Ann: Kaskara Drilling Intercepts Extensive Minera, page-8

re: Ann: Kaskara Drilling Intercepts Extensiv... lol sell.. yeah.. whos going to believe that rationale..

i doubt you would be selling if you held.. very unconvincing..

at a minimum you you would hold. after a report like that

and if you were unsure of things thus far, and you understood what the geology is indicating you would probably think about adding or buying.

there is nothing reported other than very clear and conclusive confirmation that there are huge signs of extensive sulfide mineralisation below.


mljet.. your response as a non holder regarding this report is to sell, so where is it indicating in the report that what was always indicated has suddenly vanished? and how can you conclude that the assays confirmation of all that was reported previously regarding the kaskara prospect is indicating anything other than what has always been said about kaskara?






kaskara

Mineralisation is clustered in oxidised zones that are up to 30 m thick. Within these broad zones, irregular bodies of copper-lead-zinc mineralised hematitic material are up to several metres thick, and are surrounded by networks of hematitic veins. The hematitic material is variably mineralised by mottramite (Figure 4) and descloizite, and to a lesser extent galena, sphalerite and/or chalcocite. Widespread occurrence of these copper-lead-zinc minerals confirms Tsumeb-style mineralisation at Kaskara.
Drilling at Kaskara has intercepted oxidised zones at over 190 m beneath surface. Extension to depth of such oxidised zones is known to preferentially occur around the ore deposits of the Otavi Mountainland (e.g. Tsumeb, Berg Aukas, Abenab etc.). Deep oxidation and weathering at Kaskara is therefore considered highly favourable for the presence of extensive sulfide mineralisation at and around Kaskara.



the assay results at kaskara are given in a factual way

EXTENSIVE MINERALISATION INTERSECTED AT KASKARA


in the latest report there are clear explanations given on relationships of oxides to sulphides



Relationship of oxide zones to sulphides

The soft, oxidised, hematitic mineralised zones are considered to be in contact with sulphide mineralisation at depth, and have formed as a result of very deep weathering of the rocks in the vicinity of this mineralisation. There is clearly a genetic relationship between the oxide material and sulphide mineralisation which has been documented at other deposits in the region, including Tsumeb and Berg Aukas.


Upcoming drilling will continue to follow these irregular zones to depth in order to track our way to the sulphide mineralisation below.


UPCOMING WORK AT KASKARA


With the forthcoming easing of the wet season rains, Sabre will begin clearing access on the hill at Kaskara. A series of tracks and drill pads will be constructed to enable access to areas that were not accessible in the recent pilot programme.

The upcoming drill programme will comprise deep pattern drilling, using a combination of RC and triple tube diamond drilling. Around 30 holes are planned. This programme will drill deep beneath the outcropping gossans to intercept sulphide mineralisation at depth.