Agbaou is located in southern Côte d’Ivoire approximately 200km north of Abidjan, the economic capital (and erstwhile political capital) of the country. The mine is connected to the national electrical grid by a 15km, 91kV electrical transmission line and substation at site and the permit, which comprises the mine area, is reached by tarred and secondary gravel roads.
Alluvial gold has been known and exploited by local artisanal miners (colloquially ‘orpailleurs’ in the region) for many years. Gold mineralization, in bedrock, was first reported at Agbaou during the late 1980s, while the ground was held by a joint-venture between BHP and SODEMI. Significant exploration was undertaken between 1988 and 1994, including regional and detailed soil sampling, pit sampling, ground geophysics and a programme of eight diamond drill-holes over 1,680m (210m/hole). However, BHP allowed its permit to lapse and, between 1996 and 2000, the property was held by Diversified Mineral Resources (DMR). DMR was subsequently taken over by Hargraves Resources in 1999, which undertook an exploration programme that included semi-regional soil sampling, pit sampling, 36 RAB holes over 1,682m (average 47m/hole) and 203 RC drill holes over 22,149m (109m/hole).
Hargraves was acquired by Durban Roodeport Deep in late 1999. However, the permit was withdrawn by the government on the grounds of insufficient expenditure and, on 27 November 2003 following the completion of a bidding process, the Ministry of Mines and Energy for Côte d’Ivoire granted the Agbaou exploration permit to Etruscan Resources. Endeavour purchased Etruscan by degrees in 2009 and 2010, after which Etruscan’s name was changed to Endeavour.
Commercial production was achieved at Agbaou in January 2014.
Côte d’Ivoire is almost completely underlain by Precambrian rocks of the Leo-Man shield. The north-south trending Sassandra Fault marks the boundary between the Archean Kenema-Man domain, along the western country border and the Birimian Baoule-Mossi domain.
The Agbaou area is underlain by rocks of the Archean-Proterozoic Man Shield, which forms the southern half of the larger West African Craton. The shear-zone hosted gold mineralization of the Agbaou deposit occurs within a sheared volcano-sedimentary succession that was subjected to lower green-schist facies metamorphism, forming the Birimian age Oumé-Fetekro Greenstone Belt, surrounded by granodioritic intrusions. At Agbaou itself, the greenstone belt is folded into an antiform and the Agbaou deposit lies near the hinge of the fold, on the eastern limb.
Gold occurs in a mesothermal auriferous sulphide (pyrite + pyrrhotite) assemblage associated with quartz veins. The quartz veins are characterized by a wide range of quartz-vein types, brecciation, boudinage, sericitic and carbonate alteration. However, the mineralized quartz veins have a very distinctive texture that has been described as ‘mottled’ and are easily identifiable in the drill intersections and pit mapping.
The Agbaou operation comprises a conventional open pit, selective mining method (using BCM as its mining contractor) followed by conventional gravity/CIL processing.
The Agbaou plant is designed to recover gold from a variably weathered orebody at a total treatment rate of 1.3–1.6 Mtpa. The average feed grade for Agbaou over the life of operations is expected to be 2.4g/t (cf an average resource grade of 2.36g/t and an average reserve grade of 2.34g/t; see Exhibit 6). The comminution circuit of the process plant is composed of a primary jaw crusher, followed by SAG and ball mills. A dedicated gravity circuit consists of a concentrator, intensive cyanidation package and an electro-winning cell. The rest of the milled product is processed in the CIL circuit. The CIL tails slurry undergoes cyanide destruction prior to disposal in the tailings dam. Loaded carbon is acid washed and rinsed prior to elution. The electrolyte leaving the elution circuit undergoes electro-winning where gold sludge is produced. The sludge is dewatered using a pot filter and dried in a drying oven ahead of smelting. Fluxes are added to the dried gold sludge and the mixture placed in the smelting furnace. After smelting the furnace crucible contents are poured into cascading moulds. The gold bars are cleaned, sampled, labelled and prepared for shipping.
An ongoing exploration programme initiated in 2016 is focused on the North and South Pit extensions, the Agbaou South target, and on generating targets beyond current resource boundaries to replenish otherwise depleting reserves.
Agbaou’s 2017 exploration programme amounted to US$6m, totalling 31,400m of drilling. The primary objective was to conduct in-pit drilling at the North Pit and to test gold in soil anomalies on parallel shear zones. The campaign at the North Pit confirmed that its mineralisation extends at depth with occurrences of higher grade intercepts.
