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NI 43-101 Technical report, Surface diamond drilling ... - Iamgold

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R a r e E a r t h E l e m e n t E x p l o r a t i o n P r o g r a m M a r c h - 2 0 1 3<br />

W i n t e r - S u m m e r 2 0 1 2 P a g e | 112<br />

Item 22. RECOMMENDATIONS<br />

22.1 Geological compilation and resources modelling.<br />

The new geological information collected during the 2012 <strong>drilling</strong> program was not totally<br />

interpreted. The REE zone contacts were frequently intercepted, especially at depth, and an<br />

update of the geological model is needed. In the Saint-Honoré carbonatite complex context,<br />

the 2011 geological model (Lafleur, P.J., 2012) contained enough detail to update the TREO<br />

resources without any doubt on the reliability of the results. By modeling the transition zone<br />

(“low grade zone”) and the REE core zone (“high grade zone”) a grade interpolation could be<br />

applied individually to those new geological volumes. The expected results on the resources<br />

model will be an increasing of the TREO concentration coupled with a decreasing of the<br />

tonnage in the core zone. With cumulative mineral inventory of over 1 billion tonnes,<br />

decreasing the tonnage won’t have a negative aspect compared to the benefit of increasing the<br />

concentration.<br />

The specific gravity used for the 2012 block model included the 2011 back ground value for<br />

the carbonatite of 2.86 t/m 3 . Basic statistics made over the new available density data base<br />

returned an average value for the carbonatite of 3.11 t/m 3 . This change must be studied. An<br />

increasing amount of barite is noted at depth and must necessarily affect the density. A<br />

density distribution pattern, within different geological domain or inside one domain, must be<br />

integrated to the next geological interpretation and blocks model.<br />

The TREO value is a composite of 14 individual rare earth elements values added together.<br />

A proportion relationship between each element was established by P.J. Lafleur. Base on this<br />

information only the TREO attribute was calculated for the 2012 block model. The statistic<br />

and the variography of each element should be added for validation or comparisons.<br />

22.2 Mineralogical characterisation and metallurgy.<br />

A Mineralogical study is ongoing. The petrographic, the geochemical and the mineralization<br />

characterisation of the REE zone at depth, under 500 metres below surface, are the objects of<br />

a master project. Preliminary <strong>report</strong> should be produced to help the geological modeling and<br />

metallurgical test works. A synergy between geological improvement and metallurgical<br />

testing would be benefit to the REE project.<br />

The hyper spectral technology might help the geological team to build a homogeneous data<br />

base to improve the actual geological model. Even if the traditional core logging description<br />

seems to work for outlying the core zone, the spectral technology can precisely evaluated the<br />

REE mineral concentration and nature especially in the brecciated facies where the<br />

granulometry become smaller. It is recommended to test the benefit of the hyper spectral<br />

technology by building the library with the entire representative and available core.<br />

3400, chemin du Columbium, St-Honoré-de-Chicoutimi, QC G0V 1L0 Canada – tel. : 418 673-4694 Fax : 418 673-3179<br />

E-mail : info.niobec@iamgold.com www.niobec.com

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