Geodynamic controls on magmatic arc migration and quiescence
GM Gianni, SP Luján - Earth-Science Reviews, 2021 - Elsevier
Reconfigurations of magmatic arcs through time have been recognized since pioneering
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …
Lithospheric evolution of the Pre-and Early Andean convergent margin, Chile
V Oliveros, P Vásquez, C Creixell, F Lucassen… - Gondwana …, 2020 - Elsevier
Abstract The proto-Andean and Early Andean evolution of the southwestern Gondwana
margin comprises three stages that differ in their magmatic evolution and deformational …
margin comprises three stages that differ in their magmatic evolution and deformational …
Tectonic evolution of the North Patagonian Andes (41–44 S) through recognition of syntectonic strata
Abstract The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low
topography, reduced crustal thickness and a broad lateral development determined by a …
topography, reduced crustal thickness and a broad lateral development determined by a …
Reconciling orogenic drivers for the evolution of the Bangong‐Nujiang Tethys during Middle‐Late Jurassic
Identifying arc‐trench systems along with spatial and temporal variations in their record of
tectono‐magmatic events is crucial for determining the orogenic divers and evolution of …
tectono‐magmatic events is crucial for determining the orogenic divers and evolution of …
Unconformity development in retroarc foreland basins: implications for the geodynamics of Andean-type margins
BK Horton - Journal of the Geological Society, 2022 - lyellcollection.org
Unconformities in foreland basins may be generated by tectonic processes that operate in
the basin, the adjacent fold–thrust belt or the broader convergent margin. Foreland basin …
the basin, the adjacent fold–thrust belt or the broader convergent margin. Foreland basin …
Pacific-type transform and convergent margins: igneous rocks, geochemical contrasts and discriminant diagrams
AV Grebennikov, AI Khanchuk - International Geology Review, 2021 - Taylor & Francis
Transform margins represent lithospheric plate boundaries with horizontal sliding of the
oceanic plate, which in time and space replaced the subduction-related convergent margins …
oceanic plate, which in time and space replaced the subduction-related convergent margins …
Thermal history of the southern Antarctic Peninsula during Cenozoic oblique subduction
Apatite (U–Th)/He and apatite fission-track thermochronology is used to constrain the
cooling and uplift history of the southern Antarctic Peninsula where easterly-directed …
cooling and uplift history of the southern Antarctic Peninsula where easterly-directed …
The fate of the Farallon slab beneath Patagonia and its links to Cenozoic intraplate magmatism, marine transgressions and topographic uplift
The arrival and subsequent stagnation of the Farallon/Nazca slab at the mantle transition
zone below southern South America triggered seemingly unrelated large-scale geological …
zone below southern South America triggered seemingly unrelated large-scale geological …
Slab melting boosts the mantle wedge contribution to Li-rich magmas
The lithium cycling in the supra-subduction mantle wedge is crucial for understanding the
generation of Li-rich magmas that may potentially source ore deposition in continental arcs …
generation of Li-rich magmas that may potentially source ore deposition in continental arcs …
Styles of trench‐parallel mid‐ocean ridge subduction affect Cenozoic geological evolution in circum‐pacific continental margins
Distinct signatures are present in the circum‐Pacific continental margins (eg, kinematics,
magmatism, and basin evolution), possibly influenced by the input of mid‐ocean ridge. It …
magmatism, and basin evolution), possibly influenced by the input of mid‐ocean ridge. It …