@article{10272/8254,
year = {2008},
url = {http://hdl.handle.net/10272/8254},
abstract = {Fluorine-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 rock},
title = {El metasomatismo de flúor en la aureola de contacto del skarn de scheelita de Los Santos (Salamanca, NO España)},
title = {F-metasomatism in the contact-metamorphic aureole of the Los Santos scheelite skarn (Salamanca, NW Spain)},
author = {Timón, S. M.},
}