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• 11806-006BZ: Selected samples at 20 m down drill hole through mineralizati<strong>on</strong>, selected BZ samples,<br />

2.11% TREO, 0.50% HREO<br />

• XPS-UZ-Feed: Upper Z<strong>on</strong>e sample processed by XPS Minerals Services<br />

• XPS-BZ-Feed: Basal Z<strong>on</strong>e sample processed by XPS Minerals Services; 1.57% TREO, 0.33% HREO<br />

The total c<strong>on</strong>tent of ore minerals in <strong>the</strong> rock ranges from 5.7% to 20%. If samples c<strong>on</strong>sidered<br />

un-mineralized (some of study 11806-006) are excluded <strong>the</strong>n <strong>the</strong> range is from 7% to 20%.<br />

Recalculating <strong>the</strong>se abundances as a percent of <strong>the</strong> ore minerals is shown in Table 9-3.<br />

Table 9-3<br />

Percent of Ore Minerals<br />

Aval<strong>on</strong> Rare Metals Inc. – Thor Lake Project<br />

% of Ore Minerals in Rock<br />

% of Ore Minerals<br />

in C<strong>on</strong>centrate<br />

11806-<br />

001<br />

11806-<br />

002<br />

11806-<br />

006<br />

11806-<br />

006UZ<br />

XPS-<br />

UZ-<br />

Feed<br />

11806-<br />

006BZ<br />

XPS-<br />

BZ-<br />

Feed<br />

11806-<br />

003<br />

11806-<br />

005<br />

Zirc<strong>on</strong> 58.2% 65.2% 66.8% 61.1% 64.6% 71.9% 69.3% 63.7% 62.3%<br />

Fergus<strong>on</strong>ite 3.2% 3.5% 3.4% 2.5% 2.7% 4.5% 5.8% 5.4% 5.3%<br />

Bastnaesite 2.1% 1.0% 4.6% 5.3% 2.7% 3.9% 6.8% 0.7% 0.8%<br />

Synchysite 4.8% 2.0% 4.9% 5.9% 3.0% 2.5% 6.1% 1.4% 1.6%<br />

M<strong>on</strong>azite 7.9% 5.5% 5.5% 8.3% 10.5% 3.2% 4.0% 5.1% 6.0%<br />

Allanite 19.0% 18.4% 9.2% 11.1% 13.0% 9.6% 6.0% 19.7% 19.5%<br />

O<strong>the</strong>r REE 0.0% 0.0% 0.2% 0.3% 0.0% 0.2% 0.0% 0.1% 0.1%<br />

Columbite 4.8% 4.5% 5.5% 5.6% 3.5% 4.3% 2.0% 3.9% 4.4%<br />

Total 100% 100% 100% 100% 100% 100% 100% 100% 100%<br />

Note that <strong>the</strong> minerals occur in relative abundance from zirc<strong>on</strong>, to allanite, to m<strong>on</strong>azite, with<br />

fergus<strong>on</strong>ite, bastnaesite and synchysite varying c<strong>on</strong>siderably from case to case.<br />

A summary of <strong>the</strong> results given above shows that <strong>the</strong> Upper and Basal Z<strong>on</strong>e mineralizati<strong>on</strong> both<br />

have similar distributi<strong>on</strong>s of minerals with <strong>the</strong> excepti<strong>on</strong> of <strong>the</strong> higher levels of fergus<strong>on</strong>ite and<br />

zirc<strong>on</strong> in <strong>the</strong> Basal Z<strong>on</strong>e (which both relate to HREE). O<strong>the</strong>r than this difference, <strong>the</strong><br />

abundance of <strong>the</strong> minerals is similar in Upper and Basal Z<strong>on</strong>es suggesting that <strong>the</strong> differences<br />

between <strong>the</strong>se z<strong>on</strong>es are in degree ra<strong>the</strong>r than absolute terms.<br />

The ec<strong>on</strong>omically interesting minerals in <strong>the</strong> Nechalacho <strong>deposit</strong> are fine-grained and form<br />

intimate admixtures which have, in <strong>the</strong> past, presented metallurgical difficulties.<br />

Technical Report 43-101 – March 13, 2011 Page 9-3<br />

Prepared by Aval<strong>on</strong> Rare Metals Inc.

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