@article {ferraterprimeros,
	title = {{PRIMEROS VALORES DE VELOCIDAD DE DESLIZAMIENTO LATERAL EN LA FALLA ALHAMA DE MURCIA BASADOS EN TRINCHERAS 3D}},
	journal = {Segunda reuni{\'o}n Ib{\'e}rica sobre fallas activas y paleosismolog{\'\i}a},
	year = {2014},
	pages = {19},
	author = {Ferrater, M and Ortu{\~n}o, M and Masana, E and Perea, H and Baize, S and Mart{\'\i}nez-D{\'\i}az, J J and Pall{\`a}s, R and Garc{\'\i}a-Mel{\'e}ndez, E}
}
@article {Lucchi2013,
	title = {{Postglacial sedimentary processes on the Storfjorden and Kveithola trough mouth fans: Significance of extreme glacimarine sedimentation}},
	journal = {Global and Planetary Change},
	volume = {111},
	year = {2013},
	month = {dec},
	pages = {309{\textendash}326},
	abstract = {The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the northwestern Barents Sea has been investigated within two coordinated Spanish and Italian projects in the framework of the International Polar Year (IPY) Activity 367, NICE STREAMS. The investigation has been conducted using a multidisciplinary approach to the study of sediment cores positioned on high-resolution multibeam bathymetry and TOPAS/CHIRP sub-bottom profiles.Core correlation and the age model were based on 27 AMS 14C samples, rock magnetic parameters, lithofacies sequences, and the presence of marker beds including two oxidized layers marking the post Last Glacial Maximum (LGM) inception of deglaciation (OX-2) and the Younger Dryas cold climatic event (OX-1).Sediment facies analysis allowed the distinction of a number of depositional processes whose onset appears closely related to ice stream dynamics and oceanographic patterns in response to climate change. The glacigenic diamicton with low water content, high density, and high shear strength, deposited during glacial maxima, indicates ice streams grounded at the shelf edge. Massive release of IRD occurred at the inception of deglaciation in response to increased calving rates with possible outer ice streams lift off and collapse. The presence of a several-meter-thick sequence of interlaminated sediments deposited by subglacial outbursts of turbid meltwater (plumites) indicates rapid ice streams{\textquoteright} melting and retreat. Crudely-layered and heavily-bioturbated sediments were deposited by contour currents under climatic/environmental conditions favorable to bioproductivity.The extreme sedimentation rate of 3.4cma-1 calculated for the plumites from the upper-slope area indicates a massive, nearly instantaneous (less than 150years), terrigenous input corresponding to an outstanding meltwater event. We propose these interlaminated sediments to represent the high-latitude marine record of MeltWater Pulse 1a (MWP-1a). Different bathymetric and oceanographic conditions controlled locally the mode of glacial retreat, resulting in different thickness of plumites on the upper continental slope of the Storfjorden and Kveithola TMFs. It is possible that the southern part of Storfjorden TMF received additional sediments from the deglaciation of the neighboring Kveithola ice stream. {\textcopyright} 2013.},
	keywords = {Barents Sea, Gullies, LGM, Meltwater plumes, MWP-1a, Sedimentary processes},
	issn = {09218181},
	doi = {10.1016/j.gloplacha.2013.10.008},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84887563264\&partnerID=tZOtx3y1},
	author = {Lucchi, R.G. and Camerlenghi, A. and Rebesco, M. and Colmenero-Hidalgo, E. and Sierro, F.J. and Sagnotti, L. and Urgeles, R. and Melis, R. and Morigi, C. and B{\'a}rcena, M.-A. and Giorgetti, G. and Villa, G. and Persico, D. and Flores, J.-A. and Rigual-Hern{\'a}ndez, A.S. and Pedrosa, M.T. and Macri, P. and Caburlotto, A.}
}
@article {E.Gracia2013,
	title = {{Preface: Marine and Lake Paleoseismology}},
	journal = {Natural Hazards and Earth System Science},
	volume = {13},
	number = {12},
	year = {2013},
	month = {dec},
	pages = {3469{\textendash}3478},
