Geo-Temas, 16 (1) ISSN 1576-5172 Abstract: Seabed morphology, sub-bottom characteristics and benthic communities of the Hespérides volcanic complex, located in the continental slope of the Gulf of Cadiz, have been analyzed. The aim of this study is to characterize the morphological features, the geological processes and near-bottom water masses for understanding the relationships between the occurrence of this fluid venting related edifice and their associated biota. Additionally, dominant benthic species associated with seepage, hard substrates or soft bottoms have also been observed in different areas of the complex. Mud breccia sediments and chemosymbiotic metazoans are mainly located at the summit indicating a higher seepage activity. ...
VII Congreso Geológico de España, 14-18 julio 2008, Las Palmas de Gran Canaria.-- 4 pages, 1 figure[...
Simposio sobre el Margen Ibérico Atlántico (9º. 2018. Coimbra, Portugal)More than 70 mud volcanoes (...
Mercator mud volcano has been explored by direct visual observations using a ROV at 350 to 370 m dep...
Se ha analizado la morfología del fondo, las características sub-superficiales y los hábitats bentó...
The seabed morphology and the sub-bottom characteristics of a sector of the Gulf of Cádiz continent...
Mud volcanoes are conical edifices formed by the vertical migration of muddy sediments and fluids (...
The seabed morphology, type of sediments, and dominant benthic species on eleven mud volcanoes and d...
The Iberian margin in the Gulf of Cádiz hosts a fluid venting area embedded into a contourite deposi...
Esta tesis doctoral ha sido realizada en el Centro Oceanográfico de Málaga del Instituto Español de ...
The Gulf of Cadiz is located in the boundary of two lithospheric plates, this tectonic activity pro...
Based on new discoveries of submarine chimneys and pavements related to leaking gases in the Gulf of...
The El Arraiche mud volcano field consists of eight mud volcanoes up to 255 m high and 5.4 km wide, ...
The seabed morphology and the sub-superficial characteristics of the Cristóbal Colón diapir located...
The Iberian margin in the Gulf of Cádiz hosts a fluid venting area embedded into a contourite deposi...
The Gulf of Cádiz represents an area of extensive seepage of the south-western Iberian Peninsula tha...
VII Congreso Geológico de España, 14-18 julio 2008, Las Palmas de Gran Canaria.-- 4 pages, 1 figure[...
Simposio sobre el Margen Ibérico Atlántico (9º. 2018. Coimbra, Portugal)More than 70 mud volcanoes (...
Mercator mud volcano has been explored by direct visual observations using a ROV at 350 to 370 m dep...
Se ha analizado la morfología del fondo, las características sub-superficiales y los hábitats bentó...
The seabed morphology and the sub-bottom characteristics of a sector of the Gulf of Cádiz continent...
Mud volcanoes are conical edifices formed by the vertical migration of muddy sediments and fluids (...
The seabed morphology, type of sediments, and dominant benthic species on eleven mud volcanoes and d...
The Iberian margin in the Gulf of Cádiz hosts a fluid venting area embedded into a contourite deposi...
Esta tesis doctoral ha sido realizada en el Centro Oceanográfico de Málaga del Instituto Español de ...
The Gulf of Cadiz is located in the boundary of two lithospheric plates, this tectonic activity pro...
Based on new discoveries of submarine chimneys and pavements related to leaking gases in the Gulf of...
The El Arraiche mud volcano field consists of eight mud volcanoes up to 255 m high and 5.4 km wide, ...
The seabed morphology and the sub-superficial characteristics of the Cristóbal Colón diapir located...
The Iberian margin in the Gulf of Cádiz hosts a fluid venting area embedded into a contourite deposi...
The Gulf of Cádiz represents an area of extensive seepage of the south-western Iberian Peninsula tha...
VII Congreso Geológico de España, 14-18 julio 2008, Las Palmas de Gran Canaria.-- 4 pages, 1 figure[...
Simposio sobre el Margen Ibérico Atlántico (9º. 2018. Coimbra, Portugal)More than 70 mud volcanoes (...
Mercator mud volcano has been explored by direct visual observations using a ROV at 350 to 370 m dep...