Arc-parallel shear deformation and escape flow in the mantle wedge of the Central America subduction zone: Evidence fromPwave anisotropy
Author:
Affiliation:
1. Institute of Geosciences, SFB574; Christian-Albrechts-University; Otto-Hahn-Platz 1,; D-24118; Kiel; Germany
2. Institute of Petroleum Geology and Geophysics, SB RAS; Prospekt Akademika Koptuga, 3; Novosibirsk; 630090; Russia
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/gc/gc1106/2010GC003325/2010GC003325.pdf
Reference74 articles.
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2. Shear wave anisotropy beneath Nicaragua and Costa Rica: Implications for flow in the mantle wedge;Abt;Geochem. Geophys. Geosyst.,2009
3. Constraints on upper mantle anisotropy surrounding the Cocos slab from SK(K)S splitting;Abt;J. Geophys. Res.,2010
4. Anisotropy and mantle flow in the Chile-Argentina subduction zone from shear wave splitting analysis;Anderson;Geophys. Res. Lett.,2004
5. Three-dimensional P wave velocity structure on the shallow part of the Central Costa Rican Pacific margin from local earthquake tomography using off- and onshore networks;Arroyo;Geophys. J. Int.,2009
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