A US$4m exploration programme, totalling approximately 16,000m, has been planned for 2018 with the aim of delineating the depth potential of the North Pit (with the goal of delineating a resource) and further investigating targets on parallel trends.
Karma is located in north central Burkina Faso, 20km east of the city of Ouahigouya and approximately 185km northwest of the capital, Ouagadougou. It comprises eight exploration permits (Kao Nord, Kao Sud, Youba, Rounga, Tougou, Bogoya, Bonguirga and Namissiguima-Ouest) and the Karma exploitation permit. The Karma mine was acquired by Endeavour in 2016 and announced first gold production in April 2016. It includes six identified gold deposits and is a shallow open pit with no blasting required and a low strip ratio. Commercial production was declared on 1 October 2016.
The geology of Burkina Faso may be divided into three major litho-tectonic domains: a Paleoproterozoic (Birimian) basement underlying most of the country; a Neoproterozoic sedimentary cover developed along the western, northern and southeastern portions of the country; and a Cenozoic mobile belt that forms small inliersin the northwestern and extreme eastern regions of the country.
Karma is located in the Paleoproterozoic Baole-Mossi domain (see Tabakoto, above) and, within this, on the regionally east-west trending Goren greenstone belt, which is one of the larger Birimian greenstone belts in central north Burkina Faso. Local geology consists of a folded sequence of greywacke, siltstone, shale and volcanoclastic rocks. The western margin of the project area contains a broad, north-south magnetic lineament that is interpreted as a first-order, crustal scale, sinistral, shear zone named the Ouahigouya Shear Zone, which branches into a series of north-east trending sub-shears that cross the Karma property and extends to the south into the Houndé Greenstone Belt. Regional gold metallogenesis is tightly constrained to the Eburnean Orogeny between 1.98–2.13bn years ago. At least six mineral deposits have been defined on the property, including Kao, North Kao, Goulagou I, Goulagou II, Nami and Rambo.
The Karma deposits may best be described as structurally controlled, orogenic, hydrothermal deposits. Elements of stratigraphic control may result from mineralisation/alteration being channelled along specific structural/lithological controls such as competency contrasts between intrusive and sedimentary rocks that have affected porosity and fluid flow.
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The Kao deposit is composed of a structurally controlled alteration and veining system. The bulk of the highest grades and thickest intercepts occur along a northeast dipping set of structures and, in particular, at their intersections with a dominant north-south structure. The structures are weakly to intensely foliated, hydrothermally altered and are host to multiple generations of quartz-sericite-pyrite-arsenopyrite veining. A combination of arsenopyrite and the presence of quartz veining generally correlate with higher gold grades.
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The North Kao deposit is predominantly intrusive-hosted and consists of a stacked sequence of structurally-controlled tabular bodies, defined by pervasive quartz-sericite-pyrite alteration, breccia and locally distributed stockwork, shear and extension veining. Gold is closely associated with each of these features, with the sheared breccia and quartz-sericite-pyrite veins carrying the highest grades.
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Goulagou I consists of up to 10 discrete lenses of gold mineralised rock over an east-west strike length of 2.1km, ranging from 5–40m thick and dipping near-vertically. It is open along strike and down dip below 200m.
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Goulagou II is similar to Goulagou I, except that it consists of three to five steeply dipping lenses, with widths ranging from 5–30m over 2.4km of east-west strike. Higher grade, steeply plunging shoots occur at distinct flexures along strike.
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Rambo Main comprises several relatively small mineralised lenses with the main zone containing a steeply plunging mineralised shoot. Thicknesses of the mineralised zones range from c 2.5–25.0m and exhibit good continuity. The deposit is open to the east and down dip.
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Nami is composed of three mineralised lenses with shallow dips towards the west-southwest. The strike length of the deposit is c 550m, with a down plunge extent of 300m and thicknesses ranging from c 2.5–25.0m, with good continuity. Again, the deposit is open to the west, north and south.
The Karma mine plan envisages the development of five pit areas in sequence to provide the ore feed for heap leach operations. The mining method is conventional open pit mining with medium-sized equipment (eg 90t capacity haul trucks) with target ore production during the life of the mine of 4.0Mtpa from no more than two open pits at any one time. As is typical for open pit operations in West Africa, three types of material are being mined – oxide, transition and sulphide material. The oxides and some of the transition material do not require blasting. However, harder, deeper rocks do.
