Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/32408
Title: The El Masnou Infralittoral sedimentary environment (Barcelona province, NW Mediterranean Sea): morphology and Holocene seismic stratigraphy
Author: Ercilla, Gemma
Estrada Llàcer, Ferran
Casas Layola, David
Durán, Ruth
Nuez, Marta
Alonso, Belén (Alonso Martínez)
Farran Vert, Marcel·lí
Keywords: Estratigrafia sísmica
Holocè
Litoral
Masnou (Catalunya)
Seismic stratigraphy
Holocene
Seashore
Masnou (Catalonia)
Issue Date: Mar-2009
Publisher: Consejo Superior de Investigaciones Científicas (CSIC)
Abstract: A detailed analysis of the morphology and the Holocene seismic and sequence stratigraphy and architecture of the infralittoral sedimentary environment of the El Masnou coast (Catalonia, NW Mediterranean Sea) was carried out using multibeam bathymetry and GeoPulse seismic data. This environment extends down to 26-30 m water depth, and is defined morphologically by two depositional wedges whose seafloor is affected by erosive furrows, slides, fields of large- and small-scale wavy bedforms, and dredging trenches and pits. Erosive terraces are also identified in the transition domain toward the inner continental shelf. The Holocene stratigraphy of the infralittoral environment is defined by two major seismic sequences (lower and upper), each one formed by internal seismic units. The sequences and units are characterised by downlapping surfaces made up of deposits formed by progradation of coastal lithosomes. The stratigraphy and stratal architecture, displaying a retrogradational arrangement with progradational patterns of minor order, were controlled by different sea-level positions. The stratigraphic division represents the coastal response to the last fourth-order transgressive and highstand conditions, modulated by small-scale sea-level oscillations (≈1-2 m) of fith to sixth order. This study also highlights the advantage of an integrated analysis using acoustic/seismic methods for practical assessment of the anthropogenic effects on infralittoral domains based on the association of marine geological observations.
Note: Reproducció del document publicat a: http://dx.doi.org/10.3989/scimar.2010.74n1179
It is part of: Scientia Marina, 2009, vol. 74, num. 1, p. 179-179
Related resource: http://dx.doi.org/10.3989/scimar.2010.74n1179
URI: http://hdl.handle.net/2445/32408
ISSN: 0214-8358
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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