Revisión de la zonación metamórfica y los procesos de blastesis-deformación de la región de Somosierra (Sistema Central Español)
DOI:
https://doi.org/10.3989/egeol.87433-4590Keywords:
Metamorphic zones, porphyroblast growth, Spanish Central SystemAbstract
Mineral assemblage in metapelites and quarts segregations have been studied in the Somosierra massif. Proposed mineral zonas have a spatial relation with a major ducile shear zone, the Berzosa Fault (B.S.Z.), interpreted as a Hercynian synmetamorphic structure. The relationships beetwen the main crystal growth phase, and the Hercynian second deformation phase, have been stablished.
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