%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture non répertoriées par l'AERES
%A Sallarès, Valenti
%A Charvis, Philippe
%A Flueh, E.R.
%A Bialas, J.
%T Seismic structure of Cocos and Malpelo volcanic ridges and implications for hot spot-ridge interaction
%D 2003
%L fdi:010032982
%G ENG
%J Journal of Geophysical Research
%@ 0148-0227
%K VOLCANISME ; POINT CHAUD ; TOMOGRAPHIE ; SISMOTECTONIQUE ; CROUTE OCEANIQUE ; GEODYNAMIQUE
%K COLON ARCHIPIELAGO
%K COCOS ; MALPELO
%N B12
%P 5-1-5-21
%R 10.1029/2003JB002431
%U https://www.documentation.ird.fr/hor/fdi:010032982
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers20-10/010032982.pdf
%V 108
%W Horizon (IRD)
%X The Cocos and Malpelo Volcanic Ridges are blocks of thickened oceanic crust thought to be the result of the interaction between the Galapagos hot spot and the Cocos Nazca Spreading Center during the last 20 m.y. In this work we investigate the seismic structure of these two aseismic ridges along three wide angle transects acquired during the Panama basin and Galapagos plume New Investigations of Intraplate magmatism (PAGANINI) 1999 experiment. A two dimensional velocity field with the Moho geometry is obtained using joint refraction/reflection travel time tomography, and the uncertainty and robustness of the results are estimated by performing a Monte Carlo type analysis. Our results show that the maximum crustal thickness along these profiles ranges from 16.5 km (southern Cocos) to 19 km (northern Cocos and Malpelo). Oceanic layer 2 thickness is quite uniform regardless of total crustal thickness variations; crustal thickening is mainly accommodated by layer 3. These observations are shown to be consistent with gravity data. The variation of layer 3 velocities is similar along all profiles, being lower where crust is thicker. This leads to an overall anticorrelation between crustal thickness and bulk lower crustal velocity. Since this anticorrelation is contrary to crustal thickening resulting from passive upwelling of abnormally hot mantle, it is necessary to consider active upwelling components and/or some compositional heterogeneities in the mantle source. The NW limit of the Malpelo Ridge shows a dramatic crustal thinning and displays high lower crustal velocities and a poorly defined crust mantle boundary, suggesting that differential motion along the Coiba transform fault probably separated Regina and Malpelo Ridges.
%$ 066GPHMAR