Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/16904
Title: Slope instability along the northeastern Iberian and Balearic continental margins
Author: Lastras Membrive, Galderic
Canals Artigas, Miquel
Amblàs i Novellas, David
Frigola Ferrer, Jaime I.
Urgeles Esclasans, Roger
Calafat Frau, Antoni
Acosta, Juan, 1949-
Keywords: Estratigrafia sísmica
Mediterrània, Mar
Seismic stratigraphy
Mediterranean Sea
Issue Date: 2007
Publisher: Universitat de Barcelona (UB). Institut de Ciències de la Terra Jaume Almera (ICTJA). Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDEA). Universitat Autonònoma de Barcelona (UAB). Consejo Superior de Investigaciones Científicas (CSIC)
Abstract: This paper gathers the available information on submarine landslides identified in the northeastern Iberian continental margin and presents new data on both already known landslides and new, previously unknown ones. The 2,000 km2, 26 km3 resulting deposit of the BIG'95 debris flow in the Ebro margin; the 4 up to 16 km2, 0.4 km3 Eivissa slides in the Eivissa Channel; the 2 up to 65.6 km2, 1.46 km3 Barcelona slides in the shallow southern Catalan margin; and the western Gulf of Lions debris flow in the deep north Catalan margin are presented. This compilation is completed with several other previously undescribed small-scale mass-wasting deposits together with those observed in the Balearic Promontory. The amount and widespreading of submarine landslide deposits in the northern Iberian margins demonstrate that these margins are not an exception to the common occurence of these kind of structures worldwide, and give an idea on these phenomena recurrence even in margins considered moderately quiet, in terms of seismicity.
Note: Reproducció del document publicat a http://www.geologica-acta.com/pdf/vol0501a04.pdf
It is part of: Geologica Acta, 2007, vol. 5, núm. 1, p. 35-47
URI: http://hdl.handle.net/2445/16904
ISSN: 1695-6133
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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