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The central Andes

  • The Central Andes and the Atacama Desert represent a unique geological, climatic, and magmatic setting on our planet. It is the only place on Earth where subduction of an oceanic plate below an active continental margin has led to an extensive mountain chain and an orogenic plateau that is second in size only to the Tibetan Plateau, which resulted from continental collision. In this article, we introduce the history of the Central Andes and the evolution of its landscape. We also discuss links between tectonic forces, magmatism, and the extreme hyperarid climate of this land that, in turn, has led to rich deposits of precious ores and minerals.

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Author details:Gerhard Wörner, Taylor F. SchildgenORCiD, Martin ReichORCiD
DOI:https://doi.org/10.2138/gselements.14.4.225
ISSN:1811-5209
ISSN:1811-5217
Title of parent work (English):Elements : an international magazine of mineralogy, geochemistry, and petrology
Subtitle (English):elements of an extreme land
Publisher:Mineralogical Society of America
Place of publishing:Chantilly
Publication type:Article
Language:English
Date of first publication:2018/07/28
Publication year:2018
Release date:2021/10/22
Tag:active continental margin; hyperaridity; mineral deposits; tectonic shortening; uplift and erosion; volcanism
Volume:14
Issue:4
Number of pages:6
First page:225
Last Page:230
Organizational units:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Geowissenschaften
DDC classification:5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften
Peer review:Referiert
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