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Technical Report for the Maricunga Gold Mine - Kinross Gold

Technical Report for the Maricunga Gold Mine - Kinross Gold

Technical Report for the Maricunga Gold Mine - Kinross Gold

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<strong>Kinross</strong> <strong>Gold</strong> Corporation<strong>Maricunga</strong> <strong>Mine</strong> <strong>Technical</strong> <strong>Report</strong>17.0 MINERAL RESOURCE AND MINERAL RESERVE ESTIMATE17.1 IntroductionThe <strong>Mine</strong>ral Resource and Reserve Estimates <strong>for</strong> <strong>the</strong> <strong>Maricunga</strong> Project have beenprepared under <strong>the</strong> direct supervision of Maryse Bélanger, P. Geo., Director <strong>Technical</strong>Services, <strong>Kinross</strong> Americas.During <strong>the</strong> course of 2007, a full review of <strong>the</strong> geologic interpretation and <strong>the</strong> spatial controlsof mineralization was undertaken <strong>for</strong> both Verde and Pancho resulting in new resourcemodels to support updated <strong>Mine</strong>ral Resource and <strong>Mine</strong>ral Reserve estimates.17.2 Interpretation and Grade Domains17.2.1 VerdeThe gold grade model <strong>for</strong> Verde used to rely on a lithological interpretation completed by <strong>the</strong>site geologists to discriminate between mineralized and barren lithologic units. Miningexperience at Verde has shown that <strong>the</strong> mineralization tends to cross over all lithologies.The Verde model update prepared in 2007 incorporates a new interpretation based on abetter understanding of <strong>the</strong> geology and <strong>the</strong> mineralization and its spatial distribution.Essentially, mining has shown that <strong>the</strong> gold content of <strong>the</strong> material mined is often related toits position relative to <strong>the</strong> known post-mineral intrusive bodies at Verde East and VerdeWest.The model update is based on <strong>the</strong> new interpretation <strong>for</strong> Verde East and Verde West. Theconcept and resulting geometry are <strong>the</strong> same <strong>for</strong> both open-pit areas. The mineralizationand its inner limits are defined within a zone of high-grade material centred about a postmineralintrusive. The proximity to <strong>the</strong> post-mineral intrusive is what affects most <strong>the</strong> overallgrade distribution.The halo surrounding <strong>the</strong> higher-grade core is slightly more diffuse and incorporatesmineralization of lesser tenor. The overall concept also concurs with observations in <strong>the</strong>mining areas where <strong>the</strong> material closer to <strong>the</strong> PMI displays stronger brecciation and more78

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