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Late Miocene exhumation of the Western Cordillera, Ecuador, driven by increased coupling between the subducting Carnegie Ridge and the South American …
The subduction of bathymetric highs, such as aseismic ridges, leads to far‐reaching
changes in the dynamics of subduction zones with increased plate coupling and …
changes in the dynamics of subduction zones with increased plate coupling and …
Structural evolution of the southern Ecuadorian forearc in the Santa Elena Peninsula region
The southern Ecuadorian forearc system is related to the subduction of the oceanic
Farallon/Nazca Plate beneath the continental South American Plate since the Late …
Farallon/Nazca Plate beneath the continental South American Plate since the Late …
Exhumation and topographic evolution of the Chiapas Massif Complex (southern Mexico) constrained by thermochronologic data modeling along vertical profiles
Thermochronometry is used to better understand the processes responsible for Cenozoic
magmatism and exhumation of the Chiapas Massif Complex that spans a diffuse triple …
magmatism and exhumation of the Chiapas Massif Complex that spans a diffuse triple …
Geodynamic controls in the southernmost Northern Andes magmatic arc: Trace elements and Hf-O isotopic systematics in forearc detrital zircon
U-Pb dating of single detrital zircon grains by laser ablation–inductively coupled plasma–
mass spectrometry (LA-ICP-MS) paired with Hf and O isotopic and trace-element analyses …
mass spectrometry (LA-ICP-MS) paired with Hf and O isotopic and trace-element analyses …
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
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 …
Holocene marine tephra offshore Ecuador and Southern Colombia: First trench‐to‐arc correlations and implication for magnitude of major eruptions
Tephra layers preserved in marine sediments are strong tools to study the frequency,
magnitude and source of past major explosive eruptions. Thirty‐seven volcanoes from the …
magnitude and source of past major explosive eruptions. Thirty‐seven volcanoes from the …
[PDF][PDF] Early Miocene aequipectininin bivalves of the Pirabas Formation of the Pará State, northeastern Brazil
A taxonomic revision of the Tribe Aequipectini from the upper Burdigalian, Lower Miocene
Pirabas Formation in Brazil) resulted in an identification of Leptopecten daideleus comb …
Pirabas Formation in Brazil) resulted in an identification of Leptopecten daideleus comb …
Multi-Scale Imaging of the Andean Subduction Zone from the Crust of the Northern Andes to the Nazca Slab's Descent into the Lower Mantle from Seismic …
EE Rodríguez - 2023 - search.proquest.com
Abstract The Nazca-South America subduction zone spans> 7,000 km of the South America
margin. It is characterized by the subduction of the oceanic Nazca plate beneath continental …
margin. It is characterized by the subduction of the oceanic Nazca plate beneath continental …
Catálogo de edades radiométricas de Ecuador
La geocronología es una herramienta de la cartografía geológica que permite determinar la
edad de las secuencias estratigráficas y cuerpos intrusivos, con el objetivo de verificar la …
edad de las secuencias estratigráficas y cuerpos intrusivos, con el objetivo de verificar la …
Exhumation of the Western Cordillera, Ecuador driven by late Miocene subduction of the Carnegie Ridge
Cenozoic growth of the Andes has been strongly influenced by subduction dynamics,
reactivation of inherited crustal heterogeneities, and the superposed effects of climate …
reactivation of inherited crustal heterogeneities, and the superposed effects of climate …