ANNUAL INFORMATION FORM ENDEAVOUR MINING CORPORATION

gold-pyrite mineralization. There is no significant component of refractory gold in the sulphide
zone at Adamus. The surface projection of identified mineralization trends northwest for
approximately 900m and is up to 400m wide. Within this zone there are seven distinct domains
of varying orientation and style that were used for the resource estimation.
The Bokrobo deposit comprises generally north-south trending, steeply west dipping auriferous
quartz veins hosted by strongly silica and iron carbonate altered, medium to coarse grained,
carbonaceous greywacke. A north-south trending dolerite dyke, dipping sub-vertically to the
west cuts the depth extension of the main vein. In the southern portion of the deposit, a westnorthwest
to east-southeast trending, steeply south-southeast plunging ‘dyke-like’ granitic
intrusion is cut by numerous auriferous quartz veins forming a sheeted vein system. In the north
of the deposit, mineralization generally occurs in a single lode, but in the south, the
mineralization occurs as two main lodes and a series of narrow stacked lodes around or in the
outer margins of the granite intrusion.
Akropon mineralization occurs within a wide zone of silicification associated with pyrite and
quartz veining with sericite as an accessory alteration mineral. The difference between the
apparent dip of the mineralization and bedding suggests an en echelon vein array or possibly
complex veining across a fold closure. Very little arsenopyrite has been identified at Akropon
and the mineralization in other deposits in this area are non-refractory, but metallurgical testing
is required.
At Nfutu mineralization occurs within quartz-pyrite veins and pyrite disseminations, typically
around veins, in the host rocks with silica, iron carbonate and sericite as the major alteration
minerals. Multiple flat-lying to shallowly east dipping and southeast plunging lodes occur as
stacked lenses that appear to thicken with depth. Mineralization is more prominent at the
graphitic phyllite-greywacke contact than in the competent greywacke. Only traces of
arsenopyrite were identified in drill core, and preliminary metallurgy shows that mineralization
is non-refractory.
At Aliva mineralization occurs as a series of stacked, shallowly east-dipping lenses subparallel to
the east dipping contact between carbonaceous phyllite footwall and greywacke hangingwall.
Mineralization appears to wrap around gentle to open folds and is associated with quartz veins
with sericite alteration and pyrite disseminations in the veins and surrounding host rocks. No
arsenopyrite has been identified at Aliva and the mineralization in other deposits in this area are
non-refractory. Metallurgical testwork on 76 samples of all material types returned over 90%
recovery.
At Avrebo the gold mineralization occurs in north-south to northeast-southwest trending,
subvertical to steeply east-dipping, strongly sericite-iron carbonate altered lodes within
metabasalt. Pyrite has been the only sulphide identified to date suggesting that the sulphide
gold component may be non-refractory. Metallurgical tests have not yet been completed.
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