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Weathering and hydrochemistry associated with the old mine workings at Fonte Santa (NE Portugal)
The quartz veins containing scheelite from Fonte Santa mine cut the Lower Ordovician quartzites. A
muscovite–biotite granite (G1) and a muscovite granite (G2), both S-type, crop out close to the Fonte Santa
mine and are related to the Moncorvo–Bemposta shear zone. The most altered samples of G2 show intense
muscovitization and microclinization and contain chlorite, columbite–tantalite, wolframite, W-ixiolite and
Fe-oxides. The tin-bearing granites contain 18 ppm (G1) and 73 ppm (G2) Sn. The most altered samples of
G2 correspond to a tungsten granite. The quartz veins contain muscovite, chlorite, tourmaline, scheelite,
pyrrhotite, pyrite, sphalerite, chalcopyrite, galena, arsenopyrite, iron oxides, Fe sulfates, phosphates of Pb, Fe
and Al. The Fonte Santa mine area was exploited for W between 1942 and 1982. At the end of November
2006, a flood event damaged the tailings dam of Fonte Santa mine, releasing contaminated material and
increasing contaminant levels in water within the area of influence of the mine. The waters related to the
Fonte Santa mine are poorly mineralized, with electrical conductivity of b965 μS/cm, and of a mixed type or
HCO3
− and SO4 2− types. Most pH values (5.0−8.5) indicate that there is no significant acidic drainage in the
region, as found in other areas. More acidic values (pH=3.4) were found in the mine's lagoon. Waters
associated with mineralized veins and old mine activities have Fe and Mn concentrations that forbid their
use for human consumption and agriculture. Natural Na, Mg and K water contents are associated with the
alteration of albite, chlorite and muscovite of country rock, while Ca with the W-bearing quartz veins.
Weathering agents are carbonic and sulphuric acids and the latter has a strong influence in areas draining
fine-grained mine tailings.
DOI:10.1016/j.gexplo.2010.05.001
The quartz veins containing scheelite from Fonte Santa mine area were exploited for W between 1942 and
1982. At the end of November 2006, a flood event damaged the dam land of Fonte Santa mine and metal
content of water increased. Fonte Santa mine area cuts the quartzites close to the Fonte Santa muscovite
granite. The granite contains quartz, microcline, albite, muscovite, chlorite, columbite-tantalite, volframite,
W-ixiolite and ilmenite. The quartz veins contain muscovite, chlorite, tourmaline, scheelite, pyrrhotite,
pyrite, sphalerite, chalcopyrite, galena, arsenopyrite, magnetite, jarosite, phosphates of Pb, Fe and Al. The
waters related to the Fonte Santa mine are poorly mineralized, with electrical conductivity < 965 μS / cm, of
mixed type or HCO3
- and SO4
2- types. These waters have Fe and Mn contents that forbid to use that for
human consumption and agriculture. Sodium, Mg and K water contents are associated with the alteration of
albite, chlorite and muscovite of country rock, while Ca is related to the W-bearing quartz veins.