@article{10272/13297,
year = {1996},
url = {http://hdl.handle.net/10272/13297},
abstract = {The late Hercynian Santa Coloma granodiorite intruded Paleozoic metasediments of upper Ordovician to Devonian age. Several forms of tungsten-bearing ores are found associated to the Santa Coloma granodiorite in the Central Pyrenees: veins, filled joints and skarns. Fluid inclusion study in quartz crystals from veins suggests that the mineralising fluid was a polysaline brine (22 wt% NaCI eq.) wich was trapped at 360 ±30 °C and 2.5 ±0.3 kbar, even the first mineralizing stage could be formed at higher temperatures (up to 500°C). Preliminary data of 8 MS of sulphides from skarn and vein mineralizations show values near 5 ± 1%o suggesting a sulphur of magmatic origin},
publisher = {Sociedad Geológica de España},
keywords = {Tungsten},
keywords = {Scheelite,},
keywords = {Hercynian},
keywords = {Vein},
keywords = {Skam},
keywords = {Pyrenees},
title = {Las mineralizaciones de wolframio asociadas a la granodiorita de Santa Coloma (Andorra)},
title = {Tungsten-bearing ores related to the Santa Coloma granodiorlte (Andorra)},
author = {Espinola, M. R. and Soler Gil, Albert and Arcos, D.},
}