| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4687975 | Journal of Geodynamics | 2015 | 91 Pages |
Abstract
- Geophysical data image a Pleistocene volcanic ridge offshore Capo Vaticano.
- Inverse 3D magnetic modeling reveals the volcano plumbing system at depth.
- The volcanic ridge formed at the intersection of a NW- and NE-trending normal fault.
- High-angle, NE-trending, SE-dipping normal fault formed during Pleistocene.
- The structural pattern controlled the pathways of ascending magma through time.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
M.F. Loreto, F. Pepe, R. De Ritis, G. Ventura, V. Ferrante, F. Speranza, I. Tomini, M. Sacchi,