Magnetotelluric image of the Chilean subduction zone in the Salar de Atacama region (23°-24°S): Insights into factors controlling the distribution of volcanic arc magmatism.

Author:

Ślęzak Katarzyna,Díaz Daniel,Vargas Jaime Araya,Cordell Darcy,Reyes-Cordova Felipe,Segovia María José

Funder

CONICYT

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference78 articles.

1. Tectonomagmatic characteristics of the back-arc portion of the Calama–Olacapato–El Toro fault zone, Central Andes;Acocella;Tectonics,2011

2. Tectonics, Climates, and Landscape Evolution of the Southern Central Andes: The Argentine Puna Plateau and adjacent Regions between 22° and 30° S;Alonso,2006

3. The role of inherited tectono-sedimentary architecture in the development of the central Andean mountain belt: Insights from the Cordillera de Domeyko;Amilibia;J. Struct. Geol.,2008

4. Large-Scale Distribution of Fluids in the Subduction Zone of Northern Chile—Constraints from Magnetotelluric Monitoring;Araya Vargas,2016

5. Fluid distribution in the Central Andes subduction zone imaged with magnetotellurics;Araya Vargas;J. Geophys. Res. Solid Earth,2019

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