2-33 269 DETAIL MAGNETOMETER AND

ELECTROMAGNETIC SURVEYS ON THE

MAPLE-8 (east/west grid)

CLIFFORD TOWNSHIP

LARDER LAKE MINING DIVISION

DISTRICT OF COCHRANE, ONTARIO

FOR

TIGER GOLD EXPLORATION CORPORATION

OCTOBER 13,2006 MISS WENDY K. WELLER

GEOTECH

RECEIVED . OCT 1 6 Z006 ~~

GEOSCIENCE ASSeSSMENT OFFICE

Tiger Gold - MAPLE-8(e/w grid) by Wendy Weller

TABLE OF CONTENTS

TABLE OF CONTENTS

SUMMARY

INTRODUCTION

LOCATION AND ACCESS

PROPERTY HISTORY

REGIONAL GEOLOGY

TOPOGRAPHY

2006-M-8 east/west grid (EIGHT MINING CLAIMS)

MAGNETOMETER/ELECTROMAGNETIC SURVEYS

OBSERVATION AND CONCLUSIONS

CONCLUSIONS

REFERENCES

TECHNICAL DATA

ASSESSMENT DATA FORM

CERTIFICATE

MAPS

LOCATION AND ACCESS (FIGURES Ja)

TABLE 1 - TABLE OF LITHOLOGIC UNITS FOR THE CLIFFORD

TOWNSHIP

7,8

2

3

4

5

5

5,6

6

8,9

9

10

11

12

13

5a)

5b)

GROUND MAGNETOMETER SURVEY MAP NO. M-8(e/w)/2006/mag In back pocket

GROUND VLF-EM SURVEY - NAA PROFILED MAP NO.

M-8( e/w )/2006/vlf. ..... In

pocket

2

back

Tiger Gold - MAPLE-8(c!w grid) by Wendy Weller 4

SUMMARY:

The report includes a Detail Magnetometer and Electromagnetic Surveys as required

by The Ministry of North em Development and Mines for assessment work purposes.

The report includes an introduction to the property, property history, general geology,

field observations and conclusions based on the field surveys.

Technical data is provided at the back of this report. Field data is compiled on the

accompanying plan maps M-8(e/w)/2006/mag and M-8/2006/vlf, found in the back of this

report.

Tigei Gold - ~1APLE-8(e!w grid) by Wendy Weller

INTRODUCTION

DETAIL MAGNETOMETER AND ELECTROMAGNETIC SURVEYS ON THE

MAPLE-8 (east/west grid) CLIFFORD TOWNSHIP

LARDER LAKE MINING DIVISIN DISTRICT OF COCHRANE, ONTARIO

5

There is 1 block (eight units) in the group. Claim 4211988 is located in Clifford

Township, Larder Lake Mining Division.

On October ], 2006 a new south baseline was started. A east/west grid was turned off

the new south baseline at the number 400 meter post west of the number 4 corner post at 270

every 50 meters going east/west and stations cut and measured every 25 meters.

Line cutting was contracted out to Mr. Alain Pariscoat , Mr. Steve Hoffman and Mr. B.

Culhane.

The magnetometer survey was performed by Mr John Perron.

The electromagnetic survey was performed by Miss Wendy K. Weller as well as all

chaining of the picket lines and baseline.

AJ) drafting and contouring and report writing was done by Miss Wendy K. Weller in

the evenings during the project.

LOCATION AND ACCESS FIGURE la) PAGE 5a )

NAD83 5 degree grid

TABLE 1

Clifford and Ben Nevis Townships

Table 1 T"OLE OF LlTIIOLO(;IC l':,\rrs FOR TilE CLIFFORD· BEN 1'\E\"IS :\RE.\.

CENOZOIC

QUATERNARY

Recent PC;lI, alhl\"ium.

Plcistocenc Gr3\1"1 .• and, till 3nd d.1Y.

