| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4715378 | Journal of Volcanology and Geothermal Research | 2006 | 17 Pages |
Abstract
The petrographic and geochemical characteristics of CBVF products suggest that the magma originated from a garnet-bearing lherzolite mantle source with asthenospheric characteristics, as a result of decompression, partial melting and ascent. These melts would have risen through a system of deep faults like the Gastre Fault System, following the last Quaternary glacial event.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Gabriela I. Massaferro, Miguel J. Haller, Massimo D'Orazio, Viviana I. Alric,