Ann: Exploration Update - Drilling to Resume this Month, page-85

Can any of our geo,s explain this please in the absences of regolith development explained a weak geochemical signiture. Could I be right in thinking this could be applied to Beauwolf with the failed soil sampling. I also found this interesting Now for a brief rundown of the geology as illustrated on this map and box model.
The local country rocks are sedimentary and dip 70 DEGREES ( sound familiar) to the SW.
The hanging wall rocks are composed of conglomerates and sandstones of the Merougils
Creek Beds, which from our drilling to date are barren and have little prospectivity.
Mineralisation is hosted within a unit called the black flags mudstone which varies in
thickness from 15-100m. Shears form along its contacts which are collectively known as
the Speedway Shear.
Gold is contained in steep lodes characterised by Quartz, Albite and Pyrite and is very
distinctive and easy to recognise against the unmineralised portions of the mudstone
host.
Lode thickness varies from less than 1m to over 20 metres in the thicker portions of the
orebody and has been defined for nearly 2km in strike length.
The footwall rocks range from sandstones, conglomerates and andesites and are also
part of the Black Flags group. There are some thin but very high grade flat lying
extensional veins in the footwall that occur intermittently along the strike length of the
10 orebody. The focus to date has been on the main lode system and these veins have not
been adequately drilled and represent significant upside potential.
The entire package has been intruded by barren mafic dykes and is overlain by a thin
layer of unconsolidated lake sediments, which range from a few metres in the north to
~30m in the south. Does this sound similar to Slate Dam.? or am I way off geology was not my strong point at school (maybe if I had listened it could have been) lol will be more than happy to be told I'm wrong