| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4715099 | Journal of Volcanology and Geothermal Research | 2011 | 21 Pages |
Abstract
⺠Luingo caldera is modelled by AFC-r as a mixture of 20:80 crustal/mantle melts. ⺠Presence of garnet in the source indicates crustal thickening (Coira and Kay, 1993). ⺠Major thickening event during the middle Miocene in the western portion of SCVZ. ⺠Major thickening event during the upper Miocene in the eastern portion of SCVZ. ⺠Distribution of volcanics and geochemistry help to envisage a broad arc in the SCVZ.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
S. Guzmán, I.A. Petrinovic, J.A. Brod, F.D. Hongn, R.E. Seggiaro, C. Montero, R. Carniel, E.L. Dantas, M. Sudo,