Gabros coroníticos en el macizo cristalino de Toledo
- Luis C. Barbero González 1
- Carlos Villaseca González 1
- 1 Geociencias. Medio-Ambiente
ISSN: 0213-683X
Année de publication: 1988
Número: 5
Pages: 66-68
Type: Article
D'autres publications dans: Geogaceta
Résumé
The Bastida gabbros massif is formed by olivine norites and piroxene gabbronorites. The metamorphic conditions are those of the intermediate to low pressure granulite facies, producing the coronitic texture that exhibit this gabbros