Geochemistry and Gold Mineralisation Potential of Ungwan Rimi and Environs, Part of Wamba 210 Sw/Kurra Sheet 189 Sw, North-Central, Nigeria
Keywords:
Basement Complex, Geochemistry, Factor Analyses, Dispersion Pattern, Metal RatioAbstract
The Ungwan Rimi area is located at the southern fringe of North-Central Nigeria
and lies between (Lat. 8°34'19"E, 8°38'29"N and long. 8° 58'00"E, 9°00'45"N) near
Wamba town. The area is underlain by Precambrian Basement Complex rocks. A
A total of 20 samples were collected. Eight (8) are rocks samples, while twelve (12)
stream sediment samples. The samples were carried to the laboratory for XRF
analysis. The plutonic bodies observed from the geochemical classification plots
depict granite and granodiorite to diorite. The major elements variation diagrams
show that the rocks are essentially peraluminous, subalkaline, and calc alkaline to
tholeiitic series rocks. The granitic rocks as intrusions into pre-existing migmatite
gneisses are magnetic, while the migmatite gneisses are generally ferroans in
composition. The rocks are S-type, which strongly implies being derived from
sedimentary protoliths. The wide variation coexistence between the lithophiles
elements clearly suggest that the rocks were possibly formed from fractional
crystallization of melts derived from partial melting under the subduction-related
settings. The geochemical distribution patterns revealed the relative distribution of
pathfinder elements (Sn,Co,Sc,Ni,Cd,V,Ta,Nb,W,Hf, Ba,Th,U,Pt,Sb) of gold in the
area. Ungwan Rimi and environs were geochemically assessed using factor analysis
and correlation coefficient so as to establish the possible gold occurrence. The factor
analyses (Factor 1:Cl,S,Sc,Co,Ni,Y,Cd,Sn, Au; Factor 2: V,Ta,W,Sb,Nb;Factor
3: Ba, Hf, Th, and U) and co-efficient of correlation (Au vs Sn, Nbvs.Ta, Nbvs.Ta, W vs Ta,
Sbvs W) supported the possible association between the pathfinder elements of gold
in the area. The enrichment map derived from the metal ratio values for both the
rocks and stream sediments depict areas of better promise in terms of gold
potential in the area.
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