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Pulacayo Project Feasibility Study - Apogee Silver

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<strong>Pulacayo</strong> 1 000 t/d Phase I <strong>Feasibility</strong> <strong>Study</strong> - NI 43-101 Technical Report<br />

090644-3-0000-20-IFI-100<br />

Figure 14.2: Isometric View of the Oxide-Sulphide Transition Surface DTM – View to NW<br />

Sectional interpretation showed that although silver and lead grade continues across the<br />

oxide-sulphide boundary, the metals show depletion in the oxide zone. Zinc assay core<br />

results are low to anomalous within the oxide zone and are interpreted to be almost<br />

completely depleted. On this basis, the oxide-sulphide surface DTM model was used as a<br />

hard boundary in grade interpolation, with assay composites unable to contribute to the<br />

interpolation of blocks on opposite sides of the surface.<br />

14.3.4.3 Domain Modeling<br />

The spatial distribution of volcanic host rocks and sulphide-silver mineralization contributes<br />

directly to variability in grade distribution within the <strong>Pulacayo</strong> deposit as defined by <strong>Apogee</strong><br />

drilling. Stringer and disseminated style mineralization with locally massive to semi-massive<br />

zones are typical of the TVS within the intruding andesitic volcanics. Despite observed<br />

deposit scale zonation of all three metals throughout the history of mining, with higher grade<br />

silver occurring at middle elevations and increasing base metal values with depth, the TVS<br />

can locally be defined by any one metal or various combinations of the three.<br />

The previous resource estimate by Mercator used an NSR-based spatial domain model to<br />

define that portion of the TVS having the greatest economic potential. Although this method<br />

accommodates spatial grade variability within the deposit and adequately constrains<br />

interpolation, a smearing effect of each metal can potentially occur by diluting higher-grade<br />

vein based mineralization into lower-grade adjacent tons from the lack of hard individual<br />

grade boundaries for high grade structures. Detailed sectional geological modeling<br />

subsequent to the previous resource allowed development of a more precise correlation of<br />

veining and associated mineralization, resulting in a transition from the NSR-domain<br />

methodology to the individual metal domain methodology used in the current resource.<br />

Assay results for silver, lead and zinc were displayed on drill hole traces at nominal 50 m<br />

section spacing and sectional interpretations for each metal based on these values were<br />

used to develop metal-specific, independent, three dimensional wireframe solid models. The<br />

TWP Sudamérica S.A. Av. Encalada 1257 Of. 801, Santiago de Surco Lima 33, Perú (51-1) 4377473<br />

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