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technical report on the nechalacho deposit, thor lake project ...

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from secti<strong>on</strong> to secti<strong>on</strong> - this may be a reflecti<strong>on</strong> of pressure/temperature differences or a<br />

chemical disequilibrium boundary.<br />

REE, Ta, Nb and Zr mineralizati<strong>on</strong> in <strong>the</strong> Nechalacho <strong>deposit</strong> occurs in broad, enriched subhoriz<strong>on</strong>tal<br />

replacement z<strong>on</strong>es, in additi<strong>on</strong> to being widely disseminated over much of <strong>the</strong><br />

<strong>deposit</strong>. Minerals hosting <strong>the</strong>se elements are primarily zirc<strong>on</strong>, fergus<strong>on</strong>ite, ferro-columbite,<br />

allanite, m<strong>on</strong>azite, bastnaesite and synchisite. The highest grades of HREEs, LREEs, niobium,<br />

and tantalum tend to occur in magnetite-hematite and zirc<strong>on</strong>-rich areas within <strong>the</strong> sub-horiz<strong>on</strong>tal<br />

replacement z<strong>on</strong>es.<br />

The Nechalacho <strong>deposit</strong> is hosted by a layered magmatic peralkaline intrusi<strong>on</strong> of aegirine<br />

syenites, nepheline syenites and related cumulates. REE-bearing minerals were originally<br />

<strong>deposit</strong>ed in-situ as disseminated grains, probably eudyalite, during cooling and as cyclic<br />

cumulate layers. Hydro<strong>the</strong>rmal alterati<strong>on</strong> of <strong>the</strong>se original zirc<strong>on</strong>-silicates has partially<br />

remobilized <strong>the</strong> REE’s, particularly <strong>the</strong> LREE’s as part of <strong>the</strong> process of metasomatism. For <strong>the</strong><br />

LREEs, remobilizati<strong>on</strong> appears to be fairly local, but could also have been more extensive,<br />

<strong>deposit</strong>ing LREE’s in z<strong>on</strong>es away from <strong>the</strong>ir original site of crystallizati<strong>on</strong>. HREE’s do not<br />

appear to be remobilized and <strong>the</strong>ir occurrence is c<strong>on</strong>sidered to be in-situ.<br />

Technical Report 43-101 – March 13, 2011 Page 8-5<br />

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

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