Gabros coroníticos en el macizo cristalino de Toledo
- Luis C. Barbero González 1
- Carlos Villaseca González 1
- 1 Geociencias. Medio-Ambiente
ISSN: 0213-683X
Datum der Publikation: 1988
Nummer: 5
Seiten: 66-68
Art: Artikel
Andere Publikationen in: Geogaceta
Zusammenfassung
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