U", .. "/.Jr,,,i,y

PRECA~lBRIAN

MIDDLE TO LATE PREC:\M8RL\~ (PROTEROZOIC)

~L\FIC I~TRl'SI\'E ROCKS Qli\"iOl' di3h3<r. quaru di3h3,r.

'"/nnire! clln/'It"/

EARLY PRECAMBRMN (ARCHEAN)

FELSIC INTRl'SI\'E ROCKS Granodioritc, quartz dinritr, Ili .. ritr. ,yrnitr. "'hlspou p"'phyry and

qllaru:·rrld<par porph)·r)·.

/""u/;:" (",,'n(1

MAFIC TO INTERMEDIATE INTRUSIVE ROCKS Gahhrn, qllartz "ahlm., hnrnhlrndr .,IhI".. 3nll uinrilr.

\'OLC:\NIC ROCKS

Felsic Volcanic Roclls Rhyexlal"ilc aOlI rhyolile; :o.la"in'. IIl1w.hrn·d.I, IIIIf .hr.I,t"Cia. IIIIf anll

lapilli.lulf.

Intermediate Volcanic Roc'" Antll'~ile and dacile: :o.lauh·c, (lilltl,,"e.I, Row·hrct:da, Iliff, argillite.

Mafic Volcanic Rocks Basalt: Massivc, pillowed, now·hrcccia, luff·hreccia.

Paqe 5 b)

Tiger Gold - MAPLE-8(e/w grid) by Wendy Weller 6

LOCA TION AND ACCESS

The Maple Eight Group is found in the north central half of Clifford Township,

east/west of Highway 672.

The Maple Eight Group is found in the Larder Lake Mining Division, and they are

within the jurisdiction of the Kirkland Lake Resident Geologist. Access is from Kirkland

Lake towards the east for 13 kilometers to the Harker-Holloway road (Highway 672). Follow

672 north for 34.4 kilometers.

PROPERTY HISTORY

At present time, the Maple 8 Group is a new block of unpatented mining claims that is

presently being worked on by Tiger Gold Exploration Limited.

October 6, 2006 a small south grid was handed in, with both magnetometer and

electromagnetic surveys performed.

REGIONAL GEOLOGY

The Clifford Township, is underlain by Archean Volcanic Suites belonging to the

Abitibi Subprovince, Superior Province of the Canadian Shield. The volcanic rocks are

intruded by a variety of related mafic to felsic stocks sills and dykes. Later Precambrian

dykes of diabasic composition and texture trend in a north-westerly, northerly or northeasterly

direction and have filled in along pre-existing structures (see Jansen, 1975 and] 978).

The general area can be defined as being hounded on the south by the Larder Lake

Fault and on the north by the Destor-Porcupine Fault, both regional, east-west trending

Tiger Gold - MAPLE-8(e/w grid) by Wendy Weller 7

structures along which are major gold mining camps such as Timmins, Harker-Holloway,

Kirkland Lake, Virginiatown and Val D'or. A major east-west trending synclinorium is

present between the two faults. The younger Blake River Group is flanked on the north and

the south by rocks of the Kinojevis Group. The southern contact between the two groups is

much more structurally affected than is the northern contact.

Rocks of the Kinojevis Group are to a large extent composed of iron tholeites. Such

iron-rich composition is reflected in bands of high magnetic susceptibility alternating with

bands of lesser magnetism. The weaker zones of magnetism outline sequences of sediments

and/or calc-alkaline volcanics. The contact with the overlying Blake River Group can be

defined from air magnetic data, however a zone of vertical gradation up to a mile wide mayor

may not be present. Subtle maf:,l1letic variations which may represent economically significant

features (Kimberlite pipes or alteration zones) can easily be masked within the Kinojevis

Group.

Blake River Volcanic Rocks are composed of calc-alkaline minerals. Massive and

pillow flows occur in sequence with pillow and pyroclastic breccia and lapilli and ash tuff.

