Upper Plate Controls on the Formation of Broken Foreland Basins in the Andean Retroarc Between 26°S and 28°S: From Cretaceous Rifting to Paleogene and Miocene Broken Foreland Basins-Reference-Cited by-同舟云学术

Upper Plate Controls on the Formation of Broken Foreland Basins in the Andean Retroarc Between 26°S and 28°S: From Cretaceous Rifting to Paleogene and Miocene Broken Foreland Basins

Published:2020-06-29 Issue:7 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Zapata S.¹^ORCID,Sobel E. R.¹^ORCID,Del Papa C.²,Glodny J.³^ORCID

Affiliation:

1. Institute of Geosciences University of Potsdam Potsdam Germany

2. Cicterra CONICET‐University of Cordoba Cordoba Argentina

3. GFZ German Research Centre for Geosciences Potsdam Germany

Funder

Deutsche Forschungsgemeinschaft

Consejo Nacional de Investigaciones Científicas y Técnicas

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008876

Reference97 articles.

1. Combined thin-skinned and thick-skinned deformation in the central Andean foreland of northwestern Argentina

2. The Puncoviscana Formation of northwest Argentina: U-Pb geochronology of detrital zircons and Rb-Sr metamorphic ages and their bearing on its stratigraphic age, sediment provenance and tectonic setting

3. Rapid long-term erosion in the rain shadow of the Shillong Plateau, Eastern Himalaya

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

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