Publications des scientifiques de l'IRD

Michaud François, Chabert Anne, Collot Jean Yves, Sallarès Valenti, Flueh E.R., Charvis Philippe, Graindorge D., Gustcher M.A., Bialas J. (2005). Fields of multi-kilometer scale sub-circular depressions in the Carnegie Ridge sedimentary blanket : effect of underwater carbonate dissolution ?. Marine Geology, 216, p. 205-219. ISSN 0025-3227.

Titre du document
Fields of multi-kilometer scale sub-circular depressions in the Carnegie Ridge sedimentary blanket : effect of underwater carbonate dissolution ?
Année de publication
2005
Type de document
Article référencé dans le Web of Science WOS:000229051100002
Auteurs
Michaud François, Chabert Anne, Collot Jean Yves, Sallarès Valenti, Flueh E.R., Charvis Philippe, Graindorge D., Gustcher M.A., Bialas J.
Source
Marine Geology, 2005, 216, p. 205-219 ISSN 0025-3227
Offshore Ecuador, the Carnegie Ridge is a volcanic ridge with a carbonate sediment drape. During the SALIERI Cruise, multibeam bathymetry was collected across Carnegie Ridge with the Simrad EM120 of the R/V SONNE. The most conspicuous features discovered on the Carnegie Ridge are fields of circular closed depressions widely distributed along the mid-slope of the northern and southern flanks of the ridge between 1500 and 2600 m water depth. These circular depressions are 1-4 km wide and typically 100-400 m deep. Most are flat floored and some are so densely packed that they form a honeycomb pattern. The depressions were carved into the ridge sedimentary blanket, which consists of carbonate sediment and has been dated from upper Miocene to upper Pleistocene. Several hypotheses including pockmark origin, sediment creeping, paleo-topography of the volcanic basement, effects of subbottom currents, and both marine and subaerial karstic origins are discussed. We believe that underwater dissolution process merits the most serious consideration regarding the origin of the closed depression.
Plan de classement
Géomorphologie [064GEOMOR]
Descripteurs
MARGE CONTINENTALE ACTIVE ; RELIEF SOUS MARIN ; PALEOGEOMORPHOLOGIE ; KARST ; ROCHE CARBONATEE ; DISSOLUTION
Description Géographique
EQUATEUR ; COLON ARCHIPIELAGO
Localisation
Fonds IRD [F B010034400] ; Bondy ; Quito
Identifiant IRD
fdi:010034400
Contact