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Gold
The rivers of Rio Muni are worked by local artisans using simple
panning and wooden sluice technologies. Previous commercial investigations
have concentrated on the three main areas of artisanal workings
- Coro, Aconibe, and Mongomo and there are several other known
occurrences that have been worked. Historical records are incomplete, but at least 2.3t of gold was
produced from the Coro area alone in the mid-70's.
The alluvial gold is relatively coarse grained, occurring as either
dendritic or rounded nuggets, mostly in the 350-180um size range,
although larger nuggets up to 4mm x 8 mm are relatively common.
The common occurrence of the gold with vein-quartz, clays, and
lateritic minerals attests to the proximity and variable types
of bedrock gold mineralisation which have yet to be delineated.
Diamonds
Heavy-mineral sampling results have identified zinc-rich chromites
in the Nsork area, similar to those found in the diamondiferous
lamproite dyke swarm at Mitzic (Gabon), 50km to the southeast.
Remote sensing and limited outcrop mapping show the dyke swarm
trending into the southeastern corner of Rio Muni. Furthermore,
exploration in Gabon for both gold and diamonds has identified
trails of indicator minerals and diamond right up to the southern
borders of Rio Muni. Detailed exploration work is required in
the Nsork area to establish the primary sources of the diamonds.
Columbo-tantalite
Mineralisation has been defined in the Aconibe and Ayamiken areas
by Nb and Ta soil anomalies and by the presence of heavy minerals
commonly associated with Nb-Ta-bearing pegmatites. Neither area
has been explored in great detail and thus they represent early
stage exploration prospects for pegmatites and skarn systems associated
with PanAfrican granitic intrusions. The Aconibe occurrence comprises
discrete, laterally extensive pegmatites that are also overlain
by eluvial and alluvial deposits yielding grades of 3.0 to 7.5kg/m3. Sample assays have demonstrated niobium-rich columbo-tantalite
(62.36% Nb205) with subordinate tantalum (18.74% Ta205).
Other mineral potential
Widespread lateritisation and indications of bauxitic laterite,
with grades up to 58.3% Al203, and 2.1 % to 5.3% SiO2, indicate some potential for bauxite. Anomalous values of base
metals, U, As, Ag, Mn and Mo have been detected in laterite above black shales
in the Noya Series which is part of the West Congolian foreland
basin. This has known base metal deposits immediately to the south
in Gabon, and is also equivalent in age to the Katangan sequences
of the Democratic Republic of Congo and Zambia. Basic intrusives
have been mapped in southern Rio Muni, that may be a northern
extension of the Kinguélé ultrabasics trend of northern Gabon,
which contains known Ni-PGE mineralisation. Serpentinised ultramafics
in central Rio Muni are as yet untested exploration prospects
with some potential for base metals and platinoid elements. |
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| Panning for gold |
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| Typical coarse gold from Coro |
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