Karma’s process plant consists of two crushing circuits (one for soft ore and one for hard ore), followed by a process of agglomeration, stacking, heap leaching with cyanide solution, gold adsorption, elution and smelting. Note that some of the sulphide material at Goulagou and Kao is of a refractory nature and therefore unsuitable for heap leaching. In addition, a minor amount of preg-robbing material may also reside in some of the ore, with the result that this material will be stockpiled for processing at the end of the life of the mine.
Karma consists of six contiguous exploration permits (Goulagou, Rambo, Kao, Rounga, Youba and Tougou) totalling more than 856km2 and including more than 45 high-priority targets with high grade rock values associated with gold-in-soil anomalies and historical workings that remain untested to date.
Karma’s 2017 exploration programme amounted to US$3m, totalling 41,520m of drilling focused primarily on the northeast extension of the North Kao deposit and on the Yabonsgo target. Drilling at the North Kao deposit extension confirmed the deposit’s continuity. A US$2m exploration programme totalling approximately 32,000m has been planned for 2018 with the aim of delineating indicated resources at both North Kao and Yabonsgo in addition to near-mill targets such as Rounga and on the recently acquired Zanna exploration licence.
Ity is located close to the Liberian and Guinean borders, approximately 700km northwest of Abidjan, and is accessible by paved road via Yamoussoukro or by aeroplane via Man. It has the longest history of any gold mine in Côte d’Ivoire and is closely linked to the local Yacouba community, which is based in eight villages around the project site.
Copper and gold were first discovered near the village of Ity in the 1950s by France’s Bureau Minière de la France Outre-Mer. However, initial attempts at recovery were unsuccessful owing to the fineness of the ore rheology (ie its flow and deformation). In 1983, the Société Minière d’Ity was incorporated to develop the Flotouo deposit, which poured its first gold in 1991. Substantial subsequent exploration was then responsible for identifying many other deposits in the region.
The project, as it is currently constituted, comprises a total of nine prospect areas, including four that have been, or are being, mined (namely Mont Ity, Ity Flat, ZiaNE and Walter), two near-mine deposits (Gbeitouo and Daapleu), two rock waste dumps (Teckraie and Verse Ouest) and a discontinued heap leach pad (Aires). All lie within an area approximately 5km by 3km.
The Mont Ity deposits are located in the Lower Proterozoic Birimian Formation of the Toulepleu-Ity klippe (a remnant portion of a sheet-like body after it has been isolated by the erosion of the surrounding rock), which is a small remnant of the Birimian in the West African Craton.
The Ity area itself is characterised by a series of granodiorite intrusions into a sedimentary sequence of volcano-sediments and carbonates, with all formations having been subjected to regional metamorphism. The Ity Gold project deposits are orogenic gold deposits and generally described as skarn or shear zone styles of mineralisation. Skarn deposits within the Ity Gold project include Mont Ity, Ity Flat, ZiaNE and Walter and are developed at the contacts of the granodiorite with the carbonates. Similarly, the Teckraie, Verse Ouest and Aires assets are derived from material originally mined from skarn deposits. The Daapleu deposit is characterised by the presence of a rhyolitic intrusive surrounded by a package of volcano-sediments (the rhyolite is locally known as ‘daaplite’ and is microgranular, schistose and rich in micas).
The main lithologies within the Ity project area are laterites, saprolites, metavolcanic sediments, carbonates, granodiorites, daapleu rhyolites, diorites and skarns. The mineralised portions of the reduced saprolites correspond to the decarbonation of marble and exoskarn (ie a skarn formed from a sedimentary, rather than igneous, rock). The reduced saprolites are the transition zone between oxidised material and the fresh rock. The oxidised saprolites form the major part of the mineralisation at Mont Ity. The mineralisation was originally skarn but has subsequently undergone severe supergene alteration, which was enhanced by the dissolution of the sulphides. In this case, the alteration was also responsible for the generation of karst, into which the saprolite material then collapsed.
In the meantime, the Daapleu and Gbeitouo deposits resemble typical shear zone deposits of the West African granite-greenstone terrane between two contrasting lithologies. Both deposits are associated with the major regional shear zone, but developed on secondary structures. The gold mineralisation is mesothermal in origin and occurs as free gold in quartz vein stockworks and zones of silicification, associated with arsenopyrite and, to a lesser extent, pyrite and antimony. It is found in linear shear zones in, or near, the contacts between two different rock types that show evidence of shearing. Alteration is weak to severe, depending on the development of the system. Mineralisation may also be spatially related to the emplacement of intrusives.
