@conference {Camerlenghi2010,
	title = {{A database on submarine landslides of the mediterranean sea}},
	booktitle = {Submarine Mass Movements and Their Consequences - 4th International Symposium},
	year = {2010},
	pages = {503{\textendash}513},
	publisher = {Kluwer Academic Publishers},
	organization = {Kluwer Academic Publishers},
	abstract = {Submarine landslides are ubiquitous along the continental margins of the Mediterranean basin and occur on tectonically-dominated margins as well as on passive margins and volcanic island flanks. Tectonically quiet zones seem to have the highest density of known events. Most landslides occur as long run-out distance debris flows, but slumps and deep-seated failures are also relatively common. In abyssal plains the distal product of massive failures is recorded as large megatur-bidites, while on volcanic islands the dominant failure type is flank-collapse with development of debris avalanches. Submarine landslides, excluding megaturbidites, appear to occur in all water depths between the coastline and about 2000 m. Most landslides occupy areas ranging from a few to about 600 km2 and volumes up to 220 km3. Abyssal plain megaturbidites can attain 60, 000 km2 and 1, 000 km3. The landslides headwall height are clustered around two modes: 0 to 40 m for relatively small landslides and 160 to 200 m for the largest ones. Most recorded submarine landslides are relatively young in age and several events appear to group near the Pleistocene to Holocene transition. {\textcopyright} Springer Science + Business Media B.V. 2010.},
	keywords = {Geohazard, Holocene, Mass wasting, Mediterranean, Megaturbidite, Pleistocene, Submarine landslide},
	isbn = {9789048130702},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84903488503\&partnerID=tZOtx3y1},
	author = {Camerlenghi, A. and Urgeles, R. and Fantoni, L.}
}
@booklet {LoIacono2010a,
	title = {{Very high-resolution seismo-acoustics in the study of seagrasses. The case of posidonia oceanica (Mediterranean sea)}},
	year = {2010},
	month = {mar},
	publisher = {SARTI (Technological Development Centre of Remote Acquisition and Data processing Systems)},
	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 = {{\`A}rees tem{\`a}tiques de la UPC::Enginyeria electr{\`o}nica, Holocene, Mediterranean Sea, Non linear seismo-acoustics, Seagrasses},
	url = {http://upcommons.upc.edu//handle/2099/8613},
	author = {Lo Iacono, Claudio and Gr{\'a}cia, Eul{\`a}lia and Da{\~n}obeitia, Juan Jos{\'e}}
}
