Ophiolites of Iran: Keys to understanding the tectonic evolution of SW Asia:(II) Mesozoic ophiolites

HS Moghadam, RJ Stern - Journal of Asian Earth Sciences, 2015 - Elsevier
Iran is a mosaic of continental terranes of Cadomian (520–600 Ma) age, stitched together
along sutures decorated by Paleozoic and Mesozoic ophiolites. Here we present the current …

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 …

An inter‐laboratory evaluation of OD‐3 zircon for use as a secondary U–Pb dating standard

H Iwano, Y Orihashi, T Hirata, M Ogasawara… - Island Arc, 2013 - Wiley Online Library
Zircon OD‐3 from the P aleogene K awamoto G ranodiorite (M ihara body) in J apan has
been identified as a potential multi‐grain secondary standard for U–Pb dating. We have …

Geology of the Eoarchean,> 3.95 Ga, Nulliak supracrustal rocks in the Saglek Block, northern Labrador, Canada: the oldest geological evidence for plate tectonics

T Komiya, S Yamamoto, S Aoki, Y Sawaki, A Ishikawa… - Tectonophysics, 2015 - Elsevier
The Earth is a unique planet, which has been highly evolved, diversified and complicated
through geologic time, and underwent many key events, including giant impact, magma …

Ridge subduction: Unraveling the consequences linked to a slab window development beneath South America at the Chile Triple Junction

J Sanhueza, G Yáñez, WR Buck… - Geochemistry …, 2023 - Wiley Online Library
The subduction of an active spreading center generates a clear signature in the temporal
evolution of subduction zones. It disrupts the typical arc‐type magmatism and intraplate …

Cenozoic basin evolution of the Central Patagonian Andes: Evidence from geochronology, stratigraphy, and geochemistry

A Encinas, A Folguera, R Riffo, P Molina, LF Paz… - Geoscience …, 2019 - Elsevier
Abstract The Central Patagonian Andes is a particular segment of the Andean Cordillera that
has been subjected to the subduction of two spreading ridges during Eocene and Neogene …

Are the Taitao granites formed due to subduction of the Chile ridge?

R Anma, R Armstrong, Y Orihashi, S Ike, KC Shin… - Lithos, 2009 - Elsevier
The Taitao granites are distributed around the Late Miocene Taitao ophiolite (5.66±0.33 Ma
to 5.19±0.15 Ma) exposed at the western tip of the Taitao peninsula, southern Chile,~ 50 km …

A review on forearc ophiolite obduction, Adakite-like generation, and slab window development at the Chile triple junction area: uniformitarian framework for …

J Bourgois, Y Lagabrielle, H Martin, J Dyment… - Pure and Applied …, 2016 - Springer
This paper aggregates the main basic data acquired along the Chile Triple Junction (CTJ)
area (45°–48° S), where an active spreading center is presently subducting beneath the …

Chemical and chronologic complexity in the convecting upper mantle: Evidence from the Taitao ophiolite, southern Chile

RF Schulte, M Schilling, R Anma, J Farquhar… - … et Cosmochimica Acta, 2009 - Elsevier
Exposure of the ca. 6Ma Taitao ophiolite, Chile, located∼ 50km south of the Chile Triple
Junction, allows detailed chemical and isotopic study of rocks that were recently extracted …

Ultramafic rocks in the North Patagonian Andes: is their emplacement associated with the Neogene tectonics of the Liquiñe-Ofqui Fault Zone?

F Hervé, F Fuentes, M Calderón, M Fanning… - 2017 - ri.conicet.gov.ar
En la vertiente occidental de los Andes norpatagonicos de Chiloé continental (41° 44'-42°
12'S) afloran serpentinitas y harzburgitas frescas o parcialmente serpentinizadas. Estas …