Long-lived crustal damage zones associated with fault intersections in the high Andes of Central Chile
Long-lived, high-angle fault systems constitute high-permeability zones that can localize the upward flow of hydrothermal fluids and magma throughout the upper crust. Intersections of these types of structures can develop complex interference patterns, which constitute volumes of damaged rock (netwo...
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| Udgivet i: | Andean Geology |
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| Principais autores: | , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Servicio Nacional de Geología y Minería
2019
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| Fag: | |
| Online adgang: | https://www.redalyc.org/articulo.oa?id=173961655001 https://www.redalyc.org/journal/1739/173961655001/ https://www.redalyc.org/journal/1739/173961655001/html/ https://www.redalyc.org/journal/1739/173961655001/173961655001.epub https://www.redalyc.org/journal/1739/173961655001/movil https://doi.org/10.5027/andgeoV46n2-3106 |
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