Effects of pre‐orogenic tectonic structures on the Cenozoic evolution of Andean deformed belts: Evidence from the Salar de Punta Negra Basin in the Central Andes of Northern Chile-Reference-Cited by-同舟云学术

Effects of pre‐orogenic tectonic structures on the Cenozoic evolution of Andean deformed belts: Evidence from the Salar de Punta Negra Basin in the Central Andes of Northern Chile

Published:2020-02-11 Issue:6 Volume:32 Page:1441-1462
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Res

Author:

Martínez Fernando¹^ORCID,López Cristopher¹,Parra Mauricio²

Affiliation:

1. Departamento de Ciencias Geológicas Facultad de Ingeniería y Ciencias Geológicas Universidad Católica del Norte Antofagasta Chile

2. Institute of Energy and Environment University of Sao Paulo Sao Paulo Brazil

Funder

Fondo Nacional de Desarrollo Científico y Tecnológico

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12436

Reference79 articles.

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

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

3. Sequence stratigraphy of the Mesozoic Domeyko Basin, northern Chile

4. Salar de Atacama basin: A record of compressional tectonics in the central Andes since the mid-Cretaceous

5. Clockwise block rotations along the eastern border of the Cordillera de Domeyko, Northern Chile (22°45′–23°30′S)

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