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 a...
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1990 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18160 |
| Acceso en línea: | http://hdl.handle.net/10272/18160 |
| Access Level: | acceso abierto |
| Palabra clave: | Normal faults Thrust faults Alpine tectonics Central Iberian Meseta Campo Arañuelo Basin |
| Sumario: | 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 and Montes of Toledo overthrusting to Pre-Arcosic and Arcosic sediments. This phase is included at the Guadarama, and/or Neocastellana, Phases detected in eastern Central System massif and other Meseta basins respectively |
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