Geophysical Surveys Report on the Butt Uranium Rare Earth

I I I I I I I I I I I I I I I I I I I

GEOPHYSICAL SURVEYS REPORT

on the

BUTT URANIUM RARE EARTH PROPERTY

BUTT TOWNSHIP

DISTRICT OF NIPISSING

ONTARIO

FOR 2. 45460

RECEIVED GRIFTCO CORPORATION

prepared by:

JUN 1 6 2010

GEOSCIENCE ASSESSMENT OFFICE

Dan Patrie Exploration Ltd.

L.D.S. Winter, P.Geo.

7 June 2010


TABLE OF CONTENTS

1. Introduction

2. Property 2.1 Property Description 2.2 Location, Access and Infrastructure

3. Geology

4. Instrumentation and Work Done

5. Results 5.1 Magnetometer Survey 5.2 Induced Polarization Survey

6. Summary and Conclusions

7. Recommendations

8. Personnel

9. Expenditures

References Certificate of Qualification

Figure 1 : Location Map Figure 2: Claims Map Figure 3: Regional Geology Figure 4: Property Grid

LIST OF FIGURES

Figure 5: Induced Polarization (IP) Chargeability Anomalies

LIST OF MAPS

Map 1: Total Magnetic Intensity Survey- Contoured Readings 1:5 000 8 pseudosections 1:5 000

PAGE

3

3 3 4

5

6

8 8 9

13

14

14

15

16 17

2


1. INTRODUCTION

Griftco Corporation (Griftco or the Company) holds 10 claims containing 88 units

and covering 1408 ha in Butt township, District of Nipissing, Ontario at 79° -5.8'W

longitude, 45°-42.5'N latitude (Figure 1 ). The claims are held under option from Dan

Patrie Exploration Ltd. (OPEL) and were acquired for their potential to host uranium

and rare earth mineralization of economic interest. Between 6 April and 20 April

2010 the Company carried out line cutting and a magnetometer survey followed by

an Induced Polarization (IP) survey on part of the Property. The following report

describes the work carried out on the subject claims and the results obtained.

2. PROPERTY

2.1 PROPERTY DESCRIPTION

The Butt Uranium Rare Earth Property ("the Property") is comprised of 10

unpatented contiguous mining claims containing 1 0 units and covering 1408 ha as

listed in Table 1 and as illustrated in Figure 2. The Property is located within the

Butt township claim map area (M-0064). The claims are held in the name of Dan

Patrie Exploration Ltd. and the Property is under option to Griftco Corporation by an

agreement dated 8 January 2010.

3

I I I I I I I I I I I I I I I I

FIGURE 1

I GRIFTCO CORPORATION

I BUTT URANIUM RARE EARTH PROPERTY

Location Map

I Scale 1:750 000 June 2010


TABLE 1

GRIFTCO CORPORATION

BUTT URANIUM RARE EARTH PROPERTY

Township Claim Number Claim Due Date Units Area (ha)

Butt 4214914 201 0-Jul-25 12 192

Butt 4214915 201 0-Jul-25 12 192

Butt 4214916 201 0-Jul-25 8 128

Butt 4214917 201 0-Jul-25 12 192

Butt 4214918 201 0-Jul-25 12 192

Butt 4219905 201 0-Jul-25 12 192

Butt 4246897 2011-May-12 2 32

Butt 4246898 2011-May-12 3 48

Butt 4246899 2011-May-12 3 48

Butt 4246900 2011-May-12 12 192

TOTAL 88 1408

2.2 LOCATION, ACCESS AND INFRASTRUCTURE

The Property is located approximately 50 km north-northeast of Huntsville,

Ontario at 79°-5.8'W longitude, 45°-42.5'N latitude and centred at UTM, NAD 83,

Zone 17 co-ordinates 650000mE; 5062500mN (Figure 2).

Access to the Property is by road from Provincial Highway #11 at Elmsdale,

Ontario about 20 km north of Huntsville. From Elmsdale, Provincial Highway 518

leads east to Kearney (10 km) then proceed north from here an additional 10 km to

Sand Lake. From Sand Lake to the Property is about 12 km on the Forestry Tower

Road. A number of logging roads provide good access to all sections of the

Property.

4

-----------------

\

y

After Claim Map M-0064, 1 Butt Township Scale: 1:40 000 UTM Zone 17, NAD 83

4219905

421 4914

4214917

421491 8

-

FIGURE 2

GRIFTCO CORPORATION BUTT URANIUM RARE EARTH PROPERTY

Claim Map June 2010


Algonquin Park is immediately east of the Property and the Cal Graphite

Property is immediately to the north (Figure 2).

