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Botswana

Mupane Mine

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Overview

Mine TypeOpen Pit & Underground
StatusActive
Commodities
  • Gold
Mining Method
  • Truck & Shovel / Loader
  • Blasthole slot
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SnapshotOn May 03, 2022, the Mupane mine was acquired by Hawks Mining Company Proprietary Limited (“Hawks Mining”), a company registered under the laws of Botswana and owned by certain individuals forming part of the Galane Gold’s local Botswana management team. The new Owner does not publish production data.

Owners

SourceSource
CompanyInterestOwnership
Hawks Mining Company Proprietary Limited 100 % Indirect
On May 03, 2022, Galane Gold Ltd. completed the sale of its Mupane gold mine in Botswana (the “Mupane Property”) to Hawks Mining Company Proprietary Limited (“Hawks Mining”), a company registered under the laws of Botswana.

Deposit type

  • Orogenic

Summary:

The Mupane deposits are located in an area known as the Mupanipani Hills, ridges formed by outcrops of banded siliceous and graphitic iron formation (GIF). These units of so-called „iron formation? are hosted by a sequence of metasediments, including coarse grained carbonate bearing conglomerates, para amphibolites, marbles, metapelites and minor orthoamphibolites. The host rocks are all variably schistose depending on the abundance of micaceous components (Tomkinson and Putland 2006).

The geology of the properties and the style of the gold mineralisation varies between the various deposits.

The Tati Greenstone Belt (TGB) hosts numerous small scale nickel and gold deposits.

The nickel deposits consist almost entirely of disseminated to semi massive sulphide bodies hosted by a series of late stage troctolitic intrusive bodies on the northeastern edge of the greenstone belt.

The belt has been extensively prospected in the past due to the abundance of numerous small scale narrow quartz vein hosted gold deposits. These deposits are all clearly related to late stage, high level brittle shear zones developed within the volcanics and sediments of the belt.

The deposits were generally refractory in the fresh sulphides and contained significant amounts of arsenopyrite and some stibnite although the gold is principally hosted within pyrite and to a lesser extent pyrrhotite (i.e. Map-Nora Lodes). The alteration associated with the mineralisation varies depending on the host rocks but typically consists of biotite, muscovite, chlorite, carbonate and ubiquitous quartz either as veins or silicification. Very few of these deposits appear to have developed significant magnitude to be worthwhile propositions for modern gold mining.

In style the gold mineralisation conforms to the Archaean Lode Gold or Orogenic Gold style of mineralisation. They all appear to have formed late in the history of the belt and closely resemble mineralisation seen in the Archaean greenstone belts of Canada, South America and Australia.

Mineralisation is a “disseminated-style" in well-bedded, silicified quartz-rich parts of the graphitic iron formation (GIF) at Tau and Tholo and partly silicified graphitic schists at Kwena. This style of mineralisation is unlike that of most Achaean gold deposits being a broad siliceous zone. Mineralisation is not dominated by discrete veins and the deposit lacks sharply-bounded loads. The mineralized parts are however distinctive due to the silicification of the GIF.

The ore zone at Tau lies within the GIF unit. In comparison to unmineralized GIF, mineralized GIF is substantially altered. The addition of silica, remobilized silica, carbonate, wallrock fragmentation and the addition of vein quartz and sulphides have in large part overprinted the original features of the GIF. Mineralized GIF is highly siliceous and carbonated, highly deformed with the graphitic units strongly sheared. Deformation is ductile, with a very minor brittle component, mostly fracturing, and specifically fracturing of arsenopyrite. Minor vein quartz are brecciated, sheared and incorporate much of the GIF wallrock. Arsenopyrite is the most visual sulphide phase, and gold mineralisation is sulphidation of wallrock by this phase.

Reserves

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Mining Methods

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Comminution

Crushers and Mills

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Processing

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Production

CommodityUnits2021202020192018201720162015
Gold oz  ....  Subscribe  ....  Subscribe30,29435,52729,35426,78324,321

Operational metrics

Metrics2021202020192018201720162015
Tonnes milled  ....  Subscribe  ....  Subscribe732,789 t831,158 t740 kt908 kt810 kt

Production Costs

CommodityUnits20212020201920182017
Cash costs Gold USD  ....  Subscribe  ....  Subscribe 1,090 / oz   928 / oz   933 / oz  

Financials

Units20212020201920182017
Revenue M USD  ....  Subscribe  ....  Subscribe 41.4   44.6   37.3  
Operating Income M USD  ....  Subscribe  ....  Subscribe 0.8   3   1.7  

Heavy Mobile Equipment

Fleet data has not been reported.

Personnel

Mine Management

Job TitleNameProfileRef. Date
....................... Subscription required ....................... Subscription required Subscription required Oct 4, 2023
....................... Subscription required ....................... Subscription required Subscription required Oct 4, 2023
....................... Subscription required ....................... Subscription required Subscription required Oct 4, 2023

EmployeesYear
...... Subscription required 2021
...... Subscription required 2020
...... Subscription required 2019

Aerial view:

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