Magnetite trace element compositions from two VMS deposits, their host rocks, and local glacial sediments are documented.
The geochemical censored data are investigated using the R-package robCompositions.
The data were opened using centered-log ratio transformation, and then analyzed using principal component analysis.
Magnetite grains from different VMS deposits and bedrock lithologies have distinct chemical signatures.
The chemistry of magnetite in till is useful in VMS deposit exploration in both deposit areas.