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F-metasomatism in the contact-metamorphic aureole of the Los Santos scheelite skarn (Salamanca, NW Spain)

dc.contributor.authorTimón, S. M.
dc.date.accessioned2014-06-04T10:16:09Z
dc.date.available2014-06-04T10:16:09Z
dc.date.issued2008
dc.identifier.urihttp://hdl.handle.net/10272/8254
dc.description.abstractFluorine-bearing minerals such as chondrodite, norbergite, clintonite, chlorite and F-rich mica in the Los Santos dolomite marbles indicate that contact metamorphism was accompanied by F metasomatism. The low HF concentration of 10-2,46 to 10-3,03 mol/dm3 estimated using experimentally calibrated phlogopite and biotite fluorimeters, is similar to that calculated in other marbles and skarns related to magmatic or hydrothermal fluids equilibrated with a granite rocken_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherFluorineen_US
dc.subject.otherSkarn depositsen_US
dc.subject.otherTungstenen_US
dc.subject.otherLos Santosen_US
dc.subject.otherSpainen_US
dc.titleEl metasomatismo de flúor en la aureola de contacto del skarn de scheelita de Los Santos (Salamanca, NO España)en_US
dc.titleF-metasomatism in the contact-metamorphic aureole of the Los Santos scheelite skarn (Salamanca, NW Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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