ORE SYSTEMS CONSULTING - Sweden FIG.1

Figure 1. Geological section at 2500E, Kristineberg mine, Skellefte belt, northern Sweden (courtesy of Boliden Mineral). View is to the east. The units shown include primary rock types and zones defined by alteration and metamorphic assemblages. There are two main Zn-rich massive sulfide horizons, A and B, separated by 50 to 150 m. The host rocks are of Paleoproterozoic age.





Figure 1. Geological section at 2500E, Kristineberg mine, Skellefte belt, northern Sweden (courtesy of Boliden Mineral). View is to the east. The units shown include primary rock types and zones defined by alteration and metamorphic assemblages. There are two main Zn-rich massive sulfide horizons, A and B, separated by 50 to 150 m. The host rocks are of Paleoproterozoic age.

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