| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4688226 | Journal of Geodynamics | 2013 | 11 Pages |
Abstract
⺠Hyblean lithosphere consists of a serpentinized oceanic basement. ⺠Moho discontinuity represents a serpentinization front at a depth of 19 km. ⺠The proposed model extends westward from the Ionian basin to the Sicily Channel.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Fabio Carmelo Manuella, Alfonso Brancato, Serafina Carbone, Stefano Gresta,