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NI 43-101 Independent Technical Report Mount ... - Adex Mining Inc.

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<strong>NI</strong> <strong>43</strong>-<strong>101</strong> <strong>Independent</strong> <strong>Technical</strong> <strong>Report</strong> Rev 02 January 22 nd , 2010<br />

<strong>Mount</strong> Pleasant North Zone Preliminary Assessment (Project 6526-03) 9-2<br />

The Endogranitic and North W-Mo sub-zones are not included in the focus of this <strong>Report</strong>.<br />

Figure 9-1: Representative Cross-section of <strong>Mount</strong> Pleasant Mineralized Zones<br />

(Figure Credit: Watts, Griffis & McOuat)<br />

The eight modeled sub-zones or deposits that make up the North Zone are distributed over an<br />

area of 450 by 250 metres extending from the surface to a vertical depth of 450 metres. An 1,100<br />

metre decline, which was used to collect bulk samples in 1986, extends from the Fire Tower Zone<br />

underground workings to the Endogranitic sub-zone. The decline and underground workings are<br />

presently flooded. An exploration drive developed in the 1960s extends from the surface to the<br />

vicinity of the #1-3, #4 and #6 Tin Lode sub-zones. Many of the North Zone deposits contain<br />

significant amounts of indium with the zinc. Indium-bearing tin-base metal zones in the North<br />

Zone appear to be principally associated with sphalerite and are more concentrated in the Deep<br />

Tin Zone (Sinclair et al, 2005). Host rocks are often brecciated and altered to a fine-grained,<br />

greisen-type assemblage of quartz, sericite, topaz and fluorite.<br />

The principal mineralogy of the deposits consists of fine to very fine-grained cassiterite,<br />

arsenopyrite, löllingite, sphalerite and chalcopyrite with lesser amounts of stannite, pyrite,<br />

marcasite, galena, wolframite, molybdenite, tennantite, chalcocite, bornite, native bismuth,<br />

bismuthinite and wittichenite. Other associated minerals include abundant fluorite and chlorite<br />

(Kooiman et al, 2005). The tin and porphyry tungsten-molybdenite deposits of the North Zone<br />

represent two different periods of mineralization even though they overlap spatially. Tin<br />

mineralization in the North Zone is younger than the Fire Tower Zone and crosscuts the older<br />

molybdenum-tungsten zones.<br />

Thibault & Associates <strong>Inc</strong>.<br />

Applied Process Chemical Engineering

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