| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4688442 | Journal of Geodynamics | 2011 | 20 Pages |
Abstract
ⶠA continental-to-shallow-marine wedge-top depozone developed since the Late Miocene. ⶠThe Camporeale Basin is considered as the remnant of a wide wedge-top basin. ⶠAn “outer wedge-top sequence” has been defined in the Camporeale Basin.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
C. Gugliotta,