QUEENSTON MINING INC.

Transcription

1 PO Box Government Road Larder Lake, Ontario PK L, Canada Phone () Fax () QUEENSTON MINING INC. IP and Surveys Over the

2 QUEENSTON MINING INC IP and Surveys Railroad Property TABLE OF CONTENTS. SURVEY DETAILS.... PROJECT NAME.... CLIENT.... LOCATION.... ACCESS.... SURVEY GRID.... SURVEY WORK UNDERTAKEN.... SURVEY LOG.... PERSONNEL.... SURVEY SPECIFICATIONS... OVERVIEW OF SURVEY RESULTS.... SUMMARY INTERPRETATION... LIST OF APPENDICES APPENDIX A: STATEMENT OF QUALIFICATIONS APPENDIX B: THEORETICAL BASIS AND SURVEY PROCEDURES APPENDIX C: INSTRUMENT SPECIFICATIONS APPENDIX D: LIST OF MAPS (IN MAP POCKET) LIST OF TABLES AND FIGURES Figure : Location of Railroad Property... Figure : Claim Map with Railroad Grid... Table : Survey Log... Page ii

3 QUEENSTON MINING INC IP and Surveys Railroad Property. SURVEY DETAILS. PROJECT NAME This project is known as the Railroad Property.. CLIENT. LOCATION Queenston Mining Inc. Richmond Street. Toronto, Ontario MH L The Railroad Property is located approximately. km north east of Larder Lake, Ontario. The entire survey area is located in Gauthier Township, within the Larder Lake Mining Division. Figure : Location of Railroad Property Page

4 QUEENSTON MINING INC IP and Surveys Railroad Property. ACCESS Figure : Claim Map with Railroad Grid Access to the property was attained by an unnamed access road. The access road heads north from highway approximately kilometers west of Larder Lake. From here, the x pickup was used for an additional m to a point where the grid crosses this road.. SURVEY GRID The grid consisted of. kilometers of previously established grid lines. The grid lines are spaced meter increments with stations picketed every m intervals. The baseline ran at N for a total length of m. Page

5 QUEENSTON MINING INC IP and Surveys Railroad Property. SURVEY WORK UNDERTAKEN. SURVEY LOG. Date Description Line Min Extent Max Extent Total Survey (m) September Locate survey area and begin IP survey. E N N September Continue IP survey. E N N E N N E N N September Continue IP survey. E N N E N N E N N E N N September Continue IP survey. E N N E N N E N N September Continue IP survey. E N N E N N September Continue IP survey. E N N E N N September Continue IP survey. E N N E N N Begin magnetic survey. Read east half because the ongoing IP survey. E N N E N N E N N E N. N. E N N E N N E N N E N N E N N N E E N E E September Complete IP survey and demobilize gear. E N N September Complete magnetometer survey. E N N E N N E N N E N N E N N E N N E N N E N N E N N N E E N E E Table : Survey Log Page

6 QUEENSTON MINING INC IP and Surveys Railroad Property. PERSONNEL Chris Prest of Swastika, Ontario, was crew chief and operated the IP receiver. His crew consisted of Ryan Perrier, Wesley Cairns, Charles Laframboise, Raymond Richette, Tyler Potts and Florian Fortin. Bruce Lavalley of Britt, Ontario, collected all the magnetic data.. SURVEY SPECIFICATIONS The dipole-dipole survey configuration was used for this survey. This array consists of mobile stainless steel read electrodes and one current electrode (C). The eleven potential electrodes were connected to the receiver by means of the "Snake". The power locations C and C were maintained at a distance of m behind read electrode and the read electrodes had a m spacing to a depth of. A two second transmit cycle time was used with a minimum number of receiver stacks of. A total of. line kilometers of Dipole Dipole IP was performed between September st and September th,. The survey was conducted with a GSM v Overhauser magnetometer in walkmag mode. Samples were collected every second with a simultaneous UTM position stamp also recorded. A second GSM was employed as a base station for diurnal correction. A total of. line kilometers of magnetic survey was conducted between September th and September th,. This consisted of a total of magnetic samples were collected at a.m sample interval. Page

