Mineral Resources Potential - Geothermal Resources

SEPI* 3 Km
0-
Figure 30 Geology of part of the Kenticha mmetd field showing
zoning of pegmatites, as well as the location of areas mentioned i
A: area of bamn pgmatiw: B: area of Kilkile [I. Kilkile 111 and Bupo I1
pegmatites (bayl-columbite types): C: area of Kilkile 1 and Dermidama
Mineralogy and internal structure of the pegmatite bodies
The pegmatite unit in the Kenticha rare-rnetal field consists of a
multitude of large and small veins and dykes, most of which display
inward mineralogical and textural changes. The variability of internal
units and textural complexity increases padel to the degree of lim