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Table 8-1 c<strong>on</strong>tinued<br />

moderately altered;<br />

primary minerals altered,<br />

primary textures preserved<br />

fresh or weakly altered;<br />

primary minerals and textures<br />

comm<strong>on</strong>ly preserved<br />

magmatic<br />

mineralizati<br />

<strong>on</strong><br />

67 ZIRCONO-SILICATE CUMULATES (ALTERED) eudialyte/zirc<strong>on</strong> pseudomorphs<br />

cumulate. Some remobilizati<strong>on</strong>. (former<br />

MRZ, 2b basal z<strong>on</strong>e)<br />

65 HETEROGENEOUS SYENITE (ALTERED)<br />

63 FOYAITE II coarse-grained, foyaitic syenite<br />

underlying cumulate z<strong>on</strong>e<br />

a - pegmatitic<br />

61 K-FELDSPAR PEGMATITE<br />

60 LAYERED SODIC SYENITES fresh, green aegirine and white<br />

plagioclase (+/- nepheline)<br />

a. aegirine nepheline albite syenite<br />

b. sodalite nepheline syenite<br />

c. aegirine nepheline K-spar syenite<br />

49 SPOTTED AEGIRINE AMPHIBOLE SYENITE<br />

48 BIOTITE SODALITE AEGIRINE SYENITE<br />

47 LAYERED BIOTITE SODALITE ALBITE SYENITE<br />

45 FOYAITE 3<br />

43 SODALITE AEGIRINE AMPHIBOLE PEGMATITE<br />

99 UNKNOWN<br />

a - pervasive albitizati<strong>on</strong> - unknown precursor<br />

b - pervasive mafic alterati<strong>on</strong> - unknown precursor<br />

c - pervasive fluorite-illite metasomatism<br />

96 FAULT<br />

97 BRECCIA<br />

a. Green breccia unit<br />

b. o<strong>the</strong>r<br />

The primary peralkaline rocks have been altered by pervasive hydro<strong>the</strong>rmal and metasomatic<br />

fluids. This has resulted in <strong>the</strong> partial to complete replacement of <strong>the</strong> Nechalacho syenite unit in<br />

<strong>the</strong> areas of mineralizati<strong>on</strong>. During metasomatic replacement a new assemblage of biotite,<br />

magnetite, specularite, albite and/or chlorite is generated and <strong>the</strong>se minerals tend to be<br />

associated with <strong>the</strong> rare metals and rare earth elements within <strong>the</strong> resource. The last events in<br />

<strong>the</strong> metasomatic sequence include <strong>the</strong> generati<strong>on</strong> of microcline, albite and related silicificati<strong>on</strong>.<br />

There is some suggesti<strong>on</strong> that <strong>the</strong> early-formed rocks were affected by various forms of presolidificati<strong>on</strong><br />

displacement such as magmatic re-sedimentati<strong>on</strong>, magmatic scouring, and<br />

possibly foundering during cooling. The effect of <strong>the</strong>se processes is to obscure lithological<br />

correlati<strong>on</strong>s from cross-secti<strong>on</strong> to cross-secti<strong>on</strong> and give <strong>the</strong> impressi<strong>on</strong> of structural<br />

displacement. In c<strong>on</strong>trast, <strong>the</strong> metasomatic rocks generally show a good chemical correlati<strong>on</strong><br />

Technical Report 43-101 – March 13, 2011 Page 8-4<br />

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

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