7 QUEENSTON MINING INC IP and Surveys Railroad Property OVERVIEW OF SURVEY RESULTS. SUMMARY INTERPRETATION The magnetic survey indicates a several variations in the magnetic response. The most prominent magnetic feature is a magnetic low that crosses east to west near the baseline of the grid. This feature most likely indicates the contact between either an intrusive or volcanic and the sedimentary package. Along the south flank of this appears intermittent chargeability highs which may indicate mineralization. South of this feature appears an area with substantial magnetic gradients that are in the order of what one would expect for an ultramafic. Within this appears a magnetic low trend at some points an intense low. This trend may represent a structural zone. Anomaly A along this trend represents a chargeability high anomaly. This may be related to the potential structural feature; however may also represent an area of mineralization relating to the possible structural feature. A second interpreted structural feature was added to the map. Along this trend appears a series of weak chargeability signatures. This may indicate a structural trend. For targeting future exploration projects I would recommend focusing south of the bisecting magnetic low, along the interpreted structure S which is labeled A. The magnetic gradients in this structure indicate the most likely presence of an ultramafic. This correlates to the resistivity low and chargeable high. I would focus on the area of maximum chargeability between lines E and E. Additional focus should be made in the area along the magnetic gradient between the suspected sediment and potential porphyry. The chargeable systems along this may indicate areas where there is an increase in mineralization labeled B. Page

8 QUEENSTON MINING INC IP and Surveys Railroad Property APPENDIX A STATEMENT OF QUALIFICATIONS I, C. Jason Ploeger, hereby declare that:. I am a geophysicist (non-professional) with residence in Larder Lake, Ontario and am presently employed as Geophysical Manager of Larder Geophysics Ltd. of Larder Lake, Ontario.. I graduated with a Bachelor of Science degree in geophysics from the University of Western Ontario, in London Ontario, in.. I have practiced my profession continuously since graduation in Africa, Bulgaria, Canada, Mexico and Mongolia.. I am a member of the Ontario Prospectors Association, a Vice President of the Northern Prospectors Association and a member of the Society of Exploration Geophysicists.. I do not have an interest in the properties and securities of Queenston Mining Inc.. I am responsible for the final processing and validation of the survey results and the compilation of the presentation of this report. The statements made in this report represent my professional opinion based on my consideration of the information available to me at the time of writing this report. Larder Lake, ON C. Jason Ploeger, B.Sc. (geophysics) Geophysical Manager of Larder Geophysics Ltd.

9 QUEENSTON MINING INC IP and Surveys Railroad Property APPENDIX B THEORETICAL BASIS AND SURVEY PROCEDURES TOTAL FIELD MAGNETIC SURVEY Base station corrected Total Field Magnetic surveying is conducted using at least two synchronized magnetometers of identical type. One magnetometer unit is set in a fixed position in a region of stable geomagnetic gradient, and away from possible cultural effects (i.e. moving vehicles) to monitor and correct for daily diurnal drift. This magnetometer, given the term base station, stores the time, date and total field measurement at fixed time intervals over the survey day. The second, remote mobile unit stores the coordinates, time, date, and the total field measurements simultaneously. The procedure consists of taking total magnetic measurements of the Earth s field at stations, along individual profiles, including Tie and Base lines. A meter staff is used to mount the sensor, in order to optimally minimize localized near-surface geologic noise. At the end of a survey day, the mobile and base-station units are linked, via RS- ports, for diurnal drift and other magnetic activity (ionospheric and sferic) corrections using internal software. For the gradiometer application, two identical sensors are mounted vertically at the ends of a rigid fiberglass tube. The centers of the coils are spaced a fixed distance apart (. to.m). The two coils are then read simultaneously, which alleviates the need to correct the gradient readings for diurnal variations, to measure the gradient of the total magnetic field.

