@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.} }