El anticlinal de Muel-Jaulín (Zaragoza) y su relación con la extensión cretácica

• Liesa, C.L. ^[1] ; Cortés, A.L. ^[1] ; Soria, A.R. ^[1]
  1. [1] Universidad de Zaragoza

     Universidad de Zaragoza

     Zaragoza, España

     
• Localización: Geogaceta, ISSN 0213-683X, Nº. 22, 1997 (Ejemplar dedicado a: 22ª Sesión Científica, Bilbao 1997), págs. 109-112
• Idioma: español
• Títulos paralelos:
  • The Muel-Jaulín anticline and its relation to the Cretaceous extension
• Enlaces
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• Resumen

  • The Muel-Jaulín region shows structures related to the Lower Cretaceous extension and the Tertiary compression respectively. Cretaceous normal faults constitute the northern border of the Aguilón Cretaceous basin, appearing Lower Cretaceous deposits (Villanueva de Huerva Fm.) to the South. During the Tertiary compression, minar normal faults were reactivated and folded. Main faults limiting the Cretaceous basin are slightly reactivated and they are responsible for the nucleation of the Muel-Jaulín anticline.