Titiribi Gold: Sleeping Giant in the Colombian Cordilleras (a Geophysical Study)

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1 Titiribi Gold: Sleeping Giant in the Colombian Cordilleras (a Geophysical Study) Emmett Van Reed, P.Gp. Zonge Engineering & Research Amit Tripathi, Ph.D. Terra Resources Development Technologies Jennifer L. Hare, Ph.D. Zonge Engineering & Research

2 The Search for Gold The town of Titiribi is located in the Antioquia Department, a province in the Republic of Colombia. The Sunward Resources Ltd (TSX-V: SWD) property, near the town of Titiribi, is located within the Colombian Cordillera. For two centuries Titiribi was a historic gold production center with several gold smelters, even minting its own currency. While gold has been associated with localized high-grade polymetallic veins, during the last decade large mineralized porphyries have been discovered, probable source of historic ores. This more recent quest for gold started with old mining records, geological mapping and surface geochemistry. In 1996 Zonge Engineering was asked to conduct geophysical surveys on the Colombia West gold property. Discussed today will be use of ground magnetic data and galvanic/electromagnetic geophysical techniques, Induced Polarization (IP) and Controlled Source Audio-Frequency MT (CSAMT), proved useful for mapping subsurface geology and drill target identification at Titiribi.

3 Titiribí Currency

4 Colombia, Antioquia Department Rregional Geology Colombia West Project Site (Titiribi)

5 Town of Titiribi, Antioquia Department Republic of Colombia Cerro Vetas Virgen Peak

6 Geophysical Program Based on surface geochemistry, a Geophysical Field Program was implemented to map subsurface geology at Titiribi The Geophysical Field Program collected Total Magnetic Intensity (TMI), Induced Polarization (IP) and Apparent Resistivity. Two Geometrix G-856 magnetometers were used for Magnetic Field Measurements. A Zonge GDP-32 Geophysical Receiver and GGT kw geophysical transmitter were used to collect Dipole-Dipole CR-IP and CSAMT field data.

7 Colombia West Grid and Ground Magnetic Grid Collected by Zonge: Lines A thru G, and Lines 1 thru 8 Dipole-Dipole IP Resistivity Lines Collected by Zonge: Lines 1 thru 8 CSAMT Lines Collected by Zonge: Lines 2, 4 and 6

8 Geophysical Tool Box: Magnetics Ground Magnetic Survey Measures: Total Magnetic Field Intensity (TMI). Maps: Magnetic susceptibility/distribution of magnetic minerals (for example magnetite & pyrrhotite). Importance: One of the three rock properties important on this project relating geophysical data to geology. The other two are the electrical parameters, Resistivity and Induced Polarization (IP). Note: Filtered magnetic maps include low pass, upward continued, gradient, and RTP. Analytical signal (total gradient) map is alternative to RTP at low latitudes.

9 Total Magnetic Intensity Map

10 Magnetic Analytical Signal (Total Gradient)

11 Geophysical Tool Box: Dipole-Dipole IP Dipole-Dipole Resistivity IP Survey Measures: Apparent Resistivity and IP, either in the frequency domain (CR-IP) or time domain (TD-IP). Produces Pseudosection Data which represent resistivity and induced polarization changes associated with geology. Importance: Two of the three rock properties important on this project relating geophysical data to geology. Comment: IP is associated with specific mineralization important in exploration programs.

12 CR-IP, Field Data: Line 6

13 CR-IP, 2D Smooth Model Resistivity & IP Cross Section: Line 6 Inversion Smooth-Model Resistivity (ohmmeters) Inversion Smooth-Model IP (milliradians)

14 RESISTIVITY FACTORS IP FACTORS LOWERS RESISTIVITY: porosity water content clay alteration dissolution salinity shearing faulting weathering metallic mineralization RAISES RESISTIVITY: carbonate precipitation silicification fresh water IP SOURCES: Disseminated Metallic-luster Minerals Pyrite Chalcopyrite Alteration Clay Sericite Graphitic Rocks Biotite REDUCES IP: Oxidation of pyrite-like sulfides Massive pyrite-like sulfides INCREASE OR DECREASE RESISTIVITY: metamorphism and alteration

15 Geophysical Tool Box: CSAMT Controlled Source Audio-Frequency Magnetotelluric (CSAMT) Maps: High-resolution Resistivity frequency based soundings. Measures: Electric and Magnetic fields, magnitude and phase (determines Resistive Impedance). Good lateral with moderate vertical resolution. 2D Smooth-Model CSAMT Resistivities complement 2D Smooth-Model Dipole-Dipole Resistivities, yet provide increased model resolution with greater modeled depths Note: CSAMT is not a precision IP mapping technique.

