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Feasibility Study and Technical Report - Pretivm

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9.0 EXPLORATIONInformation in this section has been excerpted from the Olssen <strong>and</strong> Jones (2012c), whichwas sourced from sections within Ghaffari et al. (2012) <strong>and</strong> updated.In September 2011, Quantec Geoscience was contracted to undertake a Spartanmagnetotelluric (MT) survey of the Snowfield <strong>and</strong> Brucejack Properties. The explorationobjectives were to map <strong>and</strong> detect porphyry mineralization to depth within the Snowfield<strong>and</strong> Brucejack Projects, <strong>and</strong> to establish an underst<strong>and</strong>ing of the geological system <strong>and</strong>fluid pathways to great depth within the Snowfield <strong>and</strong> Brucejack survey area (Gharibi etal. 2011).Approximately 57 lines were surveyed at a spacing of 500 m.The following definition of MT is taken from Quantec Geoscience’s report (Gharibi et al.2011):The (MT) method is a passive/inductive method which measures the timevariationsin the Earth’s natural electric (E) <strong>and</strong> magnetic (H) fields to image thesubsurface resistivity below the sounding site. No source or transmitter is used.The E <strong>and</strong> H fields are measured over a broad range of frequencies from 10 kHzto 1Hz (worldwide lightning activity), <strong>and</strong> from 1Hz to 0.001Hz (oscillations of theEarth’s ionosphere as it interacts with the solar wind). While the E <strong>and</strong> H fieldsare r<strong>and</strong>om, (solar wind <strong>and</strong> lightning activity) the ratio of the fields depends onthe subsurface resistivity structure.The 16 MT stations scattered over the southern part of the Brucejack area provided apreliminary underst<strong>and</strong>ing of the resistivity contrasts. There are clear contrasts betweenrock types <strong>and</strong> a significant interpreted northerly structure that appears to correlate withindicated mineralized zones from Bridge Zone to West Zone. A second interpreted eastnortheaststructure that may off-set the northerly structure is also apparent. The 16stations sparsely cover more than 2 km 2 with significant topography, <strong>and</strong> showdifferences in resistivity responses between individual stations. While the MT data maysuggest geologic features, it should be used with caution.Three-dimensional figures from the Quantec Geoscience report (Gharibi et al. 2011) arepresented in Figure 9.1 <strong>and</strong> Figure 9.2.Pretium Resources Inc. 9-1 1291990200-REP-R0012-02<strong>Feasibility</strong> <strong>Study</strong> <strong>and</strong> <strong>Technical</strong> <strong>Report</strong> on the BrucejackProject, Stewart, BC

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