| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4713257 | Journal of Volcanology and Geothermal Research | 2014 | 15 Pages |
Abstract
The Boa Vista felsic cone-sheet swarm, the youngest third episode, is formed by several hundreds of peralkaline ne-phonolitic sheets distributed within a circular surface about 11 km in radius. The cone-sheets conform a single general pattern characterized by a decreasing dip outward the structure, together with a constant dip of each individual sheet. The average inclination of sheets is around 40° in the sectors next to the centre of the structure whereas it is only about 30° next to its periphery. The magmatic focus of the sheets is located over 3 km deep almost coinciding with the convergence centre of a contemporary basic radial dike swarm.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Eumenio Ancochea, MarÃa José Huertas, Francisco Hernán, José Luis Brändle,