10 QUEENSTON MINING INC IP and Surveys Railroad Property APPENDIX B THEORETICAL BASIS AND SURVEY PROCEDURES Induced Polarization Surveys Time domain IP surveys involve measurement of the magnitude of the polarization voltage (Vp) that results from the injection of pulsed current into the ground. Two main mechanisms are known to be responsible for the IP effect although the exact causes are still poorly understood. The main mechanism in rocks containing metallic conductors is electrode polarization (overvoltage effect). This results from the build up of charge on either side of conductive grains within the rock matrix as they block the flow of current. On removal of this current the ions responsible for the charge slowly diffuse back into the electrolyte (groundwater) and the potential difference across each grain slowly decays to zero. The second mechanism, membrane polarization, results from a constriction of the flow of ions around narrow pore channels. It may also result from the excessive build up of positive ions around clay particles. This cloud of positive ions similarly blocks the passage of negative ions through pore spaces within the rock. On removal of the applied voltage the concentration of ions slowly returns to its original state resulting in the observed IP response. In TD-IP the current is usually applied in the form of a square waveform, with the polarization voltage being measured over a series of short time intervals after each current cut-off, following a short delay of approximately.s. These readings are integrated to give the area under the decay curve, which is used to define Vp. The integral voltage is divided by the observed steady voltage (the voltage due to the applied current, plus the polarization voltage) to give the apparent chargeability (Ma) measured in milliseconds. For a given charging period and integration time the measured apparent chargeability provides qualitative information on the subsurface geology. The polarization voltage is measured using a pair of non-polarizing electrodes similar to those used in spontaneous potential measurements and other IP techniques.

11 QUEENSTON MINING INC IP and Surveys Railroad Property APPENDIX C Iris Elrec Pro Receiver Specifications CHANNELS / IP RECEIVER FOR MINERAL EXPLORATION simultaneous dipoles programmable chargeability windows High accuracy and sensitivity ELREC Pro: this new receiver is a new compact and low consumption unit designed for high productivity Resistivity and Induced Polarization measurements. It features some high capabilities allowing to work in any field conditions. Reception dipoles: the ten dipoles of the ELREC Pro offer a high productivity in the field for dipole-dipole, gradient or extended poly-pole arrays. Programmable windows: beside classical arithmetic and logarithmic modes, ELREC Pro also offers a Cole- Cole mode and twenty fully programmable windows for a higher flexibility in the definition of the IP decay curve. IP display: chargeability values and IP decay curves can be displayed in real time thanks to the large graphic LCD screen. Before data acquisition, the ELREC Pro can be used as a one channel graphic display, for monitoring the noise level and checking the primary voltage waveform, through a continuous display process. Internal memory: the memory can store up to readings, each reading including the full set of parameters characterizing the measurements. The data are stored in flash memories not requiring any lithium battery for safeguard. Switching capability: thanks to extension Switch Pro box(es) connected to the ELREC Pro unit, the reception electrodes can be automatically switched to increase the productivity in-the-field.

12 QUEENSTON MINING INC IP and Surveys Railroad Property FIELD LAY-OUT OF AN ELREC PRO UNIT The ELREC Pro unit has to be used with an external transmitter, such as a VIP transmitter. The automatic synchronization (and re-synchronization at each new pulse) with the transmission signal, through a waveform recognition process, gives a high reliability of the measurement. Before starting the measurement, a grounding resistance measuring process is automatically run; this allows to check that all the electrodes are properly connected to the receiver. Extension Switch Pro box(es), with specific cables, can be connected to the ELREC Pro unit for an automatic switching of the reception electrodes according to preset sequence of measurements ; these sequences have to be created and uploaded to the unit from the ELECTRE II software. The use of such boxes allows to save time in case of the user needs to measure more than levels of investigation or in case of large D or D acquisition. DATA MANAGING PROSYS software allows to download data from the unit. From this software, one has the opportunity to visualize graphically the apparent resistivity and the chargeability sections together with the IP decay curve of each data point. Then, one can process the data (filter, insert topography, merge data files ) before exporting them to txt file or to interpretation software: RESDINV or RESIX software for pseudo-section inversion to true resistivity (and IP) D section. RESDINV software, for inversion to true resistivity (and IP) D data. TECHNICAL SPECIFICATIONS Input voltage: o Max. for channel : V o Max. for the sum from channel to channel : V o Protection: up to V Voltage measurement: o Accuracy:. % typical o Resolution: µv measurement: o Accuracy:. % typical Induced Polarization (chargeability) measured over to automatic or user defined windows Input impedance: MW Signal waveform: Time domain (ON+,OFF,ON-, OFF) with a pulse duration of ms - s - s - s - s

13 QUEENSTON MINING INC IP and Surveys Railroad Property Automatic synchronization and re-synchronization process on primary voltage signals Computation of apparent resistivity, average chargeability and standard deviation Noise reduction: automatic stacking number in relation with a given standard deviation value SP compensation through automatic linear drift correction to Hz power line rejection Battery test GENERAL SPECIFICATIONS. Data flash memory: more than readings Serial link RS- for data download Power supply: internal rechargeable V,. Ah battery ; optional external V standard car battery can be also used Weather proof Shock resistant fiber-glass case Operating temperature: - C to + C Dimensions: x x cm

