CONTINENTAL AFRICA
continued
Kibali
INTRODUCTION
Kibali is located in the north-eastern part of the Democratic Republic of the Congo (DRC) near the international borders with Uganda
and Sudan. The mine is located adjacent to the village of Doko, which located in the west of the project area. Kibali is approximately
210km by road from Arua, on the Ugandan border and immediately north of the district capital of Watsa. The operations area falls
within the administrative district of Haut Uélé in Orientale Province.
GEOLOGY
Kibali is located within the Moto Greenstone Belt, which consists of Archaean Kibalian volcano-sedimentary rocks and ironstone-
chert horizons that have been metamorphosed to greenschist facies. It is cut by regional scale north, east, north-east and north-west
trending faults and is bounded to the north by the Middle Archaean West Nile granite-gneiss complex and the south by the Upper
Zaire granitic complex.
The local geology consists of a volcano-sedimentary sequence comprising fine-grained sedimentary rocks, several varieties of pyroclastic
rocks, basaltic flow rocks, mafic-intermediate intrusions (dykes and sills) and intermediate-felsic intrusive rocks (stocks, dykes and sills).
This sequence is variably altered from slight to intense, such that in some cases the original lithology of the rock is unrecognisable.
Several major mineralised trends have been outlined by soil geochemistry data and by the distribution of known gold mineralisation.
The Kibali-Durba-Karagba Trend and the Gorumbwa-Kombokolo Splay are anomalous with respect to gold endowment and together,
define a mineralised, north-east-striking ‘mineralised corridor’, 1.5km wide and 8km long. These corridors host the deposits, of Kibali,
Sessenge, Gorumbwa, Karagba, Chauffeur and Durba and Pakaka.
The main Kibali deposit, which comprises the combination of Karagba, Chauffeur and Durba, is colloquially termed the KCD deposit
and hosts 79% of the grant’s Mineral Resource and 81% of the Ore Reserve (both for open pit and underground mining options). The
next largest deposit is Pakaka, which hosts some 6% of the Mineral Resource and 7% of the Ore Reserve. Currently only the KCD
deposit hosts an underground Ore Reserve and this constitutes 74% of the total KCD Ore Reserve.
Gold mineralisation is generally associated with structural features, resulting in tightly constrained zones which often host pods or lenses of
plunging mineralisation. Alteration is closely associated with the mineralisation and is typically carbonate-silica-albite with minor sulphide.
EXPLORATION
A large amount of exploration was undertaken by the previous owners of the Kibali project, Moto Goldmines Ltd, and this was focused
primarily on the KCD deposit. Since the acquisition of the concession area by AngloGold Ashanti and Randgold, the dominant
exploration targets have been the KCD underground area and upgrading the confidence in the proposed KCD open pit. Kibali’s
2014 exploration focused on Mineral Resource conversion drilling at Gorumbwa and Mofu satellite definition. A review of the down-
plunge 3000 and 5000 lode drilling at KDC was completed during the year, and indicated that only the 5000 lode had potential for
further exploration.
Regional work during the year took place at several targets, comprising mapping, soil, pit and trench sampling. RC drilling was
completed at Memekazi, 2km south-east of KCD, and at the Marakeke-Megi-Gekamine target area, 5km north of KCD. The Rhino-
Agbarabo IP survey completed in Q2 2014 generated several targets for follow-up work, with some positive results subsequently
returned and further work planned. Trenching at Aindi Watsa, 6km south-west of KCD, continued to confirm continuity of mineralisation,
which is still open to the west and down plunge. Recent field mapping at the Ikamva north-west and Kalimva targets has identified
previously unknown adits and ironstone units and the area, which is approximately 15km north of KCD, is considered to have good
potential.
At the regional target of Biriki-Belengo, 30km ENE of KCD, a programme of mapping, pitting, trenching and soil and stream sampling
identified four target areas for investigation. Additional targets such as Dri and Ndala were assessed and rejected for further work.
A thorough data review and development of a 3D lithological model was also completed at Mofu, 10km north-west of KCD. The
geological, mineralisation and weathering surface wireframes developed at Mofu were used in the updated Mineral Resource model
estimation of combined oxide, transitional and fresh material.
MINERAL RESOURCE AND ORE RESERVE REPORT
2014
64