摘要:The juvenile 1.89 Ga oceanic arc vol- canic rocks of the Paleoproterozoic Flin Flon volcanic belt are host to sev- eral world-class volcanogenic massive sulphide (VMS) deposits, including the recently discovered Au-rich Lalor Lake VMS deposit at Snow Lake (Fig. 1). This trip uses spectacular roadside out- crops (Figs. 2-5) to highlight current understanding of the nature and set- ting of the regionally metamorphosed VMS mineralization and alteration at the eastern end of the belt at Snow Lake.