Mineral paragenesis and sulphide trace element distribution in the metamorphosed Lovisa Zn-Pb deposit, Bergslagen (Sweden), as revealed by 3D X-ray tomography, ore petrography and LA-ICP-MS analysis

•The ore textures reflect overprint by polyphase deformation and metamorphism.•Main stage of ore modification during D2 at c. 1.83–1.80 Ga.•Coarse-grained sulphide veins and fracture fillings formed due to remobilisation.•Trace element-mineral chemistry reveals limited redistribution of metals during sulphide remobilisation.•Potential relationship with nearby Cu-Co mineralisation is suggested.