| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445050 | Journal of Structural Geology | 2013 | 15 Pages |
Abstract
⺠Transition of extensional to compressional magnetic fabrics in an inverted sedimentary basin. ⺠Progressive transition of extensional structures to compression-related cleavage is seen. ⺠Palaeostress analysis from syn-sedimentary faults better constrains the extensional episode. ⺠Extensional magnetic fabrics are found when there is a certain distance to the cleavage front. ⺠Methodology applicable to the study of the conditions of tectonic inversion of other basins.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Belén Oliva-Urcia, Teresa Román-Berdiel, Antonio M. Casas, M. Felicidad Bógalo, M. Cinta Osácar, Cristina GarcÃa-Lasanta,