@inbook {GraciaE.BartolomeR.PereaH.MorenoX.GomezdelaPenaL.RaneroC.RLoIaconoC.Martinez-LorienteS.DiezS.MasanaE.Danobeitia2014,
	title = {{Seismic hazard of active faults in the Alboran Sea inferred from submarine paleosismology}},
	booktitle = {Una aproximaci{\'o}n multidisciplinar al estudio de fallas activas, los terremotos y el riesgo s{\'\i}smico},
	year = {2014},
	pages = {101{\textendash}104},
	isbn = {978-84-617-2049-1},
	url = {http://www.researchgate.net/publication/267574309\_Una\_aproximacin\_multidisciplinar\_al\_estudio\_de\_las\_fallas\_activas\_los\_terremotos\_y\_el\_riesgo\_ssmico},
	author = {Gr{\`a}cia, E. and Bartolome, R. and Perea, H. and Moreno, X. and G{\'o}mez de la Pe{\~n}a, L. and Ranero, C.R and Lo Iacono, C. and Martinez-Loriente, S. and Diez, S. and Masana, E. and Da{\~n}obeitia, J.}
}
@inbook {Masana2013a,
	title = {{Characterizing the seismic potential of the Eastern Betics Shear Zone (EBSZ), a major source of earthquakes in Southeastern Iberia}},
	booktitle = {Contribuci{\'o}n de la Geolog{\'\i}a al An{\'a}lisis de la Peligrosidad S{\'\i}smica},
	year = {2013},
	month = {nov},
	pages = {101{\textendash}104},
	abstract = {Masana, E. ... et al.{\textendash} Primera Reuni{\'o}n Ib{\'e}rica sobre Fallas Activas y Paleosismolog{\'\i}a. Sig{\"u}enza, Guadalajara, Espa{\~n}a, 27-29 de Octubre de 2010.{\textendash} 4 pages, 1 figure},
	isbn = {978-84-693-6088-0},
	url = {http://hdl.handle.net/10261/82453},
	author = {Masana, E. and Gr{\'a}cia, Eul{\`a}lia and Moreno, Ximena and Bartolom{\'e}, Rafael and Da{\~n}obeitia, Juan Jos{\'e}}
}
@booklet {Bartolome2013,
	title = {{Seismic imaging of active faults in the Southern Alboran Sea (SE Iberian Margin): First results of the 2010 EVENT-DEEP cruise}},
	year = {2013},
	month = {sep},
	abstract = {Primera Reuni{\'o}n Ib{\'e}rica sobre Fallas Activas y Paleosismolog{\'\i}a. Sig{\"u}enza (Guadalajara, Espa{\~n}a) 27, 28 y 29 de Octubre de 2010.{\textendash} 4 pages, 4 figures},
	isbn = {isbn: 978-84-693-6088-0},
	url = {http://digital.csic.es/handle/10261/82462},
	author = {Bartolom{\'e}, Rafael and Gr{\'a}cia, Eul{\`a}lia and Lo Iacono, Claudio and Martinez-Loriente, S. and Moreno, Ximena and Perea, Hector and Masana, E. and Team, EVENT-DEEP}
}
@article {Gracia2012a,
	title = {{Acoustic and seismic imaging of the Adra Fault (NE Alboran Sea): in search of the source of the 1910 Adra earthquake}},
	journal = {Natural Hazards and Earth System Science},
	volume = {12},
	number = {11},
	year = {2012},
	month = {nov},
	pages = {3255{\textendash}3267},
	publisher = {European Geosciences Union},
	abstract = {Recently acquired swath-bathymetry data and high-resolution seismic reflection profiles offshore Adra (Almer{\'\i}a, Spain) reveal the surficial expression of a NW-SE trending 20 km-long fault, which we termed the Adra Fault. Seismic imaging across the structure depicts a sub-vertical fault reaching the seafloor surface and slightly dipping to the NE showing an along-axis structural variability. Our new data suggest normal displacement of the uppermost units with probably a lateral component. Radiocarbon dating of a gravity core located in the area indicates that seafloor sediments are of Holocene age, suggesting present-day tectonic activity. The NE Alboran Sea area is characterized by significant low-magnitude earthquakes and by historical records of moderate magnitude, such as the Mw Combining double low line 6.1 1910 Adra Earthquake. The location, dimension and kinematics of the Adra Fault agree with the fault solution and magnitude of the 1910 Adra Earthquake, whose moment tensor analysis indicates normal-dextral motion. The fault seismic parameters indicate that the Adra Fault is a potential source of large magnitude (Mw <= 6.5) earthquakes, which represents an unreported seismic hazard for the neighbouring coastal areas.{\textcopyright} 2013 IEEE.},
	issn = {1684-9981},
	doi = {10.5194/nhess-12-3255-2012},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84881091009\&partnerID=tZOtx3y1 http://digital.csic.es/handle/10261/64147},
	author = {Gr{\`a}cia, E. and Bartolome, R. and Lo Iacono, C. and Moreno, X. and Stich, D. and Mart{\'\i}nez-Diaz, J. J. and Bozzano, G. and Martinez-Loriente, S. and Perea, H. and Diez, S. and Masana, E. and Danobeitia, J. J. and Tello, O. and Sanz, J. L. and Carre{\~n}o, E.}
}
@article {Perea2012a,
	title = {{An active zone characterized by slow normal faults, the northwestern margin of the Val{\`e}ncia trough (NE Iberia): a review}},
