Characterization, origin, and evolution of one of the most eroded mafic monogenetic fields within the central Andes: The case of El País lava flow field, northern Chile

Author:

Torres IvanaORCID,Németh Károly,Ureta GabrielORCID,Aguilera FelipeORCID

Funder

CONICYT

Massey University

Universidad Católica del Norte

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference83 articles.

1. The first Morphologial analysis of scoria cones in the Negro de Aras monogenetic volcanic field, northern of Chile;Aguilera,2020

2. Geochemistry of the Salar de Atacama .1. Origin of the components and salt balance;Alonso;Rev. Geol. Chile,1996

3. Architecture and style of compressive Neogene deformation in the Eastern-Southeastern border of the Salar de Atacama basin (22°30'-24°15' S): a structural setting for the Central Andes active Volcanic Arc;Aron,2008

4. A 22,000-year record of monsoonal precipitation from northern Chile's Atacama Desert;Betancourt;Science,2000

5. The late permian peine and cas formations at the eastern margin of the salar de Atacama, northern Chile: stratigraphy, volcanic facies, and tectonics;Breitkreuz;Rev. Geol. Chile,1995

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