Mina San Pedro (Genalguacil)
Irregular veins of copper, iron, cobalt, and nickel sulfides,bearing as gangue serpentine transformed to talc. Mineralizacion host rock is included in Garnet Lherzolites, on the outskirts of the Massif de Ronda.
Late talc mineralization and faulting generated breccias on host rock.
Origin: High-temperature magmatic sulphur segregations. These fluids were injected along fractures, where the alpine Massif of Ronda contact to kinzigite-granulitic gneis.
PICTURE GALLERIES
- MINERALS
- MINES
- CARDENILLO MINE (BENAHAVIS)
- EL CANDADO MINE (MÁLAGA)
- LA VICTORIA MINE (LA VIÑUELA)
- LOS ARENALES MINE (MIJAS)
- EL NICIO MINE (ESTEPONA)
- LA GALLEGA MINE (OJÉN)
- SAN PEDRO MINE (GENALGUACIL)
- SAN JUAN SHAFT (CARRATRACA)
- MARBELLA MINE (BENAHAVIS)
- TAJO LAS GRAJAS (ALHAURIN DE LA TORRE-MIJAS)
- MONTECORTO DISTRICT
- EL PEÑONCILLO MINE (MARBELLA-OJÉN)
- LOS LINAREJOS MINE (OJEN)
- CONCHITA MINE (ESTEPONA)
- LOS ANGELITOS AND LLANOS DE LA PLATA MINING DISTRICT (ALHAURIN DE LA TORRE)
- NATURAL GEOSITES