16 Electric Field Dipoles Magnetic Field Coil Scalar CSAMT Field Setup Schematic (not to scale) Electric Field Dipoles 50 m (= one station)

17 CSAMT, 2D Smooth Model Resistivity Cross Section with Field Data: Line 6

18 Colombia West Project

19 CR-IP Grid: 2D Smooth-Model Resistivity Porphyry

20 CR-IP Grid: 2D Smooth Model IP Porphyry

21 Where to Drill?

22 Comparison: Plan View Images with Magnetics NW NE NE P P P Modeled IP, 200 m depth Modeled Resistivity, 200 m depth Total Field Magnetic Drill Holes Completed x Proposed Drill Holes Note: CSAMT collected on Lines 2, 4 & 6

23 Comparison: Plan View Images with Magnetics 0 0 Modeled IP, 200 m depth Total Magnetic Intensity Total Magnetic Intensity Resistivity Overlay < 100 ohm.m Induced Polarization > 65 mr Resistivity Overlay < 100 ohm.m Drill Holes with Gold values

24 Geophysics and Geology Other than known high-grade veins worked in the vicinity of Titiribi, rock outcrop is generally poor. The geophysical survey identifies an important mineralized porphyry at Titiribi. Line 6 crosses the Cerro Vetas Porphyry. The extent of this Porphyry is identified by modeled IP, Resistivity and Total Magnetic Intensity, with patterns clearly identified on the Plan View Imaged sections. The intense IP response suggests pyrite-like mineralization is not massive, but distributed as stock-work veins or as disseminated sulfides. The intersection between the Plan View Imaged Induced Polarization and Total Magnitude Intensity (middle panel in Slide 23) may provide an interesting clue. Geophysics by itself can only suggest possibilities. Drill core and sample rock geophysical property testing provide important links between geophysical data and geology.

25 CR-IP Line 6: 2D Smooth-Model Resistivity 0 Porphyry Core The Green Line represents the 2009 topographic profile used to locate drill holes. This differs from the 1996 topographic profile used to re-model these lines in For now we just have to recognize this difference when matching results.

26 CR-IP Line 2: 2D Smooth-Model Resistivity

27 CR-IP Line 6: 2D Smooth-Model IP Porphyry Core 0

28 CR-IP Line 2: 2D Smooth-Model IP

29 CSAMT Line 6: 2D Smooth-Model Resistivity-Comparison 2D Smooth-Model Resistivity CSAMT, a = 50 m Note the difference In lateral resolution! Dipole-Dipole CRIP a = 200 m

30 Summary IP is associated with specific mineralization important to exploration at Sunward Resources Ltd Project at Titiribi, Colombia. Geology, combined with geophysics, provide optimum targets for drilling. Geologic models developed at this time provide critical guidance for the next stage of exploration the investigation similar geologic features in the vicinity of Titiribi. IP clearly identifies structure or geologic contacts which appear to divide the Cerro Vetas porphyry into at least two phases (monzonite & monzodiorite for example). Drilling indicates that Gold is associated primarily with magnetite and chalcopyrite, and occurs in higher concentration in the argillic alteration zone with high clay-magnetite around the more potassic porphyry nucleus. The argillic alteration zone appears to be well defined by both Resistivity and IP. Within zones defined by contacts, Drill hole logs and Magnetic data suggest areas with either high or low gold to magnetite ratios. Areas with high ratios appear to be associated with earlier geologic events.

31 Mineralization Out Crop Drill Core

32 Gold

33 Moz gold equivalent Cerro Vetas Inferred Resources Au Cutoff (g/t) avg grade Au (ppm) avg grade Cu% Moz Au equivalent

34 Acknowledgements Zonge Engineering wishes to express thanks for the collaborative effort of Dr Amit Tripathi with Terra Resources Development Technologies, in helping prepare this talk. Zonge Engineering also wishes to express thanks for the support provided by Sunward Resources Ltd (TSX-V: SWD); Goldplata Resources Ltd; and partners in supporting this talk by providing information from their Colombia West program. In addition, Zonge Engineering wishes to thank others for their contribution to the geophysical program at Titiribi, from ACE Development to the many Minera Muriel field helpers in 1996, without whose help we wouldn t be here today discussing this project.

35 Project Location Compilation Geology map

36 Soil Au and Geophysics

37

38 Line 6 CSAMT with gelogical model

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