| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4692548 | Tectonophysics | 2013 | 18 Pages |
Abstract
⺠The Gaspé belt results from the tectonic inversion of a former extensional basin ⺠Growth strata testify of normal motion during the Silurian to earliest Devonian ⺠Cross-sections integrate seismic data and are balanced for gravity and magnetism ⺠No efficient level of décollement ⺠A higher deformation zone is due to a vise effect between two basement blocks
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Nicolas Pinet,