Eocene to Quaternary Deformation of the Southern Puna Plateau: Thermochronology, Geochronology, and Structural Geology of an Andean Hinterland Basin (NW Argentina)-Reference-Cited by-同舟云学术

Eocene to Quaternary Deformation of the Southern Puna Plateau: Thermochronology, Geochronology, and Structural Geology of an Andean Hinterland Basin (NW Argentina)

Published:2022-06 Issue:6 Volume:41 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

McMillan Mitchell¹^ORCID,Schoenbohm Lindsay M.¹²^ORCID,Tye Alexander³^ORCID,McMillan Malcolm F.⁴^ORCID,Zhou Renjie⁵^ORCID

Affiliation:

1. Department of Earth Sciences University of Toronto Toronto ON Canada

2. Department of Chemical and Physical Sciences University of Toronto Mississauga Mississauga ON Canada

3. Department of Earth and Environmental Sciences Utah Tech University St. George UT USA

4. School of Earth Sciences University of Melbourne Parkville Vic Australia

5. School of Earth and Environmental Sciences University of Queensland Brisbane Qld Australia

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022TC007252

Reference119 articles.

1. Pure and simple shear plateau uplift, Altiplano-Puna, Argentina and Bolivia

2. THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES

3. The role of inherited tectono-sedimentary architecture in the development of the central Andean mountain belt: Insights from the Cordillera de Domeyko

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