Análisis de la formación en el macizo metamórfico de Honrubia (SCE)
- González Casado, José Manuel
- Capote del Villar, Ramón
- Casquet Martín, César
ISSN: 0213-0696
Year of publication: 1984
Issue: 2
Pages: 75-94
Type: Article
More publications in: Revista de materiales y procesos geológicos
Abstract
Different tectonic microstructures developed during the hercynian orogeny in the Northernmost outcrop of the Sistema Central (Honrubia massif), are investigated in order to determine the macrostructure. We can distinguish: 1) Two important structures developed during F1, a synclinorium located in the SW and an antiform in the NE.2) Two ductile shear zones developed during F1, one of them being the prolongation of the Berzosa ductile low-angle thrust. 3) Several big Kink-Folds developed during F3. 4) A last deformation period (post. F3) with minor flods and Kink-Bands. And a las brittle faulting period with two principal trends, (NW-SE) and (SE-NE).