	abstract = {This special issue of Natural Hazards and Earth System Sciences (NHESS) contains 16 papers that resulted from the European Science Foundation (ESF) Research Conference "Submarine Paleoseismology: The Offshore Search of Large Holocene Earthquakes" that was held at the Universit{\"a}tszentrum Obergurgl (Austria), from 11 to 16 September 2010 (Pantosti et al., 2011). The conference enabled scientists from a number of existing lines of research to give an official start and international recognition to subaqueous paleoseismology. The scope of this Special Issue is built on the content of the ESF conference and includes different aspects of marine and lake paleoseismology. The 16 papers are separated into two main groups, namely, on-fault or off-fault paleoseismic studies. On-fault paleoseismology focuses on the observation, measurement and quantification of history of movements along the fault plane, where direct evidence of earthquake activity includes displacement of sediment strata and landforms such as seafloor scarps (Argnani et al., 2012; Beck et al., 2012; Gr{\`a}cia et al., 2012; Perea et al., 2012; Polonia et al., 2012). Off-fault paleoseismology uses the sedimentary record to identify deposits generated, directly or indirectly by seismic activity, such as mass-transport deposits, turbidites and tsunamites (Drab et al., 2012; Morey et al., 2013; Cattaneo et al., 2012; Gerardi et al., 2012; Goldfinger et al., 2013b; Langridge et al., 2012; Nelson et al., 2012; Patton et al., 2013; Pouderoux et al., 2012a; Smedile et al., 2012; Vacchi et al., 2012). {\textcopyright} 2013 Author(s).},
	issn = {1684-9981},
	doi = {10.5194/nhess-13-3469-2013},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84891048700\&partnerID=tZOtx3y1},
	author = {E. Gr{\`a}cia, E. and Lamarche, G. and Nelson, H. and Pantosti, D.}
}
@booklet {Martinez-Loriente2013a,
	title = {{Pre-stack depth migration seismic imaging of the Coral Patch Ridge and adjacent Horseshoe and Seine Abyssal Plains (Gulf of Cadiz): tectonic implications}},
	year = {2013},
	month = {apr},
	publisher = {Universidad de Oviedo},
	abstract = {Peer Reviewed},
	url = {http://digital.csic.es/handle/10261/75234},
	author = {Martinez-Loriente, S. and Gr{\'a}cia, Eul{\`a}lia and Bartolom{\'e}, Rafael and Klaeschen, D. and Vizcaino, A. and Sallares, Valenti and Da{\~n}obeitia, Juan Jos{\'e} and Zitellini, N.}
}
@conference {DeLaPuente2010,
	title = {{The potential of discontinuous Galerkin methods for full waveform tomography}},
	booktitle = {72nd European Association of Geoscientists and Engineers Conference and Exhibition 2010: A New Spring for Geoscience. Incorporating SPE EUROPEC 2010},
	volume = {6},
	year = {2010},
	pages = {4144{\textendash}4148},
	abstract = {We present a discontinuous Galerkin solver for Full Waveform Tomography applications in seismic exploration. We discuss the advantages and drawbacks of using unstructured meshes in the model discretization and present a numerical example. {\textcopyright} 2010, European Association of Geoscientists and Engineers.},
	isbn = {9781617386671},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-78249285605\&partnerID=tZOtx3y1},
	author = {De La Puente, J. and Sallar{\`e}s, V. and Ranero, C. R.}
}
@booklet {MorenoMota2009,
	title = {{Paleoseismology of active faults based on multiscale seismic imaging}},
	journal = {Instrumentation ViewPoint},
	number = {8},
	year = {2009},
	pages = {50{\textendash}51},
	publisher = {Universitat Polit{\`e}cnica de Catalunya},
	abstract = {The study of active structures offshore requires very-high resolution seismic imaging in order to observe the most recent layers below sea floor. In the other hand, high penetration methods are necessary to observe deeper reflections for understanding the evolution of the structure throughout the time. The aim of our study is to establish the seismic potential of the offshore segment of the Carboneras Fault, Eastern Betics, based on multiscale seismic imaging. Three different scale methods have been acquired and are compared here: very-high-resolution sub-bottom profiler TOPAS, very-high-resolution single-channel seismic (Sparker) and high-resolution multi-channel seismic. From seismic profiles, faulted Quaternary layers suggest that the Carboneras Fault is active. Sediment coring and dating analysis are used to consider ages for key reflectors observed in TOPAS profiles, and a change in the vertical slip-rate through the Quaternary is inferred.},
	keywords = {Tecnolog{\'\i}a industrial. Tecnolog{\'\i}a mec{\'a}nica, Tecnolog{\'\i}as},
	issn = {1886-4864},
	url = {http://dialnet.unirioja.es/servlet/articulo?codigo=3202510\&info=resumen\&idioma=ENG},
	author = {Moreno Mota, Ximena and Gr{\`a}cia i Mont, Eulalia and Bartolom{\'e}, Rafael and Iacono, Claudio}
}
@article {Secanell2008,
	title = {{Probabilistic seismic hazard assessment of the Pyrenean region}},
	journal = {Journal of Seismology},
	volume = {12},
	number = {3},
	year = {2008},
	month = {mar},
	pages = {323{\textendash}341},
