Ann: Broad High-grade Lithium Intersections extend BP33, page-15

Am i correct in thinking we may have come across a whole new system?
Sounds really encouraging to say the least

The southern BP33 pegmatite dips steeply to the east and strikes in a north south
direction. This is a different trend compared to the main BP33 pegmatite (Figure 3)
and it is uncertain at this stage how the two bodies are related. Although
spodumene has been identified, the southern pegmatite is not as strongly
mineralised as the main body. The true thickness of the body varies between 4 to
10m but does appear to be increasing in thickness with depth