Until recently, the Ity complex has been operated as two conventional open pit mines (Mont Ity and Tontouo) using articulated 40t trucks and hydraulic backhoes or 80t front shovel excavators. Limited drill and blast activities were required, as the material that was mined was largely oxidised clay and/or laterites.
There remain several years of heap leach reserves to be mined and additional opportunities exist to increase these reserves with known oxidised material. Ore facies not containing sulphide are substantially free milling and do not show any preg-robbing characteristics. However, the ore facies containing sulphide are partially refractory and direct cyanidation yields a lower gold recovery. As a result, as oxide ore has become depleted Endeavour has studied alternatives for the development and exploitation of the deeper, sulphide ores, including considerable metallurgical testwork to confirm the response to a CIL plant by ALS in Kamloops, British Columbia. In particular, testwork results have indicated that Daapleu primary ores contain significant arsenopyrite and that a standard cyanide leach will extract only 60–65% contained gold, whereas the oxide ores are free milling with leach extraction of 90–96%.
In conclusion, the Ity CIL plant will process a range of ore types (oxide, transition and fresh) with variable ore characteristics, gold grades and metallurgical treatment requirements. Note that the primary ores are significantly more competent than the oxide ores. Key project and ore specific design criteria that the plant must meet are:
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4Mtpa of blended ore; 51% primary and 49% oxide (LOM)
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Single-stage primary crushing to produce a crushed product size of 100% passing (P100) 326mm (P80 of 166mm)
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Two-stage SAG/ball milling to produce a P80 grind size of 75µm
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A CIL circuit incorporating eight CIL tanks
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Elution, electro-winning and smelting to produce doré
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Tailings pumping to the tailings storage facility (TSF)
Electrical power will be supplied from the Ivoirian national grid and back-up diesel generators.
BFS and subsequent optimisation
Endeavour completed a bankable feasibility study on the Ity CIL project in December 2016. Successful subsequent exploration then allowed it re-size the plant and to update the BFS in 2017 and to increase annual throughput from 3Mtpa to 4Mtpa. A summary of the optimised study relative to the original BFS is provided in the table below:
Exhibit 5: Ity CIL project optimised study vs original BFS
|
2016 feasibility study |
2017 optimisation study |
Change (units) |
Change (%) |
Mining schedule |
|
|
|
|
Mine life |
12 |
15 |
3 |
25 |
Total material moved (kt) |
125,448 |
166,752 |
41,304 |
32.9 |
Total waste moved (kt) |
85,087 |
109,559 |
24,472 |
28.8 |
Total ore mined (kt) |
40,362 |
57,194 |
16,832 |
41.7 |
Stripping ratio |
2.11 |
1.92 |
-0.19 |
-9.1 |
Grade (g/t) |
1.42 |
1.57 |
0.15 |
10.3 |
Contained gold (oz) |
1,845,275 |
2,883,339 |
1,038,064 |
56.3 |
|
|
|
|
|
Processing schedule |
|
|
|
|
Total ore processed (kt) |
41,042 |
57,000 |
15,958 |
38.9 |
Grade (g/t) |
1.42 |
1.57 |
0.14 |
9.9 |
Contained gold (oz) |
1,881,667 |
2,872,370 |
990,704 |
52.7 |
Recovery (%) |
83.1 |
85.8 |
2.7 |
3.3 |
Gold produced (oz) |
1,563,322 |
2,464,485 |
901,163 |
57.6 |
Payable gold (oz) |
1,561,759 |
2,462,020 |
900,261 |
57.6 |
Payable silver (oz) |
3,136,196 |
4,943,761 |
1,807,565 |
57.6 |
|
|
|
|
|
Operating costs |
|
|
|
|
Mining (US$/t ore) |
7.81 |
8.30 |
0.49 |
6.3 |
Processing and maintenance (US$/t) |
10.56 |
11.96 |
1.41 |
13.3 |
Site G&A (US$/t) |
2.81 |
2.23 |
-0.58 |
-20.8 |
Total operating costs (US$/t) |
21.05 |
22.52 |
1.47 |
7.0 |
|
|
|
|
|
Capex |
|
|
|
|
LOM capex (US$000's) |
364,000 |
452,500 |
88,500 |
24.3 |
|
|
|
|
|
Economics* |
|
|
|
|
Post-tax IRR (%) |
36 |
40 |
4 |
11.1 |
Post-tax NPV5 |
411 |
710 |
299 |
72.7 |
Payback period (years) |
2.1 |
1.8 |
-0.3 |
-14.3 |
Source: Endeavour Mining, Edison Investment Research. Note: *Company calculated. Totals may not add up owing to rounding.