	abstract = {A unified probabilistic seismic hazard assessment (PSHA) for the Pyrenean region has been performed by an international team composed of experts from Spain and France during the Interreg IIIA ISARD project. It is motivated by incoherencies between the seismic hazard zonations of the design codes of France and Spain and by the need for input data to be used to define earthquake scenarios. A great effort was invested in the homogenisation of the input data. All existing seismic data are collected in a database and lead to a unified catalogue using a local magnitude scale. PSHA has been performed using logic trees combined with Monte Carlo simulations to account for both epistemic and aleatory uncertainties. As an alternative to hazard calculation based on seismic sources zone models, a zoneless method is also used to produce a hazard map less dependant on zone boundaries. Two seismogenic source models were defined to take into account the different interpretations existing among specialists. A new regional ground-motion prediction equation based on regional data has been proposed. It was used in combination with published ground-motion prediction equations derived using European and Mediterranean data. The application of this methodology leads to the definition of seismic hazard maps for 475- and 1,975-year return periods for spectral accelerations at periods of 0 (corresponding to peak ground acceleration), 0.1, 0.3, 0.6, 1 and 2 s. Median and percentiles 15\% and 85\% acceleration contour lines are represented. Finally, the seismic catalogue is used to produce a map of the maximum acceleration expected for comparison with the probabilistic hazard maps. The hazard maps are produced using a grid of 0.1{\textdegree}. The results obtained may be useful for civil protection and risk prevention purposes in France, Spain and Andorra. {\textcopyright} Springer Science+Business Media B.V. 2008.},
	keywords = {Andorra, France, Monte Carlo, Probabilistic, Seismic hazard, Seismic zonation, Spain},
	issn = {1383-4649},
	doi = {10.1007/s10950-008-9094-2},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-46349102115\&partnerID=tZOtx3y1},
	author = {Secanell, R. and Bertil, D. and Martin, C. and Goula, X. and Susagna, T. and Tapia, M. and Dominique, P. and Carbon, D. and Fleta, J.}
}
@article {Grevemeyer2007,
	title = {{Passive and active seismological study of bending-related faulting and mantle serpentinization at the Middle America trench}},
	journal = {Earth and Planetary Science Letters},
	volume = {258},
	number = {3-4},
	year = {2007},
	month = {jun},
	pages = {528{\textendash}542},
	abstract = {Water transported within the subducting oceanic lithosphere into the Earth{\textquoteright}s interior affects a wealth of subduction zone processes, including intraslab earthquakes and arc magmatism. In recent years growing evidence suggests that much of the hydration of oceanic plates occurs at the trench-ocean slope right before subduction. Here, normal faults are created while the rigid lithosphere bends into the trench. Offshore of Middle America, multi-channel seismic reflection imaging suggests that bending-related faults cut into the uppermost mantle, providing a mechanism for hydration and transformation of mantle peridotites into serpentinites. Seismic wide-angle reflection and refraction data were collected coincident with one of the seismic profiles where the faults have been imaged. Travel time inversion provides evidence that both crustal and uppermost mantle velocities are reduced with respect to the velocity structure found in mature oceanic crust away from deep-sea trenches. If mantle velocity reduction is solely produced by hydration, velocities indicate 10-15\% of serpentinization in the uppermost 3~km of the mantle, where seismic data provide enough resolution. A small network of ocean bottom hydrophones, deployed for about a month, detected \~{} 3 local micro earthquakes per day. Earthquake epicentres align with fault scarps at the seafloor and continuous earthquake activity might be an important process to facilitate the percolation of seawater into the upper mantle. {\textcopyright} 2007 Elsevier B.V. All rights reserved.},
	keywords = {bending-related normal faulting, earthquakes, global water cycle, seismic refraction, serpentinization, subduction},
	issn = {0012821X},
	doi = {10.1016/j.epsl.2007.04.013},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-34249911517\&partnerID=tZOtx3y1},
	author = {Grevemeyer, Ingo and Ranero, Cesar R. and Flueh, Ernst R. and Kl{\"a}schen, Dirk and Bialas, J{\"o}rg}
}
