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dc.contributor.authorHarders, Rieka-
dc.contributor.authorRanero, César R.-
dc.contributor.authorWeinrebe, Wilhelm-
dc.date.issued2013-09-24-
dc.identifier.citation6th International Symposium on Submarine Mass Movements and Their Consequences - Book of abstracts: 19 (2013)es_ES
dc.identifier.urihttp://hdl.handle.net/10261/98358-
dc.description6th International Symposium on Submarine Mass Movements and Their Consequences (ISSMMTC), 23-25 September 2013, Kiel, Germanyes_ES
dc.description.abstractOffshore Costa Rica large seamounts under thrust the continental convergent margin causing slides of complex morphology. The large dimension of the structures has attracted previous investigations and their basic characteristics are known. However, no detailed mapping of their complex morphology has been reported. Here we present a detailed mapping of the failure-related structures and deposits. We use deep-towed sidescan sonar data, aided by multibeam bathymetry to analyze their geometry, geomorphologic character, backscatter intensity, and spatial distribution. Those observations are used to analyze the relationship between landslide characteristics and abundance, to the changes in the style of deformation caused by the subduction of seamounts to progressively greater depth under the margines_ES
dc.language.isoenges_ES
dc.rightsclosedAccesses_ES
dc.titleCharacterization of submarine landslide complexes offshore Costa Rica: An evolutionary model related to seamount subductiones_ES
dc.typeComunicación de congresoes_ES
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://conferences.geomar.de/conferenceDisplay.py?confId=0es_ES
dc.relation.csices_ES
Aparece en las colecciones: (ICM) Comunicaciones congresos
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