Chemically they represent rhyolite, dacite, andesite and basalt. Rocks of the Blake River

Group underlie the base metal camp of Noranda, Quebec. Eastern Clifford and Ben Nevis

Townships have several base metal showings as well as relatively more bed rock exposures

then has the Elliott Groups.

TOPOGRAPHY

The claim unit covers eight mining claims. The topography of the area ranges from

flat black spruce swamp to the south end of the block to areas of timbered sections. Over three

quarters of the new block has many small outcrop showings that have been timbered. Two

large drainage creek cross back and forth on the south east half of the block of eight. There

are many small timber access roads crossing the block of eight that are four wheeler

accessible. The relief over this block of claims does not exceed 75 to 80 meters. Erosion due

Tiger Gold - MAPLE-8(e/w grid) by Wendy Weiler 8

to timbering operations and natural erosion has exposed small outcrop showings throughout

the block.

2006 M-8(east/west grid) (EIGHT MINING CLAIMS)

MAGENTOMETER AND ELECTROMAGNETIC SURVEYS

McPbar GP81 Proton Magnetometer

This system uses a backward motion of spinning protons of a hydrogen atom within

fluid of hydrogen and carbon. These spinning magnetic protons are caused to have two

opposite poles by applying a magnetic field using a current within a coil of wire. When the

current is stopped, the protons process about the earth's magnetic field and in turn generate a

sman current in the wire. The freqUency is proportional to the earth's total magnetic field.

The instrument used for this survey was a McPhar GP-81 Proton Magnetometer.

More information about the survey and instrument can be found on the Technical Data found

in the back of this report.

Geonics EM-16

The VLF-EM method uses as a source, one of the main submarine communication

transmitters in the 15 to 25 kHz band found throughout the world.

VLF instruments are capable of picking up these structures that change the direction of

the waves by using the tilt angle of the major axis of the polarization ellipse. The direction of

tilt indicates the direction of the conductor.

Tiger Gold MAPLE-8(e/w grid) by Wendy Weller 9

The VLF easily illustrates the location of the upper limit of dipping structures which

can be seen or plotted as VLF profiles as areas of greatest change in tilt angle per unit of

distance.

The station used was Cutler, Maine, 24.0 kHz. For information about the survey and

instrument can be found on the Technical Data Form in the back of this report.

OBSERVATION AND CONCLUSIONS

Magnetic Survey 2006:

The magnetic relief varied between 57,229 gammas to 61,014 gammas (difference of

3785 gammas).

The datum was subtracted at 57,000 gammas.

The field Map No. M-8/2006/mag can be found at the back of this report. The

magnetic trend is north to northwest direction.

In this section of the new grid the there are three magnetic low bands that are

mirrored by two very large magnetic high bands. Inside the magnetic bands there are many

small high circular anomalies. In the north section of the grid the low magnetic bands are

interrupted by a east/west shear or fault zone.

There are two large overburdened outcrops noted with many small stripped outcrops

due to timbering operations in the past 5 years. Due to timbering operations there are many

areas of these outcrops exposed that will be looked at this fall or spring for a geological

survey and possibly a stripping project.

Tiger Goid - MAPLE-8(e/w grid) by Wendy Weiier 10

Electromagnetic Survey:

The field data is presented on a map at a horizontal scale of 1:5000, Map M-

8e1w/2006/vlf. Cutler, Maine was used in this survey.

Cutler, Maine, showed 4 anomalies in the survey.

C1 - Crosses PL700S 215W to PL950S 21OW.

The topography of the area ranges from steep cliff fac·e of a overburdened outcrop to

flat timbered out black spruce swamp. The quadrature is negative. This contact may

well be geological noise.

C2 - Crosses PL600S 160E to PL950S 115E.

The topography of the area ranges from the steep east slope of a large

The quadrature is negative. This contact may also be geological noise.

C3 - Crosses PL 600S 320E to PL 950S 300E.

