The Neogene to Quaternary evolution of the Neuquén Andes broken foreland forced by tectonic, climatic and surface processes (southern Central Andes)-Reference-Cited by-同舟云学术

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The Neogene to Quaternary evolution of the Neuquén Andes broken foreland forced by tectonic, climatic and surface processes (southern Central Andes)

Published:2023-11 Issue: Volume:131 Page:104620
ISSN:0895-9811
Container-title:Journal of South American Earth Sciences
language:en
Short-container-title:Journal of South American Earth Sciences

Author:

Messager Grégoire^ORCID,Huyghe Damien,Bonnel Cédric,Nivière Bertrand,Fasentieux Bertrand

Funder

Total SA

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference146 articles.

1. Foreland shortening and crustal balancing in the Andes at 30oS latitude;Allmendinger;Tectonics,1990

2. Erosion as a driving mechanism of intracontinental mountain growth;Avouac;J. Geophys. Res. Solid Earth,1996

3. Quaternary history of the piedmont reach of Río Diamante, Argentina;Baker;J. S. Am. Earth Sci.,2009

4. Episodic development of a convergent margin inferred from structures and processes along the southern Chile margin;Bangs;Tectonics,1997

5. Patagonian vegetation turnovers during the Paleogene-early Neogene: origin of arid-adapted floras;Barreda;Bot. Rev.,2007

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