The composition of magmatic Ni-Cu-(PGE) sulfide deposits in the Tati and Selebi-Phikwe belts of eastern Botswana
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Unfortunately, the tick marks of the picrite-crust mixing lines in Fig. 5 have been plotted erroneously. As a result, the correct value of crustal component is < ca. 5% at Tati (not <10–20% as stated in the text) and > ca 5% at Phikwe-Dikoloti (as opposed to >10–20%).
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