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Message: repost

Here is a repost dealing with mineralization, notice hoqw conveniently the link is broken in this post as well.

Important 2007 release

posted on Feb 16, 13 06:09PMUse the IP Check tool[?]

Below you will see the proof of the different other mineralized structures on the Tesoro besides the veins. This is very important because its showing you that not only do other structures carry gold, they are showing you that a wider mining width can be obtained and is not as dilutive to the grade as if this adjacent rock was barren. Also, if you look at the grades of this other mineralization, you can see that its currently way above what some companies are already mining profitably. Also, your geophysics reveal many of these structure being present on the Tesoro and clearly shows these structures being related to the anomalies. So, if you have gold in these structures at shallow depths, and you can follow these same structures on the geophysics to depths, and remember the gold comes from depth, shouldn,t the anomalies have some gold? Also, I would like you to take note of the widths of these structures, and remember the widths of the samples taken in the drilling results. Also, maybe it may be a good idea to remember some of the alteration widths that Dynacor has, at approx 800m below us in elevation, around 4m or so where sampled. Although they do not appear to widen much over this 800m, it does show widening, and remember that they are much further north and may only be a projection or shoot off the Tesoro larger body. The geophysics from the Tesoro, suggest these zones widening considerably and extensively at the 300m level where they become part of an anomaly that is ~1km wide or wider at the same elevation as Dynacors veins.

Anyhow, here is an excerpt;

In addition to gold occurring in the quartz veins, it also occurs in adjacent rock units (the andesite dyke, fault gouge and fresh granodiorite.) Of 11 samples of "andesite dyke", the average grade is 1.73g/t gold (range 0.02 to 10.0g/t gold) across an average width of 82cm. Of 11 samples of "fault gouge", the average grade is 4.46g/t gold (range 0.05 to 24.7g/t gold) across an average width of 30cm. Of 6 samples of "fresh granodiorite", assays range from 60ppb gold to 870ppb (0.87g/t) gold, with an average grade of 0.36g/t gold across an average width of 40cm. This low-grade material is being stockpiled on surface for possible future processing.

Development work on the A-4 Vein System is ongoing. The A-4 shaft is currently at a depth of 40m.

http://www.steliasmines.com/storage/news_releases/Sli-News-2007-13-FINAL.pdf

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