Las mineralizaciones ferríferas del coto minero San Guillermo (Jerez de los Caballeros, Badajoz, España)

dc.contributor.authorSanabria, R.
dc.contributor.authorCasquet Martín, César
dc.contributor.authorTornos, Fernando
dc.contributor.authorGalindo, Carmen
dc.date.accessioned2014-09-03T09:01:05Z
dc.date.available2014-09-03T09:01:05Z
dc.date.issued2005
dc.description.abstractStratoid magnetite and skarn magnetite were mined at the San Guillermo mine district. Structural and textural evidence suggest that they formed by replacement of older rocks in Variscan orogeny times during a protracted process that begun with fluid flow and stratoid magnetite formation along thrusts. This was followed by the Brovales pluton emplacement probably controlled by an oblique shear zone. Exo and endoskarns with magnetite formed at this time, partly before and partly after complete crystallization of the plutonen_US
dc.identifier.urihttp://hdl.handle.net/10272/8735
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherOre depositsen_US
dc.subject.otherMagnetiteen_US
dc.subject.otherSkarnen_US
dc.subject.otherOssa Morena zoneen_US
dc.subject.otherVariscanen_US
dc.titleLas mineralizaciones ferríferas del coto minero San Guillermo (Jerez de los Caballeros, Badajoz, España)en_US
dc.titleIron mineralizations of the San Guillermo mining district (Jerez de los Caballeros, Badajoz, Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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