3. GEOLOGY

The Butt Uranium Rare Earth Property is located within the Kiosk domain of the

Algonquin Terrain of the Central Gneiss Belt of the Western Grenville Province,

Ontario (Figure 3). The central Gneiss Belt and the Central Metasedimentary Belt

are the 2 major subdivisions of the Grenville Province in Ontario.

The Central Gneiss Belt consists mainly of upper amphibolite and local granulite

facies, quartzo-feldspathic gneisses chiefly of igneous origin with subordinate

paragneiss. The dominant structural trend is northeasterly, however, northwesterly

trends occur along Georgian Bay. The Central Gneiss Belt consists of a variety of

Archean to Mesoproterozoic crustal segments, all of which have been affected by

the "Grenville Orogeny". Rocks of 3 main ages are present. North of the French

River, reworked Archean and Paleoproterozoic gneisses of the Nipissing Terrane

are intruded by Mesoproterozoic (1700 to 1350 Ma) plutonic rocks, with granitic and

monzonitic rocks predominant. The bulk of the Central Gneiss Belt (Algonquin and

Tomiko terranes) consists of Mesoproterozoic gneisses (1800 to 1600 Ma) intruded

by 1500 to 1400 million-year-old granitic and monzonitic plutons that may represent

an extension of the Eastern Granite-Rhyolite Province across the Grenville Front.

The Parry Sound Terrane consists of mafic to intermediate rocks extracted from the

mantle at about 1450 to 1350 Ma.

Distinctive lithotectonic terranes, some further sub-divided into domains, have

been identified within the Central Gneiss Belt. The terranes and domains are

distinguished by differences in rock types, internal structure, metamorphic grade,

geologic history and locally by geophysical signature. They are bounded by zones

of intensely deformed layered rocks traceable for tens of kilometres.

5


Georgian

Bay

Abbreviations A Ahmic Domain 8 Britt Domain

Be Beoverstone Domain CMBBZ CenTral Metosedimentory Belt

Boundary Zone F Fishog Domain

GFTZ Grenville Front Tectonic Zone

• PROPERTY

Age of crust or major period of magmatism

~ 1170 10 1100 Ma

Q 1300 to 1250 Mo

- 1450 to 1350 Mo

Lake Ontario.

GH Go Home Domain H Huntsville Domain K Kiosk Domain

Me McCraney Domain Mel McClintock Domain MR Moan River Domain N Navar Domain

FIGURE 3

GRIFTCO CORPORATION

BUTT URANIUM RARE EARTH PROPERTY Regional Geological Framework

After: OGS, Geology of Ontario

Part 2, p. 720

~ 1800 to 1600, ~ 1500 to 1400 Ma

~ 2700 to 2300 Ma

m Paleozoic cover rocks

/ Terrane boundary

/ Domain boundary

NE Nepewassi Domain 0 Opeongo Domain P Powossan Domain

PS Parry Sound Domain R Rosseau Domain S Seguin Domain

TL Tilden Lake Domain

June 2010


The Algonquin Terrane consists of quartzo-feldspathic gneisses of plutonic and

supracrustal origin characterized by a complex pattern of structural domains. Thus,

the Algonquin Terrane is an area of Mesoproterozoic, polycyclic rocks, consisting of

a number of domains (domains and subdomains ). The southern and western parts

of the Algonquin Terrane have been subdivided into the Britt, Ahmic, Kiosk,

Rosseau, Go Home, Huntsville, Novar, McClintock doamins interpreted to represent

the lowest portion of a stacked succession of thrust sheets in this region. Large

folded sheets of gneissic granites with primary isotopic ages in the 1500 to 1400

million year range occur in all these domains. Rocks of this age are common in the

Eastern Granite-Rhyolite Province and the Algonquin Terrane and probably

represent a section of Mesoproterozoic crust (1800 to 1600 Ma) extensively injected

by granitic magmas of the Eastern Granite-Rhyolite Province. (Central Gneiss Belt,

Grenville Province, Part 2, Section 19, Geology of Ontario, Easton, 1992).

The Butt Uranium Rare Earth Property which lies within the Kiosk domain, is

underlain by mafic, quartzo-feldspathic and metapelitic units at the amphibolite to

granulite grade of metamorphism. In turn these units host radioactive pegmatite

dykes which host allanite, uraninite, pyrochlore, columbite and other rare earth and

uranium-bearing minerals (Ferguson, 1971; Hewitt, 1967).

4. INS"rRUMENTATION AND WORK DONE

Line cutting was carried out on the Property between 6 April and 17 April 2010

inclusive by OPEL with 27 line-km being cut.

