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Submitted
Dagnino D, Jiminez-Tejero CE, Ranero CR, Sallares V.  Submitted.  Comparison of Objective Functionals in Seismic Full Waveform Inversion.
2016
Biescas B, Ruddick B, Kormann J, Sallares V, Nedimović MR, Carniel S.  2016.  Synthetic Modeling for an Acoustic Exploration System for Physical Oceanography. Journal of Atmospheric and Oceanic Technology. 33:191–200.
2015
Tejero C.E.aJiménez, Dagnino D.a, Sallarès V.a, Ranero C.R.b.  2015.  Comparative study of objective functions to overcome noise and bandwidth limitations in full waveform inversion. Geophysical Journal International. 203:632–645.
Prada M.a, Sallarès V.a, Ranero C.R.b, Vendrell M.G.a, Grevemeyer I.c, Zitellini N.d, de Franco R.e.  2015.  The complex 3-D transition from continental crust to backarc magmatism and exhumed mantle in the Central Tyrrhenian basin. Geophysical Journal International. 203:63–78.
Bangs N.L.a, McIntosh K.D.a, Silver E.A.b, Kluesner J.W.b, Ranero C.R.c.  2015.  Fluid accumulation along the Costa Rica subduction thrust and development of the seismogenic zone. Journal of Geophysical Research B: Solid Earth. 120:67–86.
Hensen C, Scholz F, Nuzzo M, Valadares V, Grácia E, Terrinha P, Liebetrau V, Kaul N, Silva S, Martínez-Loriente S et al..  2015.  Strike-slip faults mediate the rise of crustal-derived fluids and mud volcanism in the deep sea. Geology. 43:339–342.
Hensen C, Scholz F, Nuzzo M, Valadares V, Grácia E, Terrinha P, Liebetrau V, Kaul N, Silva S, Martínez-Loriente S et al..  2015.  Strike-slip faults mediate the rise of crustal-derived fluids and mud volcanism in the deep sea. Geology. 43:339–342.
Hensen C, Scholz F, Nuzzo M, Valadares V, Grácia E, Terrinha P, Liebetrau V, Kaul N, Silva S, Martínez-Loriente S et al..  2015.  Strike-slip faults mediate the rise of crustal-derived fluids and mud volcanism in the deep sea. Geology. 43:339–342.
Garcia X.a, Seillé H.b, Elsenbeck J.c, Evans R.L.c, Jegen M.d, Hölz S.d, Ledo J.e, Lovatini A.f, Marti A.e, Marcuello A.e et al..  2015.  Structure of the mantle beneath the Alboran Basin from magnetotelluric soundings. Geochemistry, Geophysics, Geosystems. 16:4261–4274.
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.
2014
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.
Tejero C.EJimenez, Dagnino D., Sallarès V., Ranero C..  2014.  Comparison of objective functionals in seismic full waveform inversion. 76th European Association of Geoscientists and Engineers Conference and Exhibition 2014: Experience the Energy - Incorporating SPE EUROPEC 2014. :2819–2823.
Garcia X, Monteys X, Evans RL, Szpak M.  2014.  Constraints on a shallow offshore gas environment determined by a multidisciplinary geophysical approach: The Malin Sea, NW Ireland. Geochemistry, Geophysics, Geosystems. 15:867–885.
Papadopoulos GA, Grácia E, Urgeles R, Sallares V, De Martini PMarco, Pantosti D, González M, Yalciner AC, Mascle J, Sakellariou D et al..  2014.  Historical and pre-historical tsunamis in the Mediterranean and its connected seas: Geological signatures, generation mechanisms and coastal impacts. Marine Geology. 354:81–109.
Papadopoulos GA, Grácia E, Urgeles R, Sallares V, De Martini PMarco, Pantosti D, González M, Yalciner AC, Mascle J, Sakellariou D et al..  2014.  Historical and pre-historical tsunamis in the Mediterranean and its connected seas: Geological signatures, generation mechanisms and coastal impacts. Marine Geology. 354:81–109.
Papadopoulos GA, Grácia E, Urgeles R, Sallares V, De Martini PMarco, Pantosti D, González M, Yalciner AC, Mascle J, Sakellariou D et al..  2014.  Historical and pre-historical tsunamis in the Mediterranean and its connected seas: Geological signatures, generation mechanisms and coastal impacts. Marine Geology. 354:81–109.
Marchesini I, Mergili M, Rossi M, Santangelo M, Cardinali M, Ardizzone F, Fiorucci F, Schneider-muntau B, Fellin W, Guzzetti F.  2014.  Landslide Science for a Safer Geoenvironment. 2:483–489.
Marchesini I, Mergili M, Rossi M, Santangelo M, Cardinali M, Ardizzone F, Fiorucci F, Schneider-muntau B, Fellin W, Guzzetti F.  2014.  Landslide Science for a Safer Geoenvironment. 2:483–489.
Marchesini I, Mergili M, Rossi M, Santangelo M, Cardinali M, Ardizzone F, Fiorucci F, Schneider-muntau B, Fellin W, Guzzetti F.  2014.  Landslide Science for a Safer Geoenvironment. 2:483–489.
Garcia X., Monteys X., Evans R.L, Szpak M.T..  2014.  Near seabed geology using a multidisciplinary geophysical approach in a shallow gas environment in the Malin Sea (NW Ireland).
Biescas B, Ruddick BR, Nedimovic MR, Sallares V, Bornstein G, Mojica JF.  2014.  Recovery of temperature, salinity, and potential density from ocean reflectivity. Journal of Geophysical Research: Oceans. 119:3171–3184.
Dagnino D., Sallarès V., Ranero C.R.  2014.  Scale- and parameter-adaptive model-based gradient pre-conditioner for elastic full-waveform inversion. Geophysical Journal International. 198:1130–1142.
Martínez-Loriente S, Sallares V, Grácia E, Bartolomé R, Dañobeitia JJosé, Zitellini N.  2014.  Seismic and gravity constraints on the nature of the basement in the Africa-Eurasia plate boundary: New insights for the geodynamic evolution of the SW Iberian margin. Journal of Geophysical Research: Solid Earth. 119:127–149.
Prada M., Sallarès V., Ranero C.R, Vendrell M.G, Grevemeyer I., Zitellini N., de Franco R..  2014.  Seismic structure of the Central Tyrrhenian basin: Geophysical constraints on the nature of the main crustal domains. Journal of Geophysical Research: Solid Earth. 119:52–70.
Hensen C., Scholz F., Marianne N., Valadares V., Gràcia E., Terrinha P., Liebetrau V., Kaul N., Silva S., Martinez-Loriente S. et al..  2014.  Strike-slip Faults Mediate the Rise of Basement-Derived Fluids and Mud Volcanism in the Deep Sea.

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