In 2017, Endeavour invested US$14m in the Ity exploration programme, totalling 58,500m of drilling. Following the successful drilling campaigns at the Bakatouo, Ity, Daapleu and Verse Ouest deposits, and the recent Le Plaque discovery, more than 1Moz of indicated resources were added to the CIL project as a result.
Given its strong prospectivity and potential to extend the life of the CIL project, Ity has recently accounted for the largest single portion of Endeavour’s exploration budget. Most recently, this has involved in-fill drilling at the Daapleu and Mount Ity deposits, in-fill and extension drilling at the new Bakatouo and Colline Sud discoveries and initial drilling on strong auger anomalies such as the Yacetouo and Vavoua targets.
In 2018, Endeavour will invest a further US$2m in an exploration campaign to further explore the Le Plaque target in addition to several other near-mill opportunities, with the continued aim of delineating additional resources for the CIL project. An additional US$5m will be dedicated to greenfield targets within the 100km corridor along the Ity mine.
Endeavour has a 90% interest in the 1,000km2 Houndé project, which is located approximately 250km southwest of the capital of Burkina Faso, Ouagadougou, 2.7km from a paved highway, as close as 200m to a 225kV power line and 25km from railway line that extends to the port of Abidjan (the commercial capital of Côte d’Ivoire).
Mineral exploration in the Houndé area began in 1939 by the Bureau de Recherches Geologiques et Minières and the Bureau de Mines et de la Géologie du Burkina Faso and continued until 1982. Endeavour began its interest in the project with a 40,534m in-fill programme over the Vindaloo and Madras NW zones in 358 holes (average 113m/hole) in late October 2012. Including previous owners of the project area, during the period from 2007 to 2013, Endeavour, Avion, Goldbelt and African Barrick (now Acacia Mining) completed 751 core and RC holes over 103,677m (average 138m/hole) along the trend of the Vindaloo and Madras NW zones (see below).
Rocks in the core Vindaloo and Madras NW zones are north- to northeast-trending greenschist-metamorphosed intermediate volcanics and sediments that are intruded by later gabbro sills and dykes. The Vindaloo zones, in particular, are hosted by Proterozoic age, Birimian Group, intensely sericite- and silica-altered mafic intrusion and similarly altered, sheared and altered intermediate to mafic volcanoclastics and (occasionally) sediments. The mineralisation is often quartz stockwork-style and is weakly to moderately pyritic. Drilling along the c 1.2km strike of the central core of the system has defined a coherent, gold-mineralised zone that has been traced to at least 350m depth. The entire mineralised package strikes north-northeast and dips steeply to the west to vertical. Mineralisation to the north and south varies from weak to quite strong over relatively short vertical and/or horizontal distances, leading to nodes of higher-grade mineralisation connected by zones of weaker mineralisation. The Vindaloo trend has been drill tested for a distance of c 7.7km along strike. The Vindaloo deposit itself comprises a group of closely spaced gold-mineralised structures that represent a c 4.8km section of the Vindaloo zone and a 0.9km-long section of the Madras NW zone and is open both along strike and at depth. In addition, within the modelled area, there are indications of further hanging wall, parallel gold zones and gold mineralised cross-structures.
Primary ores make up 82% of the deposit, with saprolite and transition ores the remaining 18%. Primary ores from the Vindaloo pit make up 80% of those primary ores and are the major component of the Houndé deposit. Pits have been designed for Vindaloo main, south and north, Vindaloo 1 and Vindaloo 2 and Madras NW south and Madras NW north.
Houndé’s processing plant comprises a 3.0Mtpa CIL plant and semi-autogenous ball mill crusher milling circuit to produce a fraction of 80% passing 90µm grind size. Ground fresh ore is then fed to continuous centrifugal gravity concentrators to recover free and occluded gold in heavy particles (pyrite) to a low mass gravity concentrate. This concentrate is reground to 80% passing 10µm grind size and fed to a concentrate leach circuit. Gravity concentration tails plus saprolite ore are thickened and fed into a standard CIL, elution and electro-winning circuit, with leach tails passing into a cyanide destruction (SO2/air technology) process before being pumped to storage.
