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Artículo

A geodynamic model linking Cretaceous orogeny, arc migration, foreland dynamic subsidence and marine ingression in southern South America

Gianni, Guido MartinIcon ; Davila, Federico MiguelIcon ; Echaurren Gonzalez, AndresIcon ; Fennell, Lucas MartínIcon ; Tobal, Jonathan ElíasIcon ; Navarrete Granzotto, César RodrigoIcon ; Quezada, Paulo; Folguera Telichevsky, AndresIcon ; Gimenez, Mario ErnestoIcon
Fecha de publicación: 10/2018
Editorial: Elsevier Science
Revista: Earth-science Reviews
ISSN: 0012-8252
Idioma: Inglés
Tipo de recurso: Artículo publicado
Clasificación temática:
Geología

Resumen

This study synthesizes the tectonomagmatic evolution of the Andes between 35°30′S to 48°S with the aim to spotlight early contractional phases on Andean orogenic building and to analyze their potential driving processes. We examine early tectonic stages of the different fold-thrust belts that compose this Andean segment. Additionally, we analyzed the spatio-temporal magmatic arc evolution as a proxy of dynamic changes in Andean subduction during critical tectonic stages of orogenic construction. This revision proposes a hypothesis related the existence of a continuous large-scale flat subduction setting in Cretaceous times with a similar size to the present-largest flat-slab setting on earth. This potential process would have initiated diachronically in the late Early Cretaceous and achieved full development in Late Cretaceous to earliest Paleocene times, constructing a series of fold-thrust belts on the retro-arc zone from 35°30′S to 48°S. Moreover, we assess major paleogeographic changes that took place during flat-slab full development in Maastrichtian-Danian times. At this moment, an enigmatic Atlantic-derived marine flooding covered the Patagonian foreland reaching as far as the Andean foothills. Based on flexural and dynamic topography analyses, we suggest that focused dynamic subsidence at the edge of the flat-slab may explain sudden marine ingression previously linked to continental tilting and orogenic loading during a high sea level global stage. Finally, flat-subduction destabilization could have triggered massive outpouring of synextensional intraplate volcanic rocks in southern South America and the arc retraction in late Paleogene to early Neogene times.
Palabras clave: ANDES , BROKEN FORELAND , DYNAMIC SUBSIDENCE , FLAT-SLAB , MARINE TRANSGRESSION
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info:eu-repo/semantics/openAccess Excepto donde se diga explícitamente, este item se publica bajo la siguiente descripción: Atribución-NoComercial-SinDerivadas 2.5 Argentina (CC BY-NC-ND 2.5 AR)
Identificadores
URI: http://hdl.handle.net/11336/88739
DOI: http://dx.doi.org/10.1016/j.earscirev.2018.06.016
URL: https://www.sciencedirect.com/science/article/pii/S0012825218301661
Colecciones
Articulos(CCT - SAN JUAN)
Articulos de CENTRO CIENTIFICO TECNOLOGICO CONICET - SAN JUAN
Articulos(CICTERRA)
Articulos de CENTRO DE INVEST.EN CS.DE LA TIERRA
Articulos(IDEAN)
Articulos de INSTITUTO DE ESTUDIOS ANDINOS "DON PABLO GROEBER"
Citación
Gianni, Guido Martin; Davila, Federico Miguel; Echaurren Gonzalez, Andres; Fennell, Lucas Martín; Tobal, Jonathan Elías; et al.; A geodynamic model linking Cretaceous orogeny, arc migration, foreland dynamic subsidence and marine ingression in southern South America; Elsevier Science; Earth-science Reviews; 185; 10-2018; 437-462
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