Defining IOCG signatures through compositional data analysis: A case study of lithogeochemical zoning from the Olympic Dam deposit, South Australia 机翻标题: 暂无翻译,请尝试点击翻译按钮。

Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration
2019 / 105 /
Univ Adelaide, Sch Chem Engn, Adelaide, SA 5005, Australia;BHP Olymp Dam, Adelaide, SA 5001, Australia;Univ Adelaide, Sch Chem Engn, Adelaide, SA 5005, Australia;Univ Adelaide, Sch Chem Engn, Adelaide, SA 5005, Australia;Univ Adelaide, Sch Chem Engn, Adelaide, SA 5005, Australia;Univ Adelaide, Sch Math Sci, Adelaide, SA 5005, Australia;
Dmitrijeva, Marija;Ehrig, Kathy J.;Ciobanu, Cristiana L.;Cook, Nigel J.;Verdugo-Ihl, Max R.;Metcalfe, Andrew V.;
The Olympic Dam Cu-U-Au-Ag deposit is dominantly composed of mineralised hematite-breccias and occurs entirely within the Roxby Downs Granite. Multivariate statistical analysis of a large whole-rock, 15 m-interval geochemical dataset (10,565 samples) was undertaken to identify geochemical signatures characteristic of iron-oxide copper gold (IOCG)-style mineralization and constrain the conspicuous lithogeochemical zonation observed at Olympic Dam. Statistical analyses include principal component analysis on centred logratio (clr)-transformed data coupled with hierarchical clustering. Certain groups of elements that can be interpreted in terms of an evolving hydrothermal system relative to host lithologies are derived from data analysis: granitophile (U-W-Sn-Mo); siderophile (Ni-Co); chalcophile (Ag-Bi) and related elements (As-Sb and Au-Te). The distributions of elements within each group are investigated through three vertical cross-sections and are compared with known lithological and Cu-(Fe)-sulphide zonation. Throughout the Olympic Dam Breccia Complex, the IOCG signature is defined by multi-element combinations of the commodity metals Cu, U, Au, and Ag, coupled with a range of trace elements. Overall, the IOCG signature overlaps well with Fe-metasomatism despite mismatch which is likely due to discrete styles of mineralisation found only on the margins of the deposit and also to the presence of mineralised domains within Fe-poor zones. The IOCG signature is composed of two geochemical associations, which exhibit distinct spatial distributions. The first group, Cu-U3O8-Se-S, shows concentric zonation whereas the second group, Au-W-Mo-Sb-As, forms a vertical similar to 1800 m deep corridor in the southeastern lobe of the deposit. The specific Au-W-Mo-As-Sb signature could potentially be generic within IOCG systems across the Olympic Cu-Au province and if so, would provide a proxy model for near-mine exploration.
Principal component analysis;Hierarchical clustering;Whole-rock dataset;IOCG deposits;Lithogeochemical zoning;Olympic Dam;