The tailings storage facility has capacity for 25Mt and has the potential to provide storage for up to 50Mt of tailings by increasing the embankment height and/or adding a saddle embankment to the south of the facility. The TSF is not lined owing to a near-surface, clay rich layer that limits the migration of tailings fluids away from the site. It is designed to withstand up to a one in 100 year wet event and will need to be covered at the end of operations to isolate the facility and prevent the migration of tailings.
Houndé’s water requirements are met from TSF decant, pit dewatering (including precipitation on the pit area) and runoff from the ROM pad and stockpiles with any shortfall supplied from a water storage dam fed by a water harvesting dam. Groundwater resources are very small, but are sufficient for potable water use.
The Houndé exploration tenement covers more than 1,075km2. Following a two-year period of no exploration, activities resumed in 2017 with US$5m spent on a drilling programme totalling approximately 76,000m. The campaign yielded positive results with the discovery of high-grade intercepts at both the Kari Pump target and the Sia/Sianikoui targets. In 2018, Houndé will be a key focus for Endeavour with a US$9m exploration programme (20% of the group total) totalling approximately 125,000m planned with the aim of drilling the entire Kari anomaly and delineating a maiden resource.
Kalana is located in southwestern Mali, approximately 250km south of the capital, Bamako, near the border with Guinea. It covers an area of 387.4km2, within which the Kalana Main project is located near the centre of the northern part of the permit, 1km from the town of Kalana.
Between 1985 and 1991, the Kalana mine was operated by the Société de la mine d'or de Kalana, which used two vertical shafts to mine flat dipping quartz veins and stockwork mineralisation at an average grade of 13g/t down to a depth of 108m via largely Soviet methods. The Kalana mine was restarted by Avnel (a former client of Edison) as an underground mine, although this was largely to comply with permit commitments while it conducted exploration with a view to a more modern exploitation. In the 12 years from 2004 to 2015 the mine produced 170koz of gold (average 14koz pa) from 531kt of ore at an average grade of 11.5g/t and 86% metallurgical recovery.
The Kalana project is located close to the western edge of the large Bagoe basin, which is a component of the Man-Leo shield of the West African Craton (see Tabakoto, above) and is a Paleoproterozoic orogenic gold deposit associated with a diorite intrusion within sedimentary rocks of the lower part of the Upper Birimian group. Mineralisation is hosted in narrow, shallow-dipping quartz and associated inter-vein mineralisation, which together define the vein packages. The predominant strike and direction of the quartz vein packages varies across the deposit, but has a relatively consistent orientation locally.
The mine plan for Kalana provides for a single open pit to be developed in 12 stages via conventional open pit techniques, using a maximum of 31 90t haul trucks and two excavators to support an average mining rate of 12Mtpa and a peak mining rate of 18.7Mtpa to support an average processing rate of 1.26Mtpa and a peak processing rate of 1.5Mtpa. Mining is categorised into bulk and selective areas, where drilling and blasting is needed on 10m and 5m benches, respectively. Stages 1–11 of the mine plan contain c 60% of the reserve ore tonnes and 65% of the reserve gold ounces, but only 54% of the waste tonnes. Moreover, approximately 50% of stages 1–11 are in the softer, saprolite material, which is mainly free digging. For the first three years of production, operations are focused almost exclusively on stages 1–6 in the higher grade, saprolite material, which requires minimal drilling and blasting.
The Kalana Main process plant design is based on a gravity/CIL flowsheet with a nominal 1.2Mtpa capacity when treating competent, fresh ore and 1.5Mtpa capacity when treating softer, saprolite ore. Gold is to be recovered by a combination of gravity concentration/intensive leaching and by a cyanide CIL process for the treatment of gravity tailings. Given the pronounced effect of coarse gold encountered in testing and the high gravity gold recovery achieved historically, the gravity circuit has been designed to treat the full ball mill discharge.
The TSF at Kalana will be operated as a self-raised dry wall facility with deposition starting behind a starter embankment. The average rate of rise over the life of the facility will be 2.2m per year and the basin will be lined with a 1.5mm high density polyethylene geomembrane laid on reworked soils.
The Kalana mine has existing, limited grid electrical supply from the local utility, Energie du Mali, which will be used initially during construction and latterly to provide power to the mining infrastructure and mine accommodation. Power for the plant will be provided by a combination of heavy fuel oil and diesel-fuelled generators.
Water will be sourced from return water from the TSF, water pumped from the Kalana open pit and surrounding de-watering. As the water balance of the operation is positive, there is no requirement for additional water extraction and, in fact, it is possible that excess water may need to be discharged into the environment; a water treatment plant has therefore been designed to accommodate this contingency.
