Transcontinental retroarc sediment routing controlled by subduction geometry and climate change (Central and Southern Andes, Argentina)-Reference-Cited by-同舟云学术

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Transcontinental retroarc sediment routing controlled by subduction geometry and climate change (Central and Southern Andes, Argentina)

Published:2021-09-08 Issue:6 Volume:33 Page:3406-3437
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Research

Author:

Garzanti Eduardo¹^ORCID,Capaldi Tomas²^ORCID,Vezzoli Giovanni¹^ORCID,Limonta Mara¹,Sosa Numa¹³

Affiliation:

1. Laboratory for Provenance Studies Department of Earth and Environmental Sciences Università di Milano‐Bicocca Milano Italy

2. Department of Geosciences University of Nevada Las Vegas NV USA

3. Centro de Investigaciones Geológicas (CONICET) Universidad Nacional de La Plata La Plata Argentina

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12607

Reference208 articles.

1. Quantitative Analysis of Volcanic Lithic Fragments

2. Flexural-eustatic numerical model for drowning of the Eocene perialpine carbonate ramp and implications for Alpine geodynamics

3. The Argentine Precordillera: A foreland thrust belt proximal to the subducted plate

4. Flat-slab subduction and crustal models for the seismically active Sierras Pampeanas region of Argentina

5. From cylindrical to non‐cylindrical foreland basin: Pliocene–Pleistocene evolution of the Po Plain–Northern Adriatic basin (Italy)

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