Lead isotopes of the carbonate-hosted Kabwe, Tsumeb, and Kipushi Pb-Zn-Cu sulphide deposits in relation to Pan African orogenesis in the Damaran-Lufilian Fold Belt of Central Africa

Lead isotope ratios of galena from the carbonate-hosted massive sulphide de posits of Kabwe (Pb-Zn) and Tsumeb (Pb-Zn-Cu) in Zambia and Namibia, respec tively, have been measured and found to be homogeneous and characteristic o f upper crustal source rocks. Kabwe galena has average isotope ratios of Pb -206/204 = 17.997 +/- 0.007,Pb-207/204 = 15.713 +/- 0.010 and Pb-208/204 = 38.410 +/- 0.033, Tsumeb galena has slightly higher Pb-206/204 (18.112 +/- 0.035) and slightly lower Pb-207/204 (15.674 +/- 0.016) and Pb-208/204 (38. 276 +/- 0.073) ratios than Kabwe galena. The isotopic differences are attri buted to local differences in the age and composition of the respective sou rce rocks for Kabwe and Tsumeb. The homogeneity of the ore lead in the two epigenetic deposits suggests lead sources of uniform isotopic composition o r, alternatively, thorough mixing of lead derived from sources with relativ ely similar isotopic compositions. Both deposits have relatively high U-238 /Pb-204 ratios of 10.31 and 10.09 for Kabwe and Tsumeb galenas, respectivel y. These isotope ratios are considered to be typical of the upper continent al crust in the Damaran-Lufilian orogenic belt, as also indicated by baseme nt rocks and Cu-Co sulphides in stratiform Katangan metasediments which hav e a mean mu-value of 10.25 +/- 0.12 in the Copperbelt region of Zambia and the Democratic Republic of Congo (formerly Zaire). The Th-232/Pb-204 isotop e ratios of 43.08 and 40.42 for Kabwe and Tsumeb suggest Th-enriched source regions with Th-232/U-235 (kappa-values) Of 4.18 and 4.01, respectively. M odel isotopic ages determined for the Kabwe (680 Ma) and Tsumeb (530 Ma) de posits indicate that the timing of the mineralisation was probably related to phases of orogenic activity associated with the Pan-African Lufilian and Damaran orogenies, respectively. Galena from the carbonate-hosted Kipushi Cu-Pb-Zn massive sulphide deposit in the Congo also has homogeneous lead is otope ratios, but its isotopic composition is comparable to that of the ave rage global lead evolution curve for conformable massive sulphide deposits. The mu (9.84) and kappa (3.69) values indicate a significant mantle compon ent, and the isotopic age of the Kipushi deposit (456 Ma) suggests that the emplacement of the mineralisation was related to a post-tectonic phase of igneous activity in the Lufilian belt. The isotope ratios (Pb-206/204, Pb-2 07/204, Pb-208/204) Of th, three deposits are markedly different from the h eterogeneous lead ratios of the Katangan Cu-Co stratiform mineralisation of the Copperbelt as well as those of the volcanogenic Nampundwe massive pyri te deposit in the Zambezi bell which typically define radiogenic linear tre nds on lead-lead plots. The host-rock dolomite of the Kabwe deposit also ha s homogeneous lead isotope ratios identical to the ore galena. This observa tion indicates contamination of the Kabwe Dolomite Formation with ore lead during mineralisation.