Distensión-comprensión en la cuenca de Campo Arañuelo. Implicación cortical
Pre-Arcosic detritic sediments (Paleocene-Eocene?) have been affected by normal faults; this distension phase, named Extremeña Phase, is related with Other similar regional observations. During Lower-Upper Miocene a new compressive phase cause thrusting with granite and metamorphic rocks of Gredos å...
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| Formato: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1990 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/270341 |
| Acesso em linha: | http://hdl.handle.net/10261/270341 |
| Access Level: | acceso abierto |
| Palavra-chave: | Normal faults Thrust faults Alpine tectonics Central Iberian Meseta Campo Arañuelo Basin |
| Resumo: | Pre-Arcosic detritic sediments (Paleocene-Eocene?) have been affected by normal faults; this distension phase, named Extremeña Phase, is related with Other similar regional observations. During Lower-Upper Miocene a new compressive phase cause thrusting with granite and metamorphic rocks of Gredos ånd Montes of Toledo overthrusting to Pre-Arcosic and Arcosic sediments. This phase is including at the Guadarama, and/or Neocastellana, Phases detected in eastern Central System massiff and other Meseta basins respectivaly. |
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