Observations on gold in the weathering profile at Garimpo Porquinho, an artisanal mine in the Tapajós Region, Brazilian Amazon. Geol. USP, Sér. cient. [online].
2006,
vol.5, n.2, pp. 1-11.
ISSN 1519-874X.
http://dx.doi.org/10.5327/S1519-874X2006000100001.
At
Garimpo Porquinho (Tapajós Province, Brazilian Amazon) gold-bearing
quartz veins containing sulfides occur in a narrow zone affected by
hydrothermal alteration. The artisanally mined veins are exposed in a
saprolite zone extending down at least 9 m to the fresh rock and are
covered by a 1 m thick residual soil. Lateral gold dispersion in the
saprolite is not noticeable whereas in the soil gold dispersion has been
observed as far as 2 m from the vein. Trace metals associated with gold
include Ag, Bi, As and Sb. Copper and lead, present in sulfides, can
also indicate the presence of gold. The study of gold particles in
different levels of the profile shows that gold has been affected by
weathering. In the upper levels of the profile, particles are smaller,
more rounded and pitted by dissolution. Grains of primary gold
containing up to 20% Ag are commonly exhibit silver-poor rims which may
penetrate deep into the grain. The interface between the Ag-poor rims
and the interior is very sharp. Such gold-rich rims likely formed by
self-electrorefining of electrum grains during weathering.
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