Miocene to Quaternary basin evolution at the southeastern Andean Plateau (Puna) margin (ca. 24°S lat, Northwestern Argentina)-Reference-Cited by-同舟云学术

Miocene to Quaternary basin evolution at the southeastern Andean Plateau (Puna) margin (ca. 24°S lat, Northwestern Argentina)

Published:2019-03-29 Issue:4 Volume:31 Page:808-826
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Res

Author:

Pingel Heiko¹,Alonso Ricardo N.²,Altenberger Uwe¹,Cottle John³,Strecker Manfred R.¹

Affiliation:

1. Institute of Geosciences Potsdam University Potsdam Germany

2. Departamento de Geología Universidad Nacional de Salta Salta Argentina

3. Department of Earth Science and Earth Research Institute University of California Santa Barbara California

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12346

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4. Alonso R. N. Gutiérrez R. &Viramonte J.(1984).Megacuerpos salinos cenozoicos de la Puna Argentina(Vol. 1 pp. 25–42). Presented at the IX Congreso Geológico Argentino IX Congreso Geológico Argentino.

5. Giant evaporite belts of the Neogene central Andes

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