| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1781549 | Planetary and Space Science | 2011 | 12 Pages |
Abstract
The rift is formed by several pull-apart basins developed due to the reactivation of previously formed tectonic structures. The strain spatial distribution and the overall geometry are consistent with a roughly East-West left-lateral shear transfer zone between two different lithospheric blocks.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geophysics
Authors
David Alegre Vaz,