Between 17 April and 20 April 2010 inclusive, a program of geophysical

surveying along the previously cut lines at 100 m spacings was carried out over part

of the Property (Figure 4). A total field magnetometer survey with readings being

taken at 25 m intervals was carried out over 27 line-kilometres (Map 1) .

The survey was carried out using 2 Scintrex Envi magnetometer units. The Envi

Mag has the capability to measure the total field combined with an Envi

6

I I I I

I ~

I

BUTT TWP.

URANIUM

RARE EARTH

PROPERTY

FIGURE 4

GRIFTCO CORPORATION

I BUTT URANIUM RARE EARTH PROPERTY Survey Grid

I

N


Magnetometer as a base station for correcting magnetic diurnal drift. These are

total field magnetometers which measure the magnetic field through the use of

proton processional effects caused by the interaction of a magnetic field with a spin

aligned, proton rich fluid.

An instrument accuracy precision and resolution of 0.1 nt may be obtained with

these instruments under ideal conditions. While in gradient mode which was not

done at this time, the unit has the means of measuring both the total field and the

gradient of the total field with two sensors simultaneously. In gradient mode, the

instrument sharply defines the magnetic responses determined by the total field. It

individually delineates closely spaced anomalies rather than collectively identifying

them under one broad magnetic response. Also, when doing a gradient survey the

instrument enables one to conduct a gradient survey during a magnetic storm

because the technique of simultaneously measuring with the two sensors cancels

out the effects of diurnal magnetic variations.

Microprocessors contained in these instruments allow for the collection of the

readings along with the time and its position in digital form suitable for downloading

to a computer for date processing.

A total of 27 km of magnetic readings were taken along the lines at 100 m apart

with 25 m station intervals. The field measurements were corrected for diurnal

variations of the earth's magnetic field by direct subtraction of the base station

readings from the reading taken at the same moment in the field units. The

corrected data was downloaded to a computer for plotting. The results are

presented in Map 1.

A total of 17 km of induced polarization readings were taken on the Butt Property

grid with an "a" spacing of 25 m and with 6 levels being read (N = 6). The IP survey

was a time domain pole-dipole survey and it was carried out with a Walcer 9000

transmitter in combination with a Honda 18 HP motor generator and a Scintrex IPR-

12 receiver. The motor generator and transmitter were stationary on the end of the

7


line being read with the current being transmitted through a wire with an electrode

into the ground for contact. A second wire and electrode (the live electrode) was

moved along the line being surveyed as per the survey protocol. At all times, the

transmitter man, live electrode man and receiver personnel were in radio contact.

Ahead of the live current electrode was a crew of men with electrodes at 25 m

intervals. These electrodes are connected to the receiver where the receiver

operator obtains and records the readings. The data is downloaded from the

receiver at the end of the day to a computer where the resistivity and chargeability

are calculated and plotted using pseudosections and/or maps using Geosoft

software.

The geophysical surveys were carried out by Dan Patrie Exploration Ltd.,

Massey, Ontario an experienced geophysical contractor. The survey personnel are

listed in Section 8. The IP survey was performed between 17 April and 20 April

2010 (inclusive).

5. RESULTS

5.1 MAGNETOMETER SURVEY

In an earlier report on the Property the writer (Winter, 2009) wrote, 'The total

field magnetic readings taken on the Butt Township Property indicate that the

property is divided into 2 magnetic domains along a line trending approximately 330°

(N60°W). To the northeast of this line, the magnetic readings are generally low and

vary between approximately 55000 nT to 55500 nT with scattered, more elevated

values to a maximum of approximately 56000 nT. Two trends appear to be present,

330° and 060° - 070° with the 330° trend being more noticeable. The southwestern

part of the Property has in general a higher magnetic susceptibility with values

generally in the 55600 nT to 56200 nT range".

The current survey was done in the eastern part of the earlier survey area and

shows the pattern originally reported, i.e., higher magnetic values to the south and

8


lower values to the north with the boundary between the 2 domains trending about

330° (northwest-southeast) (Map 1 ).

For the current survey, the highest values occur in an irregular pattern in the

southern 25% of the grid. Here values are generally in the range of 55300 nT to

occasionally over 55800 nT. Apart from the overall 330° trend, two other general

trends are apparent, east-west and northeasterly.

North of the baseline at 30+00N {UTM northing 5063000mN) the magnetic

readings are generally less than 55250 nT and range to lows in the 55100 nT range.

Some high values to a maximum of 56048 nT occur at the northern end of L22+00E

between 38+00N and 39+00N (Map 1 ).

