The southern Tyrrhenian continental margin is the product of Pliocene–Recent back-arc extension.An area of approximately 30 km2 of gentle (about 1.5°) lower slope of the last glacial outer shelf sedimentarywedge in water depths of between 200 and 300 m failed between 14 and 11 ka BP. We approached the landslideby multibeam and sub-bottom profiler surveying, high-resolution multichannel seismics, and coring for stratigraphicand geotechnical purposes. With regard to a slope-stability analysis, we carried out an assessment of thestratigraphic and structural setting of the area of the Licosa landslide. This analysis revealed that the landslidedetached along a marker bed that was composed of the tephra layer Y-5 (c. 39 ka). Several previously unknowngeological characteristics of the area are likely to have affected the slope stability. These are the basal erosion ofthe slope in the Licosa Channel, a high sedimentation rate in the sedimentary wedge, earthquake shaking, thevolcanic ash nature of the detachment surface, subsurface gas/fluid migration, and lateral porewater flow fromthe depocentre of wedge to the base of the slope along the high-permeability ash layers. A newly discoveredprominent structural discontinuity is identified as the fault whose activity may have triggered the landslide.

Open-slope, translational submarine landslide in a tectonically active volcanic continental margin (Licosa submarine landslide, southern Tyrrhenian Sea)

Camerlenghi A.;Zgur F.;Romeo R.;
2019-01-01

Abstract

The southern Tyrrhenian continental margin is the product of Pliocene–Recent back-arc extension.An area of approximately 30 km2 of gentle (about 1.5°) lower slope of the last glacial outer shelf sedimentarywedge in water depths of between 200 and 300 m failed between 14 and 11 ka BP. We approached the landslideby multibeam and sub-bottom profiler surveying, high-resolution multichannel seismics, and coring for stratigraphicand geotechnical purposes. With regard to a slope-stability analysis, we carried out an assessment of thestratigraphic and structural setting of the area of the Licosa landslide. This analysis revealed that the landslidedetached along a marker bed that was composed of the tephra layer Y-5 (c. 39 ka). Several previously unknowngeological characteristics of the area are likely to have affected the slope stability. These are the basal erosion ofthe slope in the Licosa Channel, a high sedimentation rate in the sedimentary wedge, earthquake shaking, thevolcanic ash nature of the detachment surface, subsurface gas/fluid migration, and lateral porewater flow fromthe depocentre of wedge to the base of the slope along the high-permeability ash layers. A newly discoveredprominent structural discontinuity is identified as the fault whose activity may have triggered the landslide.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14083/1923
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