| Autor: | J. Paricio Cardona, J. L. Simón Gómez |
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| Rok vydání: | 1988 |
| Předmět: | |
| Zdroj: | Estudios Geológicos. 44 |
| ISSN: | 1988-3250 0367-0449 |
| DOI: | 10.3989/egeol.88443-4545 |
| Popis: | We argue about micro and macrostructural data published in the paper in question supporting the hypothesis of some compressive regime being present in the Iberian Chain during the Miocene; at the same time, new data from other localities are presented. All these allow us to design a model of stress field characterized by a near N-S horizontal compression axis. After the LowerMiddle Miocene, E to ESE regional extension linked to the rifting of the eastern margin of the Iberian Peninsula is superposed. As a consequence, each point within the resulting stress field can register either compressive or extensive stress states at different times. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
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