| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9527087 | Tectonophysics | 2005 | 23 Pages |
Abstract
The main fault systems in the Permian to Cenozoic sediment fill of the CEBS are located above zones in the deeper crust across which a change in geophysical properties as P-wave velocities or gravimetric response is observed. This indicates that these structures served as templates in the crustal memory and that the prerift configuration of the continental crust is a major controlling factor for the subsequent basin evolution.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Magdalena Scheck-Wenderoth, Juliette Lamarche,