	journal = {Journal of Iberian Geology},
	volume = {38},
	number = {1},
	year = {2012},
	month = {sep},
	pages = {35{\textendash}57},
	abstract = {The northwestern margin of the Valencia trough is an area of low strain characterized by slow normal faults and low to moderate seismicity. Since the mid 1990s this area has been the subject of a number of studies on active tectonic which have proposed different approaches to the location of active faults and to the calculation of the parameters that describe their seismic cycle. Fifty-six active faults have been found and a classification has been made in accordance with their characteristics: a) faults with clear evidence of large paleo-, historic or instrumental earthquakes (2/56); b) faults with evidence of accumulated activity during the Plio-Quaternary and with associated instrumental seismicity (7/56); c) faults with evidence of accumulated activity during the Plio-Quaternary and without associated instrumental seismicity (17/56); d) faults with associated instrumental seismicity and without evidence of accumulated activity during the Plio-Quaternary (30/56), and e) faults without evidence of activity or inactive faults. The parameters that describe the seismic cycle of these faults have been evaluated by different methods that use the geological data obtained for each fault except when paleoseismological studies were available. This classification can be applied to other areas with low slip faults because of the simplicity of the approaches adopted. This study reviews the different approaches proposed and describes the active faults located, highlighting the need a) to better understand active faults in slow strain zones through paleoseismological studies, and b) to include them in seismic hazard studies.},
	keywords = {Active faults, Active tectonics, Iberian peninsula, Paleoseismology, Seismic cycle, Val{\`e}ncia trough},
	issn = {1886-7995},
	doi = {10.5209/rev\_JIGE.2012.v38.n1.39204},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84861786693\&partnerID=tZOtx3y1},
	author = {Perea, H. and Masana, E. and Santanach, P.}
}
@article {Garcia-Mayordomo2012,
	title = {{The Quaternary Active Faults Database of Iberia (QAFI v.2.0)}},
	journal = {Journal of Iberian Geology},
	volume = {38},
	number = {1},
	year = {2012},
	month = {sep},
	pages = {301{\textendash}318},
	abstract = {The Quaternary Active Faults Database of Iberia (QAFI) is an initiative lead by the Institute of Geology and Mines of Spain (Instituto Geol{\'o}gico y Minero de Espa{\~n}a, IGME) for building a public repository of scientific data regarding faults having documented activity during the last 2.59 Ma (Quaternary). QAFI also addresses a need to transfer geologic knowledge to practitioners of seismic hazard and risk in Iberia by identifying and characterizing seismogenic fault-sources. QAFI is populated by the information freely provided by more than 40 Earth science researchers, storing to date a total of 262 records. In this article we describe the development and evolution of the database, as well as its internal architecture. Additionally, a first global analysis of the data is provided with a special focus on length and slip-rate fault parameters. Finally, the database completeness and the internal consistency of the data are discussed. Even though QAFI v.2.0 is the most current resource for calculating fault-related seismic hazard in Iberia, the database is still incomplete and requires further review.},
	keywords = {Active fault, Iberia, Portugal, Quaternary, Seismic hazard, Spain},
	issn = {1886-7995},
	doi = {10.5209/rev\_JIGE.2012.v38.n1.39219},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84861912592\&partnerID=tZOtx3y1},
	author = {Garc{\'\i}a-Mayordomo, J. and Insua-Ar{\'e}valo, J.M. and Mart{\'\i}nez-D{\'\i}az, J.J. and Jim{\'e}nez-D{\'\i}az, A. and Mart{\'\i}n-Banda, R. and Mart{\'\i}n-Alfageme, S. and {\'A}lvarez-G{\'o}mez, J.A. and Rodr{\'\i}guez-Peces, M. and P{\'e}rez-L{\'o}pez, R. and Rodr{\'\i}guez-Pascua, M.A. and Masana, E. and Perea, H. and Mart{\'\i}n-Gonz{\'a}lez, F. and Giner-Robles, J. and Nemser, E.S. and Cabral, J.}
}
@article {Perea2012,
	title = {{Quaternary active tectonic structures in the offshore Bajo Segura basin (SE Iberian Peninsula {\textendash} Mediterranean Sea)}},
	journal = {Natural Hazards and Earth System Science},
	volume = {12},
	number = {10},
	year = {2012},
	month = {oct},
	pages = {3151{\textendash}3168},
