The active margin of Ecuador is characterized by strong tectonic erosion that contributes to the formation of adeep trench filled by a complex suite of sedimentary facies. Gravity flow sedimentation is ubiquitous along themargin and facies range from laterally continuous m-thick mass transport deposits to isolated cm-thick...
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April 12, 2016 (v1)Conference paperUploaded on: February 28, 2023
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October 24, 2016 (v1)Conference paper
La subduction de monts sous-marins est connue pour affectersignificativement les marges actives, en augmentant l'érosion tectonique.Par ailleurs, la participation des monts sous-marins àla nucléation/couplage au niveau des grands séismes de subductionest en plein débat. Des modèles analogiques ont montré lesprincipales caractéristiques de ces...
Uploaded on: February 28, 2023 -
September 24, 2019 (v1)Conference paper
International audience
Uploaded on: December 4, 2022 -
2015 (v1)Journal article
Selected high-resolution seismic-reflection profiles and multibeam bathymetry acquired along the convergent Ecuador margin during the ATACAMES cruise on onboard the R/V L'Atalante (Jan.15–Feb.18, 2012) allow a preliminary evaluation of the neotectonic development and stratigraphic evolution of the margin based on the sismo-stratigraphic...
Uploaded on: March 25, 2023 -
2016 (v1)Publication
International audience
Uploaded on: December 3, 2022