Distensión-comprensión en la cuenca de Campo Arañuelo. Implicación cortical.

• Autores: Carlos Martín Escorza
• Localización: Geogaceta, ISSN 0213-683X, Nº. 8, 1990, págs. 39-42
• Idioma: español
• Enlaces
  • Texto completo (pdf)
• Resumen

  • 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.