Previous work on the Gulf of Cadiz (S Iberian Margin) has revealed several mud volcanoes sitting on the accretionary wedge and aligned along west-east trending transform faults. The source of fluids in these mud volcanoes is several kilometres below the seafloor and their geochemical composition indicates that they are affected, in different degrees, by oceanic crust alteration, implying that there is active flow connecting the oceanic basement and the seafloor. To date, such kind of hydrothermal circulation is only known for relatively young oceanic crust (<60 Ma) and therefore the existence of a hydrological connection between old, sedimented oceanic crust and the seafloor is a phenomenon that may represent a (missing) link between hydrot...
The Gulf of Cadiz is characterized by extensive active and inactive fluid escape structures which ma...
Mud volcanoes are seafloor expressions of focused fluid flow that are common in compressional tecton...
The Gulf of Cadiz is an extensive seepage area in the south Iberian margin (NE Atlantic) encompassin...
During the RV METEOR M86/5 cruise (as part of the SWIMGLO project PTDC/MAR/100522/2008) three new mu...
We report on newly discovered mud volcanoes located at ∼4500 m water depth ∼90 km west of the deform...
Submersible observations and seafloor mapping over areas of mud volcanism in the eastern Mediterrane...
A new deep water mud volcano field (between 2000 and 3500 in water depth) was discovered in the deep...
Studies that focus on meiofaunal assemblages of deep-sea mud volcanoes show an unpredictable abundan...
The newly discovered Larache mud volcano field at the Moroccan Atlantic slope (200 m - 700m water de...
European Geosciences Union General Assembly 2017, 23-28 April 2017, Vienna, Austria.-- 1 pageMud vol...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanism and fluid seepage are common phenomena on the continental margin in the Gulf of Cadiz,...
The seabed morphology, type of sediments, and dominant benthic species on eleven mud volcanoes and d...
Cruise M86/5 aimed at collecting data from potential fluid dewatering sites located in the deep-sea ...
Drilling during Ocean Drilling Program Leg 160 (April–May, 1995) revealed important new evidence con...
The Gulf of Cadiz is characterized by extensive active and inactive fluid escape structures which ma...
Mud volcanoes are seafloor expressions of focused fluid flow that are common in compressional tecton...
The Gulf of Cadiz is an extensive seepage area in the south Iberian margin (NE Atlantic) encompassin...
During the RV METEOR M86/5 cruise (as part of the SWIMGLO project PTDC/MAR/100522/2008) three new mu...
We report on newly discovered mud volcanoes located at ∼4500 m water depth ∼90 km west of the deform...
Submersible observations and seafloor mapping over areas of mud volcanism in the eastern Mediterrane...
A new deep water mud volcano field (between 2000 and 3500 in water depth) was discovered in the deep...
Studies that focus on meiofaunal assemblages of deep-sea mud volcanoes show an unpredictable abundan...
The newly discovered Larache mud volcano field at the Moroccan Atlantic slope (200 m - 700m water de...
European Geosciences Union General Assembly 2017, 23-28 April 2017, Vienna, Austria.-- 1 pageMud vol...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanism and fluid seepage are common phenomena on the continental margin in the Gulf of Cadiz,...
The seabed morphology, type of sediments, and dominant benthic species on eleven mud volcanoes and d...
Cruise M86/5 aimed at collecting data from potential fluid dewatering sites located in the deep-sea ...
Drilling during Ocean Drilling Program Leg 160 (April–May, 1995) revealed important new evidence con...
The Gulf of Cadiz is characterized by extensive active and inactive fluid escape structures which ma...
Mud volcanoes are seafloor expressions of focused fluid flow that are common in compressional tecton...
The Gulf of Cadiz is an extensive seepage area in the south Iberian margin (NE Atlantic) encompassin...