Dios discovered gold dispersal trains leading up-ice to date to outcropping gold-bearing granites near major structures.
Dios explores for high potential intrusives associated with deep structures. Glacial sediment sampling defines indicator mineral dispersal trains for diamond indicator minerals for kimberlites.
Kimberlites are deep-rooted intrusives, alkaline magmatism facies, often associated with rift zones. Kimberlites (diamond potential) rise up as volcanoes coming from the earth’s mantle, some 400 kilometers at depth.