Maastrichtian-Cenozoic erosional history of the northern Peruvian Amazonian Andes implications for the Eastern Cordillera evolution (Huallaga Basin, northern Peru)
Abstract Late Cretaceous-Cenozoic Andean mountain building may have experienced
various phases of orogenesis in response to variations the dip angle of the subducting slab …
various phases of orogenesis in response to variations the dip angle of the subducting slab …
Blossoming of the Pleistocene volcanism in the Ecuadorian Andes: a review based on new and recent geochronological data
S Santamaría, M Bablon, X Quidelleur… - Bulletin of …, 2024 - Springer
The Ecuadorian arc is composed of an unusually high number of volcanoes, organized as
along-arc alignments and across-arc clusters, in a relatively small area. Although several …
along-arc alignments and across-arc clusters, in a relatively small area. Although several …
New constraints on the Late Miocene-Pliocene deformational and depositional evolution of the Eastern Cordillera and Sub-Andean Zone in southern Peru
The deformation history of the Eastern Cordillera (EC) and Sub-Andean Zone (SAZ) of
southern Peru is critical for understanding the roles that tectonics and climate played in the …
southern Peru is critical for understanding the roles that tectonics and climate played in the …
[HTML][HTML] Large-scale sea surface temperature gradients govern westerly moisture transport in western Ecuador during the Plio-Pleistocene
The cross-equatorial southwesterly winds from the eastern equatorial Pacific direct moisture
toward the Pacific coast of northwestern South America, where subsequent orographic lifting …
toward the Pacific coast of northwestern South America, where subsequent orographic lifting …
Explicit role of seamount subduction in upper plate deformation as exemplified in the Ryukyu subduction zone
X He, Q Zhou - Journal of Asian Earth Sciences, 2024 - Elsevier
The Ryukyu subduction zone is typical of the subduction of an oceanic ridge (seamount or
plateau) and back-arc rifting. How the upper plate responds to the combined effect of …
plateau) and back-arc rifting. How the upper plate responds to the combined effect of …
Evolution of the Manabí forearc basin in Ecuador: From the collision of Caribbean oceanic plateau to the build up of the Andes and Coastal Cordilleras
MJ Hernández, F Michaud, JY Collot, E d'Acremont… - Tectonophysics, 2024 - Elsevier
We investigate the evolution of the onshore Manabí forearc basin in Ecuador, which has
developed on accreted oceanic terranes. We use 2D seismic profiles to identify 10 seismic …
developed on accreted oceanic terranes. We use 2D seismic profiles to identify 10 seismic …
Deciphering permanent uplift along the Pacific coast of South America through signal analysis of various tectonic processes
R Freisleben, J Jara‐Muñoz, D Melnick, D Molina… - …, 2023 - Wiley Online Library
Abstract The tectonically active South American margin is characterized by the accumulation
of deformation contributing to uplift of the Andean forearc at millennial time scales. However …
of deformation contributing to uplift of the Andean forearc at millennial time scales. However …
Plio-Pleistocene evolution of westerly moisture transport into the northern tropical Andes
Westerly winds from the eastern equatorial Pacific direct moisture into the Western
Cordillera of the northern tropical Andes, where subsequent orographic lifting creates the …
Cordillera of the northern tropical Andes, where subsequent orographic lifting creates the …
Anatomie des structures actives au voisinage de la zone de contact interplaque de l'Équateur: apport de la sismicité
A Wickham-Piotrowski - 2023 - theses.hal.science
Les modes de glissement sur l'interface de subduction varient du glissement asismique
stable à la rupture sismique rapide en passant par des glissements transitoires lents dont la …
stable à la rupture sismique rapide en passant par des glissements transitoires lents dont la …
Deciphering the mechanisms of permanent forearc deformation based on marine terraces
R Freisleben - 2023 - publishup.uni-potsdam.de
The Andes reflect Cenozoic deformation and uplift along the South American margin in the
context of regional shortening associated with the interaction between the subducting Nazca …
context of regional shortening associated with the interaction between the subducting Nazca …