Imaging Variations in the Central Andean Mantle and the Subducting Nazca Slab with Teleseismic Tomography
The Nazca-South America convergent margin is marked by the presence of the Andean mountain belt, which stretches along the 8000-km long western margin of the South American plate. The subduction zone is characterized by significant along-strike changes in both upper plate structure and slab geometry...
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| Language: | en_US |
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The University of Arizona.
2015
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| Online Access: | http://hdl.handle.net/10150/556487 |