| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8908608 | Tectonophysics | 2018 | 37 Pages |
Abstract
Our results allow us to derive a model for the crustal structure of the Southern Central Andes. We propose that partial melts, marked by lower shear-wave velocity anomalies, are connected to shallower structural levels and reservoirs by brittle regions where dikes and exsolved fluids may propagate.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Diego González-Vidal, Anne Obermann, Andrés Tassara, Klaus Bataille, Matteo Lupi,