Copperton - Areachap Cu-Zn mineralization

Stratiform massive sulfide deposit at the Prieska Cu-Zn and Areachap mines are situated close to the eastern margin of the Namaqua Province, South Africa, within the Copperton and Jannelsepan Formations. The investigation of the petrology and geochemistry of the Prieska Cu-Zn deposits forms the basis of this study. Borehole core and surface samples were investigated petrographically. Knowledge gained during this investigation was used to select suitable samples for geochemical analysis. Suites of samples were analysed for their major element and some trace element concentrations by wavelength-dispersive X-ray fluorescence spectrometry. Concentrations of some elements in the lanthanide group were determined using the inductively coupled plasma emission spectrometer. Samples were also submitted for analysis by instrumental neutron activation analysis. Determinations of concentrations of U and Pb and isotopic compositions of Pb were done for both whole rock samples and sulfide mineral separates. Major and trace element abundances within different rock types of the Copperton Formation are discussed and compared with those of the Jannelsepan and Hartebeest Pan Formations. The petrogenetic implications of these, the U-Pb isotope systematics and S isotope ratios are used to reconstruct the geological environment of mineralization. 187 refs., 106 figs., 68 tabs