The topography of the area ranges from the steep east slope of a large timbered

outcrop to the center section of a very steep ravine with a small drainage creek.

The bottom of the creek bed is blue clay and may possible the reason for this

contact. The quadrature is positive.

C4- Crosses PL 000 195E to PL 400S 160E.

The topography of the area ranges from the north edge of a very steep ravine to

the timbered out area of spruce bog. The quadrature is negative.

Due to amount of overburden in the area the vif contacts will have to be

checked by running the Fraser Filter (mathematical equation) on the computer.

This program will help eliminate geolo1:,Tjcal background noise.

Tiger Gold - MAPLE-8(e/w grid) by Wendy Weller 11

CONCLUSIONS

Due to the results of both the magnetic and electromagnetic surveys, a vertical loop

EM unit should be run to further clarify the origins of the magnetic high and low systems.

Also a Fraser Filter program is being run to help identify the vIf contacts, from geological

nOIse.

A geological survey is being planned for the fall and possibly a small stripping and

trenching prob>ram is being looked at for the fall of 2006 to help identify the origins of the vlf

contact.

Respectfully submitted,

OCTOBER 13,2006 ~v1iss VI en.dy K. \Xl eller

Geo-Tech! AGENT

Tiger Gold - MAPLE-8(e/w grid) by Wendy Weller 12

REFERENCES

Weller, W.K. Detail magnetometer and electromagnetic Surveys

Clifford Township, District of Cochrane, Ontario.

March 27, 2006

Ontario Division of Mines Timmins - Kirkland Lake Geological Compilation Series, Map

2205, 1972.

Ontario Geological Survey Airborne Electromagnetic and Total Intensity Magnetic

Survey, Matheson-Black River Area, Elliott Township,

by Questor Surveys Limited, Map 80609, Scale

EM-16, Operating Manual, Page 27.

Tiger Gold- MAPLE-8(e/w grid) by Wendy Weller

TECHNICAL DATA

Line (mi/km) 17. km.

No. of samples/stations 263

ELECTROMAGNETIC SURVEY:

Instrument: GEONICS EM-16

Coil configuration: HORIZONTAL

Method: FIXED TRANSMITTER

Vertical scale: 1 INCH = +- 40%

Frequency: CUTLER = 24.0 kHz

Operational technique: CUTLER, MAINE.

Line traversed:

Line/picket spacing 50m125m

Operator: MISS WENDY K. WELLER

Accuracy: 1 %

Coil separation: INFINITY

Parameters:INPHASE & QUADRATURE

Horizontal scale: 1 :5,000

Station: CUTLER, MAINE

ALL READINGS TAKEN FACING NORTH 90 DEGREES TO THE STATION.

MAGNETIC SURVEY: Operator: Mr. John Perron

Accuracy: + 1 GAMMA

13

Instrument: MCPHAR GP-8 PROTON

Base station: BLOOO Diurnal method: CLOSSED LOOPS BL TIE-

INS

Base station time: EVERY 45 MINUTES Location/value: BLOOO

Contour interval: 50-100 GAMMAS Datum subtracted: 57,000 GAMMAS

Contoured by: WENDY K. WELLER Horizontal scale: 1:5,000

Operational technique: SENSOR POLE MOUNT

INDUCED POLARIZATION SURVEY

Transmitter used:

Method:

On time:

Off time:

Power source:

Electrode array:

Readings taken:

Receiver used:

Frequency:

Range:

Delay time:

Output:

Electrode spacing:

Other data:

Tiger Gold - MAPLE-8(e/w grid) by Wendy Weller

ASSESSMENT DATA FORM

Type of Work:

Prospecting: Geological:

Physical: LINE CUTTING AND CHAINING

Geophysical:ELECTROMAGNETIC (1 STATION) AND MAGNETOMETER SURVEYS

Geochemical:

Assay! Analyses:

Cost of Work: $10,343.00

Recorded holder:

