Tectonic Subsidence Modeling of Diachronous Transition From Backarc to Retroarc Basin Development and Uplift During Cordilleran Orogenesis, Patagonian‐Fuegian Andes-Reference-Cited by-同舟云学术

Tectonic Subsidence Modeling of Diachronous Transition From Backarc to Retroarc Basin Development and Uplift During Cordilleran Orogenesis, Patagonian‐Fuegian Andes

Published:2022-10 Issue:10 Volume:41 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

VanderLeest Rebecca A.¹²^ORCID,Fosdick Julie C.²^ORCID,Malkowski Matthew A.³^ORCID,Romans Brian W.⁴,Ghiglione Matías C.⁵^ORCID,Schwartz Theresa M.⁶^ORCID,Sickmann Zachary T.⁷⁸^ORCID

Affiliation:

1. Department of Life, Earth, and Environmental Sciences West Texas A&M University Canyon TX USA

2. Department of Earth Sciences University of Connecticut Storrs CT USA

3. Department of Geological Sciences University of Texas at Austin Austin TX USA

4. Department of Geosciences Virginia Tech Blacksburg VA USA

5. Instituto de Estudios Andinos CONICET‐Universidad de Buenos Aires Buenos Aires Argentina

6. Geosciences & Environmental Change Science Center U.S. Geological Survey Denver CO USA

7. Institute for Geophysics Jackson School of Geosciences University of Texas at Austin Austin TX USA

8. Geosciences Department University of Texas at Dallas Richardson TX USA

Funder

Geological Society of America

American Association of Petroleum Geologists

Society for Sedimentary Geology

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021TC006891

Reference215 articles.

1. Proyecto Tranquilo‐Otway;Álvarez P.,2006

2. Quantitative Sedimentary Basin Modeling

3. A multidisciplinary study of the Lower Cretaceous marine to continental transition in the northern Austral-Magallanes basin and its geodynamic significance

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