Estudio del metamorfismo existente en torno al granito de Lumbrales ( Salamanca )
ISSN: 0211-8327
Year of publication: 1982
Volume: 17
Pages: 7-20
Type: Article
More publications in: Studia geologica salmanticensia
Abstract
The metamorphism around the granite of Lumbrales (Salamanca), develop two bands, one to north and other to south with increasing intensity towards the granite, with graduate passing to migmatites and latest to anatexis granite of Lumbrales. The metamorphism is of low-pressure, with develop of characteristic minerals: chlorite-biotite-andalusite (cordierite)-sillimanite-K feldspar; and cordierite-K feldespar in the migmatites.