Metamorfismo regional e implicaciones geotermométricas en el alto valle del Lozoya (Sistema Central español).
Abstract
Regional metamorphism in metasediments and orthogneisses of a deep structural level in the Spanish Central System is described here. Two metamorphic events (M1 y M2) are found again. Almandine-rich garnet, staurolite and sillimanite related to M1 are conserved as relicts and point to a former Barrowian-like metamorphism. 1k is caracterized by the breakdown of staurolite and garnet and widespreading of * Departamento de Petrología. Facultad de Ciencias Geológicas. Universidad Complutnese. Madrid. 135 cordierite and sillimanite and by the development of migmatites. Peak temperatures during M2 have been determined with the garnet-cordierite and garnet-biotite geothermomethers. These data along, with topological reasons point to temperatures in the range 780 W 50~ C for a PL 5 Kb. Neverthless no granulites have been found here. 1.Downloads
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Published
1981-01-01
How to Cite
Tornos F. y Casquet C. (1981). Metamorfismo regional e implicaciones geotermométricas en el alto valle del Lozoya (Sistema Central español). Cuadernos de Geología Ibérica, 7, 135-150. https://revistas.ucm.es/index.php/CGIB/article/view/CGIB8181110135A
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