Such sediment-hosted stratified copper-silver ores are indeed interesting.
This ore dips at an angle of 10-30 degrees into the rock and undulates somewhat like a sheet within the rock. Some edges of the sheet have been exposed, and in one spot, this Dingelvik MRE has been done.
Here, the “sheet,” or the ore sediment layer, is more visible. In some places, it has been exposed elsewhere than just the edges. There is very little data. The great thing about this is that as this geology has started to become clearer and, for example, geophysics measurements are being carried out, these guys can drill almost anywhere at a steep angle and penetrate more of this sheet. This ore could be really big.
The infrastructure is in good condition, with a railway line and power lines running nearby. If it happens, it will be an underground mine, which is a good thing, as huge open-pit mines would hardly be wanted in Southern Sweden. The ore is not very rich compared to the best similar ores of all time, but the Swedes know how to utilize their very large, not-so-super-rich ores well.