@article{10272/8290,
year = {2008},
url = {http://hdl.handle.net/10272/8290},
abstract = {The Los Santos skarn shows several chemical and mineralogical features common to many other W-bearing
calcic mesozonal reduced skarn deposits. Early exoskarn consists of hedenbergite (Hd82-87), grossular (Grs53-
73) and Mo-rich scheelite. The mineral assemblage which formed during the cooling of the system is very
complex and is constituted mainly by subcalcic garnet, other hydrated silicates (amphibole, phlogopite,
prehnite, epidote-clinozoisite, chlorite, white mica and zeolite) and metallic mineralization with Mo-poor
scheelite. The aplitic granite is replaced by a calcic plagioclase and clinopyroxene endoskarn. Stockscheider,
breccias and fractures indicate a forceful emplacement and over pressure associated with volatile exsolution
from granite magma. The occurrence of zeolites indicates that the hydrothermal fluid circulation probably
communicated with the surface as in present-day geothermal systems},
title = {Secuencia paragenética del skarn de scheelita de Los Santos (Salamanca, NO España)},
title = {Paragenetic sequence of the Los Santos scheelite skarn (Salamanca, NW Spain)},
author = {Timón, S. M. and Moro, M. C.},
}