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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| Format: | article |
| Status: | Published version |
| Publication Date: | 1990 |
| Country: | España |
| Institution: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repository: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/270341 |
| Online Access: | http://hdl.handle.net/10261/270341 |
| Access Level: | Open access |
| Keyword: | Normal faults Thrust faults Alpine tectonics Central Iberian Meseta Campo Arañuelo Basin |
| Summary: | 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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