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Ammended NI 43-101 Technical Report on the Biely ... - EMED Mining

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<strong>EMED</strong> <strong>Mining</strong> - <strong>Biely</strong> VrchNovember 20<str<strong>on</strong>g>101</str<strong>on</strong>g>1.0 EXPLORATIONThe Slovak Geological Survey had mapped <strong>the</strong> hydro<strong>the</strong>rmal alterati<strong>on</strong> at <strong>Biely</strong> Vrch and <strong>the</strong>ir rockchipsampling of outcropping quartz veinlets yielded geochemically anomalous gold values up to amaximum of 1.1 g/t Au (K<strong>on</strong>ecny et al 2002).The explorati<strong>on</strong> potential of <strong>Biely</strong> Vrch was brought to <strong>the</strong> attenti<strong>on</strong> of <strong>EMED</strong> in 2005 and following<strong>the</strong> granting of <strong>the</strong> Detva Explorati<strong>on</strong> Licence (in which <strong>the</strong> <strong>Biely</strong> Vrch deposit is located) in 2006,<strong>EMED</strong> carried out;- A soil sampling survey <strong>on</strong> a 200 m x 100 m grid spacing revealed a north-southtrending gold anomaly 400 m in length and 200 m in width at >100 ppb Au (max 456ppb Au). The geochemical anomaly was coincident with: An Induced Polarisati<strong>on</strong> (“IP”) chargeability anomaly immediately to <strong>the</strong> west of <strong>the</strong>central quartz-kaolinite alterati<strong>on</strong> z<strong>on</strong>e, which may be due to pyrite – pyrrhotitemineralisati<strong>on</strong> al<strong>on</strong>g a western boundary fault (Figure 9), and A Magnetic anomaly to <strong>the</strong> east of <strong>the</strong> central quartz-kaolinite alterati<strong>on</strong> z<strong>on</strong>e thatmay be due to magnetite mineralisati<strong>on</strong> al<strong>on</strong>g an eastern boundary fault or related to<strong>the</strong> t<strong>on</strong>alite intrusi<strong>on</strong>(s).Figure 8Surface Expressi<strong>on</strong> of <strong>the</strong> <strong>Biely</strong> Vrch Gold DepositFour explorati<strong>on</strong> drill holes were completed in 2006. Hole DVE1, <strong>the</strong> discovery hole, returned 108 mat 1.26 g/t Au from surface and DVE4 returned 252 m at 1.21 g/t Au from surface. A fur<strong>the</strong>r 13 holes(DVE5 to DVE17) were completed in 2007, all of which intersected mineralisati<strong>on</strong>. In 2008, afur<strong>the</strong>r 18 holes (DVE 27 to DVE 44) were drilled at <strong>the</strong> <strong>Biely</strong> Vrch prospect at a 100 m x 100 m gridspacing over <strong>the</strong> mineralised area.Ano<strong>the</strong>r 9 drill holes (DVE 18 – 26) tested <strong>the</strong> halo around <strong>the</strong> <strong>Biely</strong> Vrch intrusive searching forextensi<strong>on</strong>s or repetiti<strong>on</strong>s of <strong>the</strong> mineralisati<strong>on</strong> with negative results.In 2009, a geostatistical analysis of <strong>the</strong> exploratory drilling was undertaken, a geological block modelwas prepared and <strong>the</strong> block model classified into Indicated and Inferred mineral resource categories.This was used as <strong>the</strong> basis for defining a potentially ec<strong>on</strong>omic open-pit mine and a preliminary cut-offgrade, in order to produce a JORC compliant resource estimate (Snowden, 2009).<str<strong>on</strong>g>NI</str<strong>on</strong>g><str<strong>on</strong>g>43</str<strong>on</strong>g> – <str<strong>on</strong>g>101</str<strong>on</strong>g> <str<strong>on</strong>g>Technical</str<strong>on</strong>g> <str<strong>on</strong>g>Report</str<strong>on</strong>g> 19 BEHRE DOLBEARLegal*5650400.1

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