| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445188 | Journal of Structural Geology | 2011 | 19 Pages |
Abstract
⺠We collected fracture data in an oblique inversion anticline. ⺠Fractures are neither parallel nor perpendicular to the strike of the study fold. ⺠Fractures mostly developed during Early Cretaceous extension. ⺠Syn-inversion fractures are parallel and perpendicular to the shortening direction. ⺠Inherited extensional fractures were reactivated as strike-slip faults.
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Geology
Authors
S. Tavani, J. Mencos, J. Bausà , J.A. Muñoz,