Geochemical prospecting of emerald beryl in the Bonfim Farm (Lajes, Rio Grande do Norte State).
The recent discovery of a new
brazilian emerald occurrence, in the Rio Grande do Norte state, works on
geological mapping and soil geochemical prospecting were done in order
to know the definition of the deposit. The main geological structures
and the rocks with potential to host emerald mineralization are
orientated with general direction NNE-SSW, corresponding to de regional
shear zone direction, associated to the E-W lineaments of the
northeastern Brazil. Sampling and analysis of 1,351 soil samples were
utilized to drawing the geochemical maps of the main elements beryl,
chromium, potassium and lithium, as well as magnesium, sodium, nickel
and vanadium. Like the emerald is a Cr-rich beryl, such maps allowed the
determination of primary mineralized or with potential zones for
emerald deposits, that are related to sin-tectonic pegmatites. Areas
with chromium anomalies had values above 500 ppm, with maximum of 1794
ppm. For beryllium, anomalous values were considered those above 2.0
ppm, with the maximum value of about 9.5 ppm. Anomalies of potassium
(>1%) and lithium (>70 ppm), as well others (Mg, Na, Ni and V)
also helped in locating the zones of pegmatite intrusions. Additional
searches have been conduced to determine the ore reserves and grade of
the mineralization.
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