The El Arraiche field is a new mud volcano field discovered near the Moroccan shelf edge in the Gulf of Cadiz that consists of 8 mud volcanoes in water depths from 200 to 700 m. The largest mud volcano in the field (Al Idrissi mud volcano) is 255 m high and 5.4 km wide. The cluster was discovered during a survey with the RV Belgica and studied further during Leg 2 of the TTR 12 survey onboard the RN Prof Logachev. The 2002 surveys yielded detailed multibeam bathymetry over a 700 km(2) study area, dense grids of high-resolution seismic data, deep-tow sub bottom profiles, sidescan sonar mosaics over the major structures. Selected video imagery lines, video guided grab samples, dredge samples, gravity cores, and box cores were collected for gr...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Detailed geophysical, geochemical and petrological data over a cluster of large mud volcanoes at the...
A new deep water mud volcano field (between 2000 and 3500 in water depth) was discovered in the deep...
The El Arraiche mud volcano field consists of eight mud volcanoes up to 255 m high and 5.4 km wide, ...
Located on the western Moroccan continental shelf of the Gulf of Cadiz, the Mercator Mud Volcano (MM...
The El Arraiche mud volcano field is situated on the Atlantic Moroccan margin. About 8 small to gian...
The newly discovered Larache mud volcano field at the Moroccan Atlantic slope (200 m - 700m water de...
The El Arraiche mud volcano field was discovered in May 2002 in the Moroccan Atlantic margin in the ...
Gas hydrates inside mud volcanoes have been observed in several locations but are generally found at...
Drilling during Ocean Drilling Program Leg 160 (April–May, 1995) revealed important new evidence con...
Mud volcanoes are seafloor expressions of focused fluid flow that are common in compressional tecton...
The gulf of Cadiz is one of the most interesting areas to study mud volcanoes and structures related...
Mud volcanoes are seafloor expressions of focused fluid flow that are common in compressional tecton...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Detailed geophysical, geochemical and petrological data over a cluster of large mud volcanoes at the...
A new deep water mud volcano field (between 2000 and 3500 in water depth) was discovered in the deep...
The El Arraiche mud volcano field consists of eight mud volcanoes up to 255 m high and 5.4 km wide, ...
Located on the western Moroccan continental shelf of the Gulf of Cadiz, the Mercator Mud Volcano (MM...
The El Arraiche mud volcano field is situated on the Atlantic Moroccan margin. About 8 small to gian...
The newly discovered Larache mud volcano field at the Moroccan Atlantic slope (200 m - 700m water de...
The El Arraiche mud volcano field was discovered in May 2002 in the Moroccan Atlantic margin in the ...
Gas hydrates inside mud volcanoes have been observed in several locations but are generally found at...
Drilling during Ocean Drilling Program Leg 160 (April–May, 1995) revealed important new evidence con...
Mud volcanoes are seafloor expressions of focused fluid flow that are common in compressional tecton...
The gulf of Cadiz is one of the most interesting areas to study mud volcanoes and structures related...
Mud volcanoes are seafloor expressions of focused fluid flow that are common in compressional tecton...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...
Mud volcanoes (MVs) are expulsion features ubiquitously present in areas of tectonic convergence bot...