Modeling Trench Sediment‐Controlled Flow in Subduction Channels: Implications for the Topographic Evolution of the Central Andean Fore Arc-Reference-Cited by-同舟云学术

Modeling Trench Sediment‐Controlled Flow in Subduction Channels: Implications for the Topographic Evolution of the Central Andean Fore Arc

Published:2018-10 Issue:10 Volume:123 Page:9121-9135
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Cosentino N. J.¹²³^ORCID,Morgan J. P.⁴^ORCID,Jordan T. E.¹^ORCID

Affiliation:

1. Department of Earth and Atmospheric Sciences Cornell University Ithaca NY USA

2. Facultad de Ciencias Exactas, Físicas y Naturales Universidad Nacional de Córdoba Córdoba Argentina

3. Consejo Nacional de Investigaciones Científicas y Tecnológicas (CONICET) Centro de Investigaciones en Ciencias de la Tierra (CICTERRA) Córdoba Argentina

4. Department of Earth Sciences, Royal Holloway University of London Egham UK

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016109

Reference66 articles.

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3. Subduction zone decoupling/retreat modeling explains south Tibet (Xigaze) and other supra-subduction zone ophiolites and their UHP mineral phases

4. Subduction dynamics and the origin of Andean orogeny and the Bolivian orocline

5. Slow rates of subduction erosion and coastal underplating along the Andean margin of Chile and Peru

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