Tertiary and quaternary stratigraphy of the deposits of the interandean depression of Ecuador (between 0° and 2° 15' S) Understanding of the stratigraphy of Tertiary and Quaternary rocks of the Ecuadorian Interandean Depression is refined by stratigraphic and sedimentological correlations, as well as by radiometric age determinations. The sedimentological dynamics, similar within the three study areas of the Interandean Depression, are characteristic of an intra-arc basin since the Late Cenozoic.Des corrélations sédimentologiques et stratigraphiques effectuées dans trois zones de la Dépression Interandine d'Équateur et de récentes datations radiométriques permettent de compléter les connaissances stratigraphiques du Tertiaire et du Quater...
The Silante Formation is a thick series of continental deposits, exposed along a trench-parallel dis...
National audienceAlong the Ecuadorian convergent margin, the onshore Manabí sedimentary forearcbasin...
Two accreted oceanic terranes are classically recognized in the Cordillera Occidental of Central Ecu...
The inter-Andean structure is defined as an approximately north–south-trending, linear, topographic ...
The aim of this study is to constrain recent deformation and stratigraphic evolution of an active ma...
The bulk of the Tertiary stratigraphy of the Borbón Basin, a forearc basin extending from northern E...
172 pages, 90 MoFinal report of the Orstom-Petroproducción cooperation agreement, QuitoThis report s...
Mémoires de Géologie Alpine - H.S. n° 32The neogene geodynamic evolution of the Ecuadorian Andes is ...
International audienceThe SW of Ecuador offers a great opportunity to study the long-term behavior o...
Cordilleran style margins exhibit significant heterogeneities both along-strike and through time. Th...
In Early Miocene times the Cordillera did not exist and the Pacific Ocean reached the Oriente. In th...
In Early Miocene times the Cordillera did not exist and the Pacific Ocean reached the Oriente. In th...
15 pages Sous presse dans le: "Journal of South American Earth Sciences"A reappraisal of the “Late C...
We obtained U–Pb zircon ages of Late Tertiary intrusions in the northern Andes to provide robust tim...
The Silante Formation is a thick series of continental deposits, exposed along a trench-parallel dis...
National audienceAlong the Ecuadorian convergent margin, the onshore Manabí sedimentary forearcbasin...
Two accreted oceanic terranes are classically recognized in the Cordillera Occidental of Central Ecu...
The inter-Andean structure is defined as an approximately north–south-trending, linear, topographic ...
The aim of this study is to constrain recent deformation and stratigraphic evolution of an active ma...
The bulk of the Tertiary stratigraphy of the Borbón Basin, a forearc basin extending from northern E...
172 pages, 90 MoFinal report of the Orstom-Petroproducción cooperation agreement, QuitoThis report s...
Mémoires de Géologie Alpine - H.S. n° 32The neogene geodynamic evolution of the Ecuadorian Andes is ...
International audienceThe SW of Ecuador offers a great opportunity to study the long-term behavior o...
Cordilleran style margins exhibit significant heterogeneities both along-strike and through time. Th...
In Early Miocene times the Cordillera did not exist and the Pacific Ocean reached the Oriente. In th...
In Early Miocene times the Cordillera did not exist and the Pacific Ocean reached the Oriente. In th...
15 pages Sous presse dans le: "Journal of South American Earth Sciences"A reappraisal of the “Late C...
We obtained U–Pb zircon ages of Late Tertiary intrusions in the northern Andes to provide robust tim...
The Silante Formation is a thick series of continental deposits, exposed along a trench-parallel dis...
National audienceAlong the Ecuadorian convergent margin, the onshore Manabí sedimentary forearcbasin...
Two accreted oceanic terranes are classically recognized in the Cordillera Occidental of Central Ecu...