Echo-character distribution in the Cantabrian Margin and the Biscay Abyssal Plain

[EN] In 2003, 2006–2009, 2014 and 2015, seven oceanographic cruises were carried out on board the Spanish R/V Hespérides in the Cantabrian Margin and the adjacent abyssal plains, covering an area of 219,124 km2. Based on the combined analysis and interpretation of the bathymetric and reflectivity da...

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Detalles Bibliográficos
Autores: Maestro González, Adolfo, Gallastegui, Alba, Moreta, Mercedes, Llave, Estefanía, Bohoyo, Fernando, Druet Vélez, María, Navas Madrazo, José Javier, Mink Proeck, Sandra Martina, Fernández Sáez, Fernando, Catalán Morollón, Manuel, Gómez-Ballesteros, María, Muñoz-Martín, Alfonso, Granja-Bruña, José Luis
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2021
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/375868
Acceso en línea:http://hdl.handle.net/10261/375868
Access Level:acceso abierto
Palabra clave:Bathymetry
Cantabrian Margin
Echo-character
Reflectivity
Parametric echo-sounder seismic profiles
Descripción
Sumario:[EN] In 2003, 2006–2009, 2014 and 2015, seven oceanographic cruises were carried out on board the Spanish R/V Hespérides in the Cantabrian Margin and the adjacent abyssal plains, covering an area of 219,124 km2. Based on the combined analysis and interpretation of the bathymetric and reflectivity data obtained with multibeam echo sounders (SIMRAD EM12, EM120 and EM1002), and ultra-high-resolution reflection seismic records acquired with the SIMRAD TOPAS PS18 parametric sounder, the mapping of the acoustic facies or echo-character at a scale of 1:1,200,000 has been carried out. Thirty types of echoes have been differentiated and gather into four main groups: Distinct, Irregular, Hyperbolic and Undulated. The echo-character depends on the acoustic response of the shallow sediment and the seabed morphology. Therefore, its analysis and characterization are basic for understanding recent and present-day sedimentary processes.