Ann: Wide Zone of Mineralisation Intersected at Durnings, page-11

CSA was mined for its lead and zinc originally before being well known for its copper production. The regolith expression of the CSA area only showed traces of copper with the only the pyrite Pb-Zn lode, and the western Cu ore body, the only lodes exposed at surface. Why Cobar -type deposits are hard to find generally.

So common in Cobar-type deposits to see 1) multiple lodes 2) polymetallic mineralization associated with different lodes 3) trace elements of mineralization nearby the main ore sources (i.e Cu). and 4) high grades in the orebodies.

Pointing out again that CSA has many sub-parallel ore lenses that strike for 120m and range up to 20m thick. Bwteen drill holes MYRC0003 and MYRC0002 we are talking over 1km so the potential for multiple lenses (and deposits) is pretty - considering too the other targets. The trace elements of Cu are what you would expect to see in the Pb-Zn lodes of CSA before they enter the main Cu body.

CSA.des (minedocs.com)