	abstract = {The Bajo Segura fault zone (BSFZ) is the northern terminal splay of the Eastern Betic shear zone (EBSZ), a large left-lateral strike-slip fault system of sigmoid geometry stretching more than 450 km from Alicante to Almera. The BSFZ extends from the onshore Bajo Segura basin further into the Mediterranean Sea and shows a moderate instrumental seismic activity characterized by small earthquakes. Nevertheless, the zone was affected by large historical earthquakes of which the largest was the 1829 Torrevieja earthquake (<I>I</ I>EMS98 X). The onshore area of the BSFZ is marked by active transpressive structures (faults and folds), whereas the offshore area has been scarcely explored from the tectonic point of view. During the EVENT-SHELF cruise, a total of 10 high-resolution single-channel seismic sparker profiles were obtained along and across the offshore Bajo Segura basin. Analysis of these profiles resulted in (a) the identification of 6 Quaternary seismo-stratigraphic units bounded by five horizons corresponding to regional erosional surfaces related to global sea level lowstands; and (b) the mapping of the active sub-seafloor structures and their correlation with those described onshore. Moreover, the results suggest that the Bajo Segura blind thrust fault or the Torrevieja left-lateral strike-slip fault, with prolongation offshore, could be considered as the source of the 1829 Torrevieja earthquake. These data improve our understanding of present deformation along the BSFZ and provide new insights into the seismic hazard in the area. {\textcopyright} 2012. Author(s) CC Attribution 3.0 License.},
	issn = {1684-9981},
	doi = {10.5194/nhess-12-3151-2012},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84867926421\&partnerID=tZOtx3y1},
	author = {Perea, H. and Gr{\`a}cia, E. and Alfaro, P. and Bartolome, R. and Lo Iacono, C. and Moreno, X. and Masana, E.}
}
@article {Nemser,
	title = {{Compilation of parameterized seismogenic sources in Iberia for the SHARE European-scale seismic source model.}},
	year = {2010},
	pages = {201{\textendash}204},
	keywords = {Database, Fault, Seismogenic, SHARE},
	isbn = {978-84-693-6088-0},
	url = {https://dspace.uevora.pt/rdpc/handle/10174/6247},
	author = {Nemser, E.S. and Garc{\'\i}a-Mayordomo, J. and Cabral, J. and Fonseca, J. and Mart{\'\i}nez-D{\'\i}az, J.J. and Alfaro Garc{\'\i}a, P. and {\`A}lvarez G{\'o}mez, J.A. and Atakan, K. and Aza{\~n}{\'o}n Hern{\'a}ndez, J.M. and Basili, R. and Besana-Ostman, G.M. and Bezzeghoud, M. and Borges, J.F. and Brum da Silveira, A. and Carlos Lopes, F. and Carvalho, J. and Dias, R.P. and Figueiredo, P.M. and Garc{\'\i}a Fern{\'a}ndez, M. and Giner Robles, J. and Gonzalez, A. and Gr{\`a}cia, E. and Gutierrez, F. and Insua Ar{\'e}valo, J.M. and Jim{\'e}nez, M.J. and Jim{\'e}nez-D{\'\i}az, A. and Lafuente Tom{\'a}s, P. and Lucha, P. and Madeira, J. and Martin Gonz{\'a}lez, F. and Masana, E. and Matias, L. and Moreno, X. and Ortu{\~n}o, M. and Perea, H. and P{\'e}rez L{\'o}pez, R. and Rodr{\'\i}guez Pascua, M.A. and Ruano, P. and Santanach, P. and Sanz de Galdeano, C. and Silva Barroso, P. and Silva, S. and Sim{\'o}n, J.L. and Terrinha, P. and Vilanova, S. and Villamor, P. and Wong, J.}
}
@booklet {Perea2013,
	title = {{Structure and Potential Seismogenic Sources of the Offshore Bajo Segura Fault Zone, Se Iberian Peninsula (Mediterranean Sea). Looking for the Source of the 1829 Torrevieja Earthquake}},
	journal = {Res{\'u}menes de la 1{\textordfeminine} Reuni{\'o}n Ib{\'e}rica sobre Fallas Activas y Paleosismolog{\'\i}a, Sig{\"u}enza, Espa{\~n}a},
	year = {2010},
	month = {sep},
	pages = {113{\textendash}116},
	abstract = {Primera Reuni{\'o}n Ib{\'e}rica sobre Fallas Activas y Paleosismolog{\'\i}a. Sig{\"u}enza (Guadalajara, Espa{\~n}a) 27, 28 y 29 de Octubre de 2010.{\textendash} 4 pages, 4 figures},
	keywords = {abstract, almost a, bajo segura, been extensively studied, betic shear zone and, bsfz, complete lack of information, during the event-shelf cruise, extends further, fallas activas, from a tectonic point, geolog{\'\i}a marina, into the mediterranean sea, is the northern terminal, of the bsfz has, of view, splay of the eastern, tect{\'o}nica activa, ten high-resolution seismic profiles, the bajo segura fault, the offshore zone has, whereas the onshore zone, zone},
	isbn = {isbn: 978-84-693-6088-0},
	url = {http://digital.csic.es/handle/10261/82456},
	author = {Perea, H. and Gr{\`a}cia, E. and Bartolom{\'e}, Rafael and Iacono, Claudio Lo and Masana, E.}
}
