RT Journal Article
T1 Las mineralizaciones ferríferas del coto minero San Guillermo(Jerez de los Caballeros, Badajoz, España)
A1 Sanabria Orellana, Raúl
A1 Casquet, César
A1 Tornos Arroyo, Fernando
A1 Galindo Francisco, Mª del Carmen
AB Stratoid magnetite and skarn magnetite were mined at the San Guillermo mine district. Structural and texturalevidence suggest that they formed by replacement of older rocks in Variscan orogeny times during a protractedprocess that begun with fluid flow and stratoid magnetite formation along thrusts. This was followed by theBrovales pluton emplacement probably controlled by an oblique shear zone. Exo and endoskarns withmagnetite formed at this time, partly before and partly after complete crystallization of the pluton.
PB Sociedad Geológica de España
SN 0213-683X
YR 2005
FD 2005
LK https://hdl.handle.net/20.500.14352/49429
UL https://hdl.handle.net/20.500.14352/49429
LA spa
DS Docta Complutense
RD 4 may 2024