Development and strategic optimisation potential
The present feasibility study, prepared by Avnel, anticipates producing an average of 101koz per year at an AISC of $730/oz over an 18-year mine life. Endeavour expects to take advantage of its project execution expertise, operating synergies and exploration experience to re-design and optimise the current feasibility study by the end of FY18. With an expanded plant capacity (eg similar to the Ity CIL project – see Exhibit 5), Endeavour believes that Kalana has the potential to increase its annual production profile to more than 150koz pa. Construction is expected to begin in mid-2019 following the completion of the Ity CIL project.
Following its acquisition of Avnel in 2017, Endeavour is working to integrate Kalana into its five-year exploration strategy (see Exhibit 7). In the meantime, the Kalana permit, covering 387km², has significant exploration potential and hosts a number of exploration prospects. Two of the most advanced of these are Kalanako and Djirila, which have both been drill-tested and are within a reasonable trucking distance of the anticipated Kalana plant site. However, management also believes there is a possibility the main deposit may be replicated in parallel structures.
A $5m exploration programme is planned for 2018, with the objective of completing 45,000m of drilling to provide an updated resource which is expected to form the basis for the updated feasibility study. Exploration is focused on in-fill and extension drilling at Kalana, as well as further drilling on the previously discovered Kalanako deposit. Additional exploration is also expected to take place on the recently acquired Fougadian licence and on permits that are expected to be granted shortly.
Tabakoto (80–90% interest, sale announced)
Tabakoto is located in western Mali, approximately 360km west of the capital, Bamako and less than 20km from the border with Senegal. It is accessed via a national highway (RN13) to the government administrative centre of Kenieba and, from there, 15km to the north on all-weather, graded dirt roads. It is also approximately 26km southeast of Randgold Resources’ Loulo mine.
Following Endeavour’s acquisition of Avion in 2012, the Segala open pit mine was converted into an underground mine, the Kofi C open pit mine was commissioned in Q115 and, in 2013, the mill’s capacity was expanded from 2,000 to 4,000tpd. Nevertheless, after a strategic assessment in Q218, management launched a sales process for Tabakoto and, on 4 September, the company announced that the mine had been sold to Algom Resources (a subsidiary of BCM Investments) for a total cash consideration of US$60.0m payable on closure of the transaction (anticipated in Q418). Relative to the US$73.2m of assets held for sale on Endeavour’s balance sheet as at end-Q218, US$60.0m in consideration implies that EDV will book an exceptional (non-cash) loss in the order of US$13.2m on conclusion of the sale in Q418 (see Exhibits 12 and 23). However, Endeavour will continue to retain ownership of the high potential greenfield Kofi exploration land package north of the Tabakoto mine, along trend with Randgold's Loulo mine.
Alluvial gold has been exploited in the Tabakoto area since at least the 1940s. Western Mali became the focus of exploration programmes in the 1960s and, in the 1980s, the United Nations Development Programme completed airborne geophysical and geochemical surveys that identified anomalies at Tabakoto, Segala and Kofi Nord. Thereafter, numerous western companies undertook exploration programmes in the area. Nevsun was the first to complete a feasibility study on the Tabakoto and Segala deposits in 2002. After an abortive attempt to enter production however, the project was sold to Avion in 2008, which also acquired the Kofi property in 2010.
Endeavour’s involvement in Tabakoto, Segala and Kofi Nord began in 2013, when it acquired Avion. Subsequent exploration largely focused on in-fill programmes, including 16 diamond drill holes over 8,020m (an average 501m/hole) and 406 RC holes over 34,969m (average 86m/hole) on the Segala exploitation permit and 41 diamond drill holes over 5,556m (average 136m/hole) and 860 RC drill holes over 53,412m (average 62m/hole) on the Kofi Nord exploitation permit.
Malian geology is dominated by the West African Craton and smaller portions of eastern Mali are part of the Tuareg Shield. Regional gold exploration has focused on the southern Leo-Man-Ghana micro-craton (referred to as the Man shield), which contains the Kenema-Man domain Archean core and the Baoule-Mossi Proterozoic domain, the latter of which is associated with the gold prolific Birimian sedimentary sequences, which account for the majority of West African gold deposits. Western Mali is underlain by the Paleoproterozoic Kedougou-Kenieba inlier (an area of older rocks surrounded by younger rocks, typically formed by the erosion of the younger overlying rocks to reveal a limited exposure of the older underlying rocks), which is effectively a window of the Man shield and is the westernmost exposure of the West African Craton. However, extensive weathering has produced large areas of laterite over the region, which masks the underlying geology of these areas and renders outcrops rare and difficult to characterise.