14 QUEENSTON MINING INC IP and Surveys Railroad Property WEIGHT: KG APPENDIX C GSM Specifications Overhauser Performance Resolution:. Relative Sensitivity:. Absolute Accuracy:. Range:, to, Gradient Tolerance: Over,/m Operating Temperature: - C to + C Operation Modes Manual: Coordinates, time, date and reading stored automatically at min. second interval. Base Station: Time, date and reading stored at to second intervals. Walking Mag: Time, date and reading stored at coordinates of fiducial. Remote Control: Optional remote control using RS- interface. Input/Output: RS- or analog (optional) output using -pin weatherproof connector. Operating Parameters Power Consumption: Only Ws per reading. Operates continuously for hours on standby. Power Source: V.Ah sealed lead acid battery standard, other batteries available Operating Temperature: - C to + C Storage Capacity Manual Operation:, readings standard, with up to, optional. With VLF stations:, standard and up to, optional. Base Station:, readings standard, with up to, optional ( hours or days uninterrupted operation with sec. intervals) Gradiometer:, readings standard, with up to, optional. With VLF stations:,, with up to, optional. Omnidirectional VLF Performance Parameters: Resolution.% and range to ±% of total field. Frequency to khz. Measured Parameters: Vertical in-phase & out-of-phase, horizontal components, total field coordinates, date, and time. Features: Up to stations measured automatically, in-field data review, displays station field strength continuously, and tilt correction for up to ± tilts. Dimensions and Weights: x x mm and weighs only.kg. Dimensions and Weights Dimensions: Console: x x mm Sensor: x mm diameter cylinder Weight: Console:.kg Sensor and Staff Assembly:.kg

15 QUEENSTON MINING INC IP and Surveys Railroad Property Standard Components GSM magnetometer console, harness, battery charger, shipping case, sensor with cable, staff, instruction manual, data transfer cable and software. Taking Advantage of a Quirk of Physics Overhauser effect magnetometers are essentially proton precession devices except that they produce an orderof magnitude greater sensitivity. These "supercharged" quantum magnetometers also deliver high absolute accuracy, rapid cycling (up to readings / second), and exceptionally low power consumption. The Overhauser effect occurs when a special liquid (with unpaired electrons) is combined with hydrogen atoms and then exposed to secondary polarization from a radio frequency (RF) magnetic field. The unpaired electrons transfer their stronger polarization to hydrogen atoms, thereby generating a strong precession signal-- that is ideal for very high-sensitivity total field measurement. In comparison with proton precession methods, RF signal generation also keeps power consumption to an absolute minimum and reduces noise (i.e. generating RF frequencies are well out of the bandwidth of the precession signal). In addition, polarization and signal measurement can occur simultaneously - which enables faster, sequential measurements. This, in turn, facilitates advanced statistical averaging over the sampling period and/or increased cycling rates (i.e. sampling speeds). The unique Overhauser unit blends physics, data quality, operational efficiency, system design and options into an instrumentation package that... exceeds proton precession and matches costlier optically pumped cesium capabilities.

16 QUEENSTON MINING INC IP and Surveys Railroad Property APPENDIX D LIST OF MAPS (IN MAP POCKET) Pseudo-Sections (:) ) QUEENSTON-RAILROAD-DpDp-E ) QUEENSTON-RAILROAD-DpDp-E ) QUEENSTON-RAILROAD-DpDp-E ) QUEENSTON-RAILROAD-DpDp-E ) QUEENSTON-RAILROAD-DpDp-E ) QUEENSTON-RAILROAD-DpDp-E ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE ) QUEENSTON-RAILROAD-DpDpE Posted profiled IP plan map (:) ) QUEENSTON-RAILROAD-DpDp-CHG ) QUEENSTON-RAILROAD-DpDp-RES Posted profiled TFM plan map (:) ) QUEENSTON-RAILROAD-MAG-CONT Summary Interpretation plan map (:) ) QUEENSTON-RAILROAD-INTERP TOTAL MAPS=

17 Pseudo Section Plot + E a na a Pant-leg I plot point V a = m + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N + N n= n= n= n= n= - n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDp-E Geosoft Software for the Earth Sciences

