, Gerber TP, Canals M, Pratson LF, Urgeles R, Lastras G, Calafat AM.  2011.  Transient erosion in the Valencia Trough turbidite systems, NW Mediterranean Basin. Geomorphology. 130:173–184.
Meléndez A.a, Korenaga J.b, Sallarès V.a, Miniussi A.c, Ranero C.R.d.  2015.  TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test. Geophysical Journal International. 203:158–174.
Rosas F.M., Duarte J.C., Neves M.C., Terrinha P., Silva S., Matias L., Gràcia E., Bartolome R..  2012.  Thrust–wrench interference between major active faults in the Gulf of Cadiz (Africa–Eurasia plate boundary, offshore SW Iberia): Tectonic implications from coupled analog and numerical modeling. Tectonophysics. 548-549:1–21.
J. Moore C, R. Urgeles R, Conin M, Flemings PB, Iturrino GJ.  2011.  Threshold of borehole failure: Breaking in before breaking out, Mississippi fan, Gulf of Mexico. Geosphere. 7:684–693.
Latham J-P, Munjiza A, Garcia X, Xiang J, Guises R.  2008.  Three-dimensional particle shape acquisition and use of shape library for DEM and FEM/DEM simulation. Minerals Engineering. 21:797–805.
Harris RN, Spinelli G, Ranero CR, Grevemeyer I, Villinger H, Barckhausen U.  2010.  Thermal regime of the Costa Rican convergent margin: 2. Thermal models of the shallow Middle America subduction zone offshore Costa Rica. Geochemistry, Geophysics, Geosystems. 11:n/a–n/a.
Harris RN, Grevemeyer I, Ranero CR, Villinger H, Barckhausen U, Henke T, Mueller C, Neben S.  2010.  Thermal regime of the Costa Rican convergent margin: 1. Along-strike variations in heat flow from probe measurements and estimated from bottom-simulating reflectors. Geochemistry, Geophysics, Geosystems. 11:n/a–n/a.
Ranero C.R, Sallarès V., Zitellini N., Grevemeyer I., Guzman M., Prada M., Moeller S., de Franco R..  2012.  The tectonic structure of the Tyrrhenian Basin, a complex interaction among faulting and magmatism. Rendiconti Online Societa Geologica Italiana. 21:251–252.
Gutscher M-A, Dominguez S, Westbrook GK, Gente P, Babonneau N, Mulder T, Gonthier E, Bartolomé R, Luis J, Rosas F et al..  2009.  Tectonic shortening and gravitational spreading in the Gulf of Cadiz accretionary wedge: Observations from multi-beam bathymetry and seismic profiling. Marine and Petroleum Geology. 26:647–659.
Simancas JFernando, Azor A, Martínez-Poyatos D, Tahiri A, Hadi HEl, González-Lodeiro F, Pérez-Estaún A, Carbonell R.  2009.  Tectonic relationships of Southwest Iberia with the allochthons of Northwest Iberia and the Moroccan Variscides. Comptes Rendus Geoscience. 341:103–113.
L. de la Peña G, Ranero C.R., Gràcia E., R. B, Party TMcruise.  2014.  Técnicas avanzadas de procesado de datos de sísmica de reflexión multicanal aplicadas a mejorar la visualización de fallas activas del Mar de Alborán. Una aproximación multidisciplinar al estudio de fallas activas, los terremotos y el riesgo sísmico. :229–232.