Go. Yes. And have a look at this.
That's a bass that comes from the upper mental as we can see from some of the cumulative jars that are in there. And this shows us that we're not only dealing with a sedimentary basin, but we're dealing with a volcano sedimentary basin. And these basels are fantastic source rocks for metals, for copper, for zinc, for silver, also for some gold.
And you can see all of these black round particles in there. They are partly resorbed as we say. That means molten pieces of upper mental rocks.
And that means this magma for these vessels has come from the upper mental. So these are olivines, rounded olivines. They cumulates of rounded olivines.
That's correct. What What would the background of copper be in these rocks? More or less.
Originally that would be around about 450 ppm. But from the analysis that you've made, you see that they are much much lower. That means they have lost some of their copper.
Yes. Yes. It's been stripped by the fluids.
Correct. Yeah. Very interesting.
Yeah.