Sneezer.... Re:SPAMMING CLOWN
posted on
Aug 05, 2008 02:05PM
NI 43-101 Update (September 2012): 11.1 Mt @ 1.68% Ni, 0.87% Cu, 0.89 gpt Pt and 3.09 gpt Pd and 0.18 gpt Au (Proven & Probable Reserves) / 8.9 Mt @ 1.10% Ni, 1.14% Cu, 1.16 gpt Pt and 3.49 gpt Pd and 0.30 gpt Au (Inferred Resource)
I quess you forgot about the anomolies that NOT did not hit on... Not that they are misses... just that they require more work... as does PRB's most recent hits of host periditite....The hole in the SE on PRB was to intersect a target at antisipated intersection of DE at about 400 meter depth! It did hit the host peridotite but at a higher elevation than the airboard indicated. This hole was at about a 70 degree angle had it been more vertical the results may have been different.
The target is at a depth of 400 meters but the intersection was at about 275 vertical passing through the ultramafic intrusion.
Thus the VTEM being redone, and downhole and ground loop to better define the target for the next phase of drilling within the next couple months.
PRB has currently about $4 to 4.5 million to undertake its work proposals...
Clearly had PRB hit massive sulphide, NOT would have also benifited from this.... I hold all 3 stocks and others... This is an area play... and all will benifit when critical mass is achieved... Thats why NOT has jv'd a lot of it's land to others.... to achieve critical mass without consuming all it's own resources and manpower.
I don't see any positive to come from the confrontational comments from Sneezer et all....JMHO
Just in case you forgot that NOT has not hit on every hole as he states, heres a few:
AT-3 anomaly
A total of 2,621 metres were drilled in eight holes testing airborne anomaly AT-3, located four kilometres to the southwest of Eagle One. These holes intersected altered (talc-chlorite alteration) and non-altered strongly magnetic peridotite units that were locally mineralized with disseminated sulphides. No significant assay results have been received to date. The presence of magnetite veinlets and disseminated sulphide mineralization in the peridotite provide some evidence of conductivity and explain the high-magnetic signature. Samples were selected from all mineralized sections, were submitted for multielement analysis and results are pending. An attached table lists the holes drilled at AT-3 anomaly, with the results from holes assayed to date.
AT-4 anomaly
A total of 951 metres in three holes were completed to test airborne anomaly AT-4 and its southwestern extension, located 5.5 kilometres southwest of Eagle One. Two holes encountered volcanogenic massive sulphide-style mineralization in intermediate to felsic volcanic assemblages and the third hole was lost. The holes returned several large widths of barren sulphide mineralization in favourable volcanic rocks uncomformably overlying the Ring of Fire. Minor visible copper-zinc mineralization observed here justifies continued exploration along this favourable northeast- to southwest-trending stratigraphy. All samples selected will be reported upon once assays have been received. An attached table lists the holes drilled in this anomaly area; all assays for the holes are pending.
AT-8 anomaly
Only one hole tested this anomaly located 6.3 kilometres to the southwest of Eagle One and two kilometres east of AT-3 anomaly. Hole NOT-08-1G29 tested airborne anomaly labelled AT-8. The hole encountered altered peridotite with little sulphide mineralization. The peridotite exhibited strong chlorite alteration and only minor sulphide mineralization was observed. No sampling was done on this hole. Deeper penetrating geophysical surveying is required here to further explain the cause of the airborne anomaly.