Ann: Discovery of a large porphyry-style system at Bottletree, page-256

Ive Gone over the reports.

WE WANT BIOTITES.

There strong at the end of BTDD003 from 550m to 725m.

BTDD005. Some around 100 to 150m.Most 500m to 800m

BTDD010. Some 150m to 250m and 680m to 700m.Most 900m to 1000m.

We have a Steep west dipping Mineralisation with most Biotite inthe most west hole and at depth and getting
deeper the more west.

There is a broad trend of increased temperature of the hydrothermal alteration indicated by the presence of secondary
biotite movingfrom east to west and to deeper levels.

The broad zonation ismirrored by a trend from some deep epithermal vein mineralisation
(quartz-pyrite-chalcopyrite-pyrrhotite veins) in the east, to potassic biotite-chalcopyrite mineral to the west increasing at depth.

INTESTING SINGULAR VEIN

One solitaryporphyry-style quartz-molybdenite vein with a prograde epidote selvage cuts thefoliation and is cut by it, and
so represents syn-deformationalporphyry-related prograde Mo mineralisation recognised only in the top of DDHBTDD010
at the extreme west of the EW section

May be indicative of a target in that vicinity.

This is around 140m true depth.So Shallow.

Dr Corbett states indicative of Target in area, but that area at present has no target.

In Superiors report

Porphyry Target E isabout 100 metres west of the BTDD010 collar and is defined by a potentiallylarge and high order copper
soil anomaly that despite being covered by soil,persists for up to 500 metres westwards under the soil cover. In addition, the
soil copper anomaly is coincident with a distinct aerial magnetic feature.

Ive mentioned many times about the Alluvial gravels in thewest and there importance in the sense they are a secondary
Deposit.
Prior to the Discovery of the singular vein at 140m true depth in hole 10.

Possible causes could have been a water event that shifted the top cover from east to west as the east is barren for Cu enriched
soils.

But with the inclusion of the vein and now the alluvials having a magnetic feature, I hope there enrichment is from a primary
source under them.

That Vein in hole 10 willconnect to something, they always do.

THE GOSSAN ENVELOPE.

This is a big bonus. Gossans are oxidized and often the top of ore deposits.

The Gossan goes south for many hundreds of metres and seems to end where Superior has marked a second wall rock zone.

It looks like they are on the NE edge of the system.

This round of drilling did not give us a Porphyry,but atleast we know we do not go East or North greatly,but West,
South West and south.

I think they are close to the core as biotites are pretty strong in hole 10, very little biotites in the east.