The Kaapvaal Craton of South Africa comprises an Archaean core of 3.5 Ga lithospheric and crustal rocks surrounded by younger accreted terrains of 3.0-2.7 and 2.1-1.9 Ga. The craton is covered by relatively undeformed 3.0-2.4 Ga supracrustal rocks, which show the effects of thermal and hydrothermal interaction. Part of this activity is manifested by a large number of epigenetic Pb-Zn (±Ag, Au, Cu, F) deposits in the cover rocks of the Kaapvaal Craton. These include small volcanic and breccia hosted deposits in mafic and felsic volcanic rocks of the 2.7 Ga Ventersdorp Supergroup and the Mississippi Valley-type (MVT) deposits in the carbonates of the Transvaal Supergroup.
MVT mineralization at the Pering (and other Zn-Pb deposits) is hosted in fracture-generated N-S breccia bodies in the Paleoproterozoic carbonate succession of the western Kaapvaal Craton. The fluids carrying the metals were focused in vertical bodies within the fracture zones (FZ), the metals and the sulphur being carried together and precipitated in organic-rich sectors of the basin. Two small Pb-Zn deposits within mafic rocks of the Ventersdorp Supergroup, stratigraphically below the basin-hosted MVTs on the southwestern part of the Kaapvaal Craton have secondary chlorite which is extremely Rb-rich, associated with the mineralization. This chlorite and the associated altered basaltic host rocks give a Rb-Sr date of 1.98 Ga, and the associated galena Pb isotope data plot on the same array as those of other Pb-Zn deposits, the radiogenic intercept giving a date of 2.0 Ga. We interpret these data to indicate a craton-wide epigenetic fluid-infiltration event, which exploited the Maquassie Quartz Porphyry (MQP) as the aquifer and metal source.
Sr isotopic results for the ore-zone gangue minerals show highly radiogenic 87 Sr/ 86 Sr ratios (>0.710) which support earlier models that the origin of radiogenic Sr isotopic composition in the calcite cements is the felsic tuffs (MQP) of the Ventersdorp Supergroup occurring at deeper levels within the basin. Relationships between d 18 O and d 13 C performed on carbonate cements within the aquifers are complex: the range in d 13 C for some of the cements represents a mixture from two sources and with a progression from heavy carbon in the host to somewhat lighter carbon in the cements. Similarly, the lighter d 18 O values have a narrow range indicative of rapid exchanges between hydrous fluid and rock.