The Tabakoto and Kofi properties are located in the eastern part of the Kedougou-Kenieba inlier. The Birimian rocks of the inlier have been subdivided into four formations: the western Mako Series (granite-greenstone belt), the Diale-Dalema Series (metasedimentary rocks), the Faleme Series (carbonate rich sedimentary rocks) and the eastern Kofi Series (detrital sedimentary rocks). The Senegal-Mail shear zone is a major, regional-scale, north-south shear zone and marks the boundary between the Diale-Dalema and Feleme Series to the west and the Kofi Series to the east. The major gold deposits of the Kedougou-Kenieba inlier are located along second, or higher, order shears associated with this structure. The Tabakoto and Kofi deposits themselves occur east of the Senegal-Mali shear zone in the eastern part of the Kedougou-Kenieba inlier and are underlain by rocks of the Kofi Series (Birimian, turbiditic sedimentary rocks). The entire package of rocks has then been deformed and metamorphosed during the Eburnean orogeny (mountain building process). While individual structures associated with each of the deformational events can host mineable deposits, multiple generations of structure enhances the probability of mineable ore.
Mineralisation at Tabakoto, Segala and Kofi is typically associated with disseminated to massive sulphides, pyrite, pyrrhotite, arsenopyrite and, occasionally, chalcopyrite and sphalerite. The gold is associated with either quartz veining or moderate to intense silicification and/or albitisation. The deposits may be characterised into three main types:
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shear zone hosted (Segala and Segala NW)
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fracture and cross structure hosted (Dar Salam, Tabakoto, Dioulafoundou and Kofi C)
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intrusive hosted (Djambaye II)
Tabakoto mining operations consist of two underground operations (Tabakoto and Segala) and one open pit (Kofi C) with gravity/CIL processing facilities. The Tabakoto underground deposits are accessed from two portals at the bottom of the Tabakoto pit. The northern portal is used to exploit the northwest trending zones in the northern half of the mine and the southern portal for both the northeast trending zones and the southern zones in the southern half of the mine. The Segala Main Zone (the largest single deposit on the property) is accessed by a portal from the side of the Segala open pit. This zone consists of several parallel structures that run along the length of the ore body. The spacing and the thickness of these structures vary. Individual veins, which may be less than 1m thick, are grouped into ore zones that can collectively be up to 35m thick. In total, there are five veins being exploited by underground mining methods, each of which uses a variation of long-hole stoping, variously with or without backfill, which may be consolidated. The mining of the Kofi C deposit, which is ostensibly to augment underground feed, is by means of conventional drill and blast and load and haul open pit mining methods.
Following an expansion in 2013, the Tabakoto plant has been designed to recover gold from a variably weathered orebody at a design capacity treatment rate of 4,000tpd. The average feed grade for Tabakoto over the life of the mine is expected to be 3.6g/t (cf a resource grade of 3.13g/t and a reserve grade of 3.35g/t) and the process design criteria consist of crushing, ore stockpiling, milling, classification and in-line leach reacting, CIL, tailings disposal, acid wash, elution, electro-winning and smelting. Sodium cyanide consumption is c 0.6kg/t and lime consumption is a fairly modest c 2.0kg/t.
Owing to a lack of immediate grid power, Tabakoto owns and operates a power station equipped with 19 diesel-driven Cummins alternators with a total nominal capacity of 22.4MW.
Given its relatively short mine life, Tabakoto had hitherto been an exploration priority at Endeavour after Houndé and Ity, with a programme focusing on both surface exploration and underground drilling, with the aim of delineating resources within trucking distance of the plant.
In 2017, Endeavour dedicated $8m to Tabakoto’s exploration programme, totalling 56,200m of drilling. The campaign was focused on both underground resource delineation and testing near-mill open-pit targets. Depleted ounces were replaced and a portion of the new measured and indicated resource was converted into reserves.
As Endeavour will retain ownership of the high potential greenfield Kofi exploration land package near the Tabakoto mine, Endeavour is investing an additional US$6m in the 2018 exploration programme, totalling approximately 45,000m of drilling. This will be allocated equally between near-mill targets (both underground and open pit) and greenfield targets on both the Kofi permit and on the new permits acquired in 2017, located immediately north of Kofi and on-trend with Randgold’s Loulo deposits.