Andean Geology is becoming an English-language journal
This transition will be effective starting July 1, 2026. All submissions but obituaries and comments, and those part of special issues, will be required to be submitted in English
Call for Papers
Special Issue: Advances in Paleontology in Chile: Opportunities and Challenges for a Synthesis
Edited by:
- Marcelo Rivadeneira, CEAZA
- Enrique Bostelmann, Sernageomin
- Martín Chávez-Hoffmeister, CIAHN
- Joseline Manfroi, CIAHN
- Philippe Moisan, Universidad de Atacama
- Karen Moreno, Universidad Austral de Chile
- Sven Nielsen, Universidad Austral de Chile
- Ana Valenzuela-Toro, CIAHN
- Natalia Villavicencio, Universidad de O'Higgins
Submission status: Open between March 1, 2026, and November 30, 2026
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Special Issue: Geoethics in Chile and Latin America - Contextual reflections for responsible geoscience
Edited by:
- Luisa Pinto, Universidad de Chile
- Hernán Bobadilla, Politecnico di Milano
- Tania Villaseñor, Pontificia Universidad Católica de Chile
- Pablo Ramírez, Universidad de Chile
- Millarca Valenzuela, Universidad Católica del Norte
Submission status: Open between August 15, 2025, and April 30, 2026
Comment on 'Geochronology (Ar-Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from northern Chile of the central Andes' of Wörner et al. (2000)
Marcelo Garcia, Gerard Herail
Abstract
presented new and important geochronologic data on the Cenozoic magmatic rocks of northern Chile, and proposed magmatic and tectonic interpretations for them. Here we comment on one of their interpretations about the Miocene tectonic evolution of the Precordillera of Arica (Pampa Oxaya, ca. 18º30'S), a region referred by them as 'Oxaya Block'. According to their geochronological data and geomorphological observations, the area, which mainly consists of Lower Miocene ignimbrites of the Oxaya Formation, is interpreted as a large gravitationally collapsed rotational block. They interpret the collapse to have been produced by gravitational instability due to steepening of the western Andean slope during uplift of the Altiplano in an overall compressive regime.