Drilling:

Other Work:

Dollars applied: $10,343.00

Survey Company:

14

Name: THE PERRON GOLD

CORPORA TfON

Name: TIGER GOLD EXPLORATION

CORPORA TION

TIGER GOLD EXPLORATION CORPORATION

Address: 103 Government Road East Kirkland Lake, ant. P2N lA9

Survey/Report Information:

Address: 103 Government Road East Kirkland Lake, ant. P2N lA9

Start of work: October ] ,106 End of work: October 9, /06

Drafting time: Oct. 7,92006 Report time: October 9,13,2006

Completion of report: Oct. 13,2006

Author: MISS WENDY K.WELLER

Work performed on claims: L-4211988

Work applied to claim(s): L-858864

L-980315, L-980316, L-980317, 1-980323, 1-980324, L-980325, L-980329, L-980330,

L-980331, L-980332, L-~MH~~ L-980334, L-980336, L-980337, L-980338, L-980339,

L-980340, L-980341, L-908342, L-980343, L-980344, L-980357, L-1225945,L-301 1709,

Persons who performed work (supervisor first):

TIGER GOLD EXPLORATION CORPORATION

WENDY K. WELLER (Supervisor) JOHN E. PERRON (assistant)

ALAIN PARISCOAT (Iinecutter) ,Steve Hoffman(linecutter), B. Culhane(linecutter).

• Tiger Gold - MAPLE-8(e/w grid) by Wendy Weller

CERTIFICATE

I, Wendy K. Weller, of Virginiatown, Ontario, do hereby certify:

1) That I am a Geotech and reside at:

17 Hilltop Crescent Box 252 V irginiatoWll, Ontario POK lXO

15

2) That I graduated from the Haileybury School of Mines as a certified

Diamond Driller in 1982. I had a staking license for the past 20 years.

3) That I was employed as a Diamond Driller for Heath and Sherwood for

1 year.

4) That I have been practicing as a Geotech for a period of nineteen (20)

years and I am qualified to write this report.

5) That I supervised and participated in this survey.

Date Wendy K. Weller

Geotech/ Agent

N

fUSes

PL300S

~3.)DS

;; ft4o~ ~

~

"" ~ 1t'l5oS

rL5bo~

Pt-SSoS

PUoo5

PCc,9>S

PL-7oo5 .'.',

'PL-75oS

PJ-8DD~

fUWS

ftqroS

PLqX)S

/ .\ '- . \,)

SYM~OLS

Claim Post" Claim Line --­Creek ~.~ -l Highway 672

Access Road .. :,

. . Inphase )I'~ /

>

" Quadrature -..." .. '...:....,-.~--Contact Axis I CI -----INSTRUMENTATION

I Instrument Used: Geonics EM16 station Used: Cutler, Maine Frequency: 24.0 kHz Vertical Scale: ± 40%

GROUND VLF-EM SURVEY

CLIFFORD TOWNSHIP

LAQDER LAKE MINING DIVISION

MAP NO. M-8/2006/vlf

Drafted by: WENDY K.WELLER

Mnppp.d by: Wendy K. Weller

Scale: 1'5000 M 100 0 100

I I I

H~ , ..

2 • 33269

-------------r

•

-..... .... --------------------

, r N

Claim Po~t. Claim Line---.' ("

Access Road,..:... Creekf'· .",

Base Station Isomagnetic

~-o~ contours?

VLF Contacts //

INSTRUMENTATION ,,Jt)

Instrument Used: McPhar GP8 Uatunn substracted 57000

Gammas Contour Intervals 100 Gamma

HAPLE-8 EAST WEST GRID

CLIFFORD TOWNSHIP

GROUND MAGNETOMETER SURVEY

MAP NO. M-8/2006/mag

REPORT BY: WENDY K.WELLER

DRAFTED BY: H.K. WELLER

Scale 1:5000 M

1

100