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Location: 16 km SE from Letlhakane, Botswana
Private Bag 001JwanengBotswana
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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.
Debswana is a joint venture between the government of Botswana and the South African diamond company De Beers; each party owns 50% of the company.
The kimberlite pipes located within mining licences form part of the Cretaceous-aged (144–65 Ma) Orapa Kimberlite Cluster. These kimberlites were emplaced through the complete sequence of local equivalents of the Karoo Supergroup rocks, which overlie rocks of the early Proterozoic Magondi Mobile Belt. The latter were thrust over the western edge of the Kaapvaal Craton, based on xenolith studies from Orapa and Letlhakane. The cratonic rocks in this area are composed of Archaean tonalitic gneiss. The Stormberg basalt at the top of the Karoo Supergroup is overlain by a thin cover of the Kalahari sands.The larger kimberlite bodies are typically steep-sided, carrot-shaped diatremes, but there are many examples of magmatic kimberlite plugs and small intrusions that terminate at the base of the basalt, or which were emplaced through the basalt as small dykes. The kimberlite bodies consist of several texturally distinct phases of kimberlite, varying from volcaniclastic to pyroclastic to hypabyssal kimberlite. The kimberlites at Orapa, Letlhakane and Damtshaa are all monogenetic (multi-vent) volcanoes.The Letlhakane mine consists of two kimberlite pipes and is one of a cluster of three kimberlite mines in central Botswana. Core logging and additional petrographic study classifies this deposit as a Group I, opaque-mineral and perovskite-rich altered probable monticellite kimberlite. Most of the kimberlite examined is massive volcaniclastic kimberlite, whilst rare layered volcaniclastic and magmatic kimberlite is also present.Spinels are a ubiquitous component of kimberlites and their compositions are frequently used as petrogenetic indicators. The compositions of Letlhakane groundmass spinels will be used to fingerprint kimberlite facies by identifying the presence of several discrete batches of magma with unique evolution trends. The spinels are excellent indicators of these trends and are apparently immune to the affects of hydrothermal and subsequent alteration. Analysis has revealed that the Letlhakane spinel are unusually titanium-rich (TiO2 from 4.93 to 17.91 wt%), which correlates with other titanium-rich textural indicators such as the presence of prograde overgrowths of sphene around atolled-textured spinels and an unusually high proportion of perovskite to spinel of around 10:1, which is the inverse of a typical kimberlite.Tailings Mineral Resource is coarse processed kimberlite discarded from the ore processing plant. Old Recovery Tailings are heavy minerals discarded from the recovery section of the ore processing plant.
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