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Location: 8 km E from Kahama, Tanzania
Tan House Tower, Plot Number 34/1 Ursino South, New Bagamoyo Road Post Office Box 1081Dar Es SalaamTanzania
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Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
Shaft depth, mining scale, backfill type and mill throughput data.Full profiles of select mines and projects.
Equipment type, model, size and quantity.Full profiles of select mines and projects.
Camp size, mine location and contacts.Full profiles of select mines and projects.
On January 24, 2020, Barrick announced that the Company had ratified the creation of Twiga Minerals Corporation, the operating company formed to manage the Tanzania mines. Effective January 1, 2020, the GoT received a free carried shareholding of 16% in each of Barrick’s Tanzanian mines (Bulyanhulu, Buzwagi and North Mara).
Buzwagi is shear-hosted quartz-veined deposit hosted in porphyritic granite. It is found in Nzega belt in the lower portion of the Nyanzian system. This belt is composed of basalt and intermediate volcanic intruded by granitoid masses which is dominated by deep-seated structure.The granite that hosts the majority (85%) of the Buzwagi deposit is a medium to coarse feldspar granite with zone orthoclase crystals up to 4cm. This is predominantly underlain by medium- to coarse-grained granite intruding mafic flow and pillow flow basalts, within which there are two other distinctive units, including a tonalite silt-like body, which is occasionally mineralised with quartz veining, sericite alteration and sulphide mineralisation. Rock units dip to the east at c 60° in the southern portion of the lease area and 65-75° in the northern portion.Several faults traverse the Buzwagi area. The most significant orientation of faulting is northwestsouth-east, parallel or sub-parallel to the Nzega shear (and probably related to it).The Buzwagi deposit is hosted within or near a north-south brittle-fracture shear corridor that is up to 450m wide and includes two ore types: shear-hosted, porphyry-hosted.As such, Buzwagi has been separated into 12 structural domains, within which mineralisation is segregated.Domain 1 (which accounts for up to 50% of Buzwagi’s in-situ gold) is up to 1,000m long and 30m wide (subject to pinching and swelling), with a consistent gold grade (averaging 2.69g/t) along its entire strike length. The gold mineralisation in this domain is associated with quartz veins and/or quartz stockwork, reflecting dilatant zones within the north-south structural corridor. By contrast, mineralisation in Domain 6 extends over a wider area than Domain 1 (>30m) and is characterised by more stockwork and less shearing. All other mineralised domains are similar to Domain 6, except that they are generally less than 10m wide. The gold mineralisation in all domains plunges 30° to the south.
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