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A
Gràcia E., Bartolome R., C. Iacono L, Moreno X., Stich D., Martínez-Diaz J.J, Bozzano G., Martinez-Loriente S., Perea H., Diez S. et al..  2012.  Acoustic and seismic imaging of the Adra Fault (NE Alboran Sea): in search of the source of the 1910 Adra earthquake. Natural Hazards and Earth System Science. 12:3255–3267.
Martínez-Loriente S, Grácia E, Bartolomé R, Sallares V, Connors C, Perea H, Iacono CLo, Klaeschen D, Terrinha P, Dañobeitia JJosé et al..  2013.  Active deformation in old oceanic lithosphere and significance for earthquake hazard: Seismic imaging of the Coral Patch Ridge area and neighboring abyssal plains (SW Iberian Margin). Geochemistry, Geophysics, Geosystems. 14:2206–2231.
de la Puente J, Käser M, Dumbser M, Igel H.  2007.  An arbitrary high-order discontinuous Galerkin method for elastic waves on unstructured meshes - IV. Anisotropy. Geophysical Journal International. 169:1210–1228.
Käser M, Dumbser M, de la Puente J, Igel H.  2007.  An arbitrary high-order Discontinuous Galerkin method for elastic waves on unstructured meshes - III. Viscoelastic attenuation. Geophysical Journal International. 168:224–242.
Coiras E, Iacono CLo, Grácia E, Dañobeitia J, Sanz JLuis.  2011.  Automatic Segmentation of Multi-Beam Data for Predictive Mapping of Benthic Habitats on the Chella Seamount (North-Eastern Alboran Sea, Western Mediterranean). IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing. 4:809–813.
H
Iacono CLo, Orejas C, Gori A, Gili JMaria, Requena S, Puig P, Ribó M.  2012.  The habitats of the Cap de Creus continental shelf and Cap de Creus Canyon, northwestern Mediterranean. Seafloor Geomorphology as Benthic Habitat. GeoHab Atlas of seafloor geomorphic features and benthic habitats. :457–469.
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.

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