18 L E E L E L E E L L E L E E L L E L E L E L E L E L E L L N E L E E E E E L L L E E L L L E E L E N L L E L E L L E L N L L E L E L E L E Queenston Mining Inc. L L E Scale : L E L N Map Drawn By: L. LaRocque Date: NAD / UTM zone N Drawing : QUEENSTON-RAILROAD-CLAIM FABRIC

19 LN LN LN LN LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE TOTAL FIELD MAGNETIC nanotesla () Queenston Mining Inc. TOTAL FIELD MAGNETIC CONTOURED PLAN MAP Base Station Corrected Posting Level: Field Inclination/Declination: degn/degw Station Seperation:.m interval Total Field Magnetic Contours: GSM OVERHAUSER MAGNETOMETER/VLF v Scale : NAD / UTM zone N Magnotometer Operated by: Bruce Lavalley Processed by: C Jason Ploeger, B.Sc. Map Drawn By: C Jason Ploeger, B.Sc. Date: Drawing : QUEENSTON-RAILROAD-MAG-CONT

20 LN LN LN LN LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE LE Anomaly Possible Structure Queenston Mining Inc. SUMMARY INTERPRETATION PLAN MAP Survey Scale : NAD / UTM zone N Processed by: C Jason Ploeger, B.Sc. Map Drawn By: C Jason Ploeger, B.Sc. Date: Drawing : QUEENSTON-RAILROAD-INTERP

21 LN LN LN LN LE LE - - LE LE LE LE LE LE - LE LE LE LE LE LE LE LE LE LE LE LE Scale : NAD / UTM zone N LE LE LE LE LE LE LE LE LE LE LE LE LE LE - APPARENT RESISTIVITY ohm.meters Pant-leg QUEENSTON MINING INC. Data Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. a na a I plot point Drawing : QUEENSTON-RAILROAD-DpDp-RES V a = m

22 LN LN LN LN LE LE LE LE - LE LE - LE LE LE LE LE LE LE LE - - LE LE - - LE LE LE LE Scale : NAD / UTM zone N - - LE LE LE LE LE LE LE LE LE LE - LE LE - LE LE CHARGEABILITY Pant-leg QUEENSTON MINING INC. Data Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. a na a I plot point Drawing : QUEENSTON-RAILROAD-DpDp-CHG V a = m

23 - - - Pant-leg Pseudo Section Plot + E a na a I plot point V a = m n= n= n= n= n= + N + N + N + N + N + N + N + N + N n= n= n= n= n= - n= n= n= n= n= + N + N + N + N + N + N + N + N + N n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

24 - - Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= N + N + N + N + N + N + N + N + N n= n= n= n= n= - - n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

25 Pseudo Section Plot + E - - Pant-leg a na a I plot point V a = m + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

26 Pseudo Section Plot + E - - Pant-leg a na a I plot point V a = m + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= - + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

27 Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

28 Pseudo Section Plot + E - - Pant-leg a na a I plot point V a = m + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= - + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

29 Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

30 - - Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

31 - - Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

32 Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= - + N + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDpE Geosoft Software for the Earth Sciences

33 - - Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N + N n= - n= - - n= - n= - n= - n= n= n= n= n= - + N + N + N + N + N + N + N + N n= n= Scale : n= n= QUEENSTON MINING INC. n= n= n= n= n= n= Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDp-E Geosoft Software for the Earth Sciences

34 Pseudo Section Plot + E a na a Pant-leg I plot point V a = m + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDp-E Geosoft Software for the Earth Sciences

35 Pseudo Section Plot + E a na a Pant-leg I plot point V a = m + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDp-E Geosoft Software for the Earth Sciences

36 - - Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= + N + N + N + N + N + N + N n= n= n= n= n= n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDp-E Geosoft Software for the Earth Sciences

37 Pant-leg Pseudo Section Plot + E a na a I plot point V a = m + N + N + N + N + N + N + N n= n= - - n= n= n= n= n= - - n= n= n= + N + N + N + N + N + N + N -. n= n= n= n= n= - n= n= n= n= n= Scale : QUEENSTON MINING INC. Interval: seconds Current: - ma Rx: Iris Elrec Pro Tx: Iris VIP (kw Time Domain) Processed by: Claudia Moraga Map Drawn By: C Jason Ploeger, B.Sc. Drawing : QUEENSTON-RAILROAD-DpDp-E Geosoft Software for the Earth Sciences