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Gold exploration in the Bjornesund region has been carried out since the early 1990s, and gold was found in the central part of the Bjornesund East area by NunaOil and the Geological Survey of Denmark and Greenland (GEUS). Records of stream sediment samples with elevated gold concentrations up to several hundred parts per billion led to the recognition that amphibolites in the central part of the Bjornesund East could be a promising target and work in 1996 led to the discovery of hydrothermally altered amphibolites with up to several hundred ppb gold. However, exploration work was limited to grassroots prospecting and none of the targets were drilled. The aim of new field work was to target areas in the Bjornesund supracrustal belt which mainly consists of amphibolites but also comprises significant proportions of diorite, anorthosite, leucogabbro, granitoid rocks and ultramafic to mafic rocks that occur as relatively thin slivers in the amphibolite. We tested if the targeted areas were favourable for gold mineralisation and investigated the relationship between the mineral potential mapping and the actual geology. Here we demonstrate that based on older data we located new gold mineralising systems in the western part of the Bjornesund supracrustal belt, identified platinum-enriched mafic to ultramafic rocks and located new occurrences of corundum at amphibolite-anorthosite contacts (Schlatter

Combining exploration and multivariate techniques to detect the Bjørnesund West gold occurrence, southern West Greenland