Diapiric ascent of silicic magma beneath the Bolivian Altiplano
Author:
Affiliation:
1. School of Earth Sciences; University of Bristol; Bristol UK
2. Instituto de Geociencias, Centro Mixto del Consejo Superior de Investigaciones Científicas y de la Universidad Complutense de Madrid; Madrid Spain
Funder
Natural Environmental Research Council
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/grl.50493/fullpdf
Reference31 articles.
1. The Bolivian Altiplano conductivity anomaly;Brasse;J. Geophys. Res.,2002
2. The mechanism of ascent and emplacement of granite magma during transpression: A syntectonic granite paradigm;Brown;Tectonophysics,1999
3. The 3-D gravity inversion package GROWTH2.0 and its application to Tenerife Island, Spain;Camacho;Comput. Geosci.,2011
4. The central Andean Altiplano-Puna magma body;Chmielowski;Geophys. Res. Lett.,1999
5. Growth of plutons by floor subsidence: Implications for rates of emplacement, intrusion spacing and melt-extraction mechanisms;Cruden;Phys. Chem. Earth Part A-Solid Earth Geodesy,2001
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