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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.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.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherSkarn depositsen_US
dc.subject.otherLos Santosen_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

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Atribución-NoComercial-SinDerivadas 3.0 España
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