Browsing by Author "Reguilón Bragado, R. M."

Now showing items 1-2 of 2

Las mineralizaciones de U de la Carretona y Casa del Gallo En el granito de Albala (Câceres)

Reguilón Bragado, R. M.; Arribas, A.; Martín lzard, A.; Mangas, J. (Sociedad Geológica de España, 1996)

The U mineralizations that are estudied in this paper are hosted in Albalagranite.They are controled by late Hercinian vertical or subvertical faults, with an aproximate orientation of N30°E. The mineral association in ...
Minerales de tierras raras en las carbonatitas del Complejo Basal de Fuerteventura (Islas Canarias)

Mangas, J.; Pérez Torrado, Francisco J.; Martín Izard, A.; Reguilón Bragado, R. M. (Sociedad Geológica de España, 1996)

The Fuerteventura carbonatites appear in the Complejo Basal as veins, breccias and shear bands in the coastline between Puerto de la Pena and Cueva de Lobos, and in the Esquinzo ravine zone. These carbonatites are formed ...

Now showing items 1-2 of 2

Las mineralizaciones de U de la Carretona y Casa del Gallo En el granito de Albala (Câceres)

Reguilón Bragado, R. M.; Arribas, A.; Martín lzard, A.; Mangas, J. (Sociedad Geológica de España, 1996)

The U mineralizations that are estudied in this paper are hosted in Albalagranite.They are controled by late Hercinian vertical or subvertical faults, with an aproximate orientation of N30°E. The mineral association in ...
Minerales de tierras raras en las carbonatitas del Complejo Basal de Fuerteventura (Islas Canarias)

Mangas, J.; Pérez Torrado, Francisco J.; Martín Izard, A.; Reguilón Bragado, R. M. (Sociedad Geológica de España, 1996)

The Fuerteventura carbonatites appear in the Complejo Basal as veins, breccias and shear bands in the coastline between Puerto de la Pena and Cueva de Lobos, and in the Esquinzo ravine zone. These carbonatites are formed ...