In summary, it is considered that the magnetic values indicate the presence of

two magnetic domains, one to the north where the magnetic susceptibilities of the

rocks are lower (55250 nT to 55100 nT) and one to the south where magnetic values

range from about 55300 nT to over 55800 nT. Three overall magnetic trends are

present, northwesterly (330°), east-west and northeasterly.

5.2 INDUCED POLARIZATION (IP) SURVEY

A total of 17 line-km were surveyed during the IP survey with the results for each

pseudosection summarized in Table 2. Pseudosections for partial lines from

17+00E to 25+00E and the baseline are provided in the pockets of the report (8

pseudosections). Figure 5 is a plan map, compiled from the pseudosections which

shows diagrammatically the location of and the trends of the main zones of

increased chargeability.

In general the background chargeability values range from <0 mVN to 5 mVN to

10 mVN. Zones of increased chargeabilities range up to 66 mVN, however, most

anomalous values are in the 20-30 m VN range i.e., the areas of increased

chargeability are in the order of 2 x to 6 x background. The areas of increased

9


chargeability show, in general, two types of patterns.

Figure 5 shows the zones of increased chargeability interpreted from the

pseudosections (n = 1 ). From about 29+00N to 34+00N on lines 17+00E to 25+00E

the interpreted IP zones show combined northeast to east-west trends with the

northeasterly trend being dominant. In the southern part of the grid, the IP zones

have a dominant northwest trend; 19+00E to 25+00E and 17+00N to 24+00N.

Resistivities are variable. In some cases increased chargeabilities occur with

increased resistivity while in other cases low resistivities are associated with higher

chargeabilities.

10

I I I I I I I I I I I I I I I I I

BL

FIGURE 5

GRIFTCO CORPORATION BUTT URANIUM RARE EARTH PROPERTY

Induced Polarization (IP) Chargeability Anomalies

Scale: line spacing 100 m June 2010 ·


LINE

17+00E

18+00E

19+00E

20+00E

TABLE 2 GRIFTCO CORPORATION

BUTT URANIUM RARE EARTH PROPERTY ZONES OF ANOMALOUS CHARGEABILITY

CHARGEABILITY VALUES STATION BACKGROUND ANOMALY

mVN mVN

From end of line (30+00N) to <0 to 5 >5 to 26

33+50N

From end of line (30+00N) to <0 to 5 >5 to 34

33+50N

40+00N to north end of line

<0 to 5 >5 to 9

From end of line {20+00N) to <0 to 10 >10 to 20

24+00N

28+00N to <0 to 10 10 to 28

31+50N

41+00N

22+00N to 24+00N

<0 to 10 10 to 30

28+00N to <0 to 10 10 to 20

32+50N

COMMENTS

Broad zone at south end of line with 2 more anomalous sections at 30+00N and 32+50N. Coincident with high resistivity 2 x to >14 x background.

Broad zone at south end of line with one more anomalous section at 30+00N. Coincident with high resistivity 2 x to 20 x background.

Increasing chargeability with increasing resistivity at north end of line.

Broad zone of increased chargeability with highest values at 23+50N. Variable resistivity.

Broad zone of increased chargeability with 2 more anomalous sections at 28+75N and 31+00N. Section at 31+00N has highest chargeabilities. Section at 28+ 75N shows higher resistivities while that at 31+00N shows lower resistivities.

Increasing chargeability and resistivity at end of line.

Broad zone of increased chargeability. In general coincident, high resistivity.

Broad zone of increased chargeability separated into a northern and southern section. Southern section at 29+00N has higher associated resistivities.

11


22+00E

23+00E

24+00E

25+00E

19+00N to <0 to 10

22+00N

30+00N to 3 to 10

32+00N

17 +OON at south end of line to 0 to 10

19+00N

30+00N to 35+00N

<0 to 10

18+00N at south end of line to 4 to 10

22+50N

26+00N to 34+00N

3 to 10

17 +OON at south end of line to 0 to 10

18+00N

26+00N to 33+00N

3 to 8

33+00N to 1 to 10

34+00N

Broad zone of increased chargeability with 2 more

10 to 32 anomalous sections at 19+00N - 20+00N and 22+00N with coincident increased resistivity.

200 m wide zone of increased

10 to 24 chargeability, increasing with depth. In part low and in part higher resistivity.

200 m wide zone of increased 10 to 32 chargeability with coincident

high resistivity.

Broad irregular zone of increased chargeability with

10 to 23 generally low resistivity except for a small zone at 33+00N -34+00N of higher values.

Broad zone of increased 10 to 19 chargeability below n = 3 with

associated high resistivity.

Broad zone of increased chargeability with 3 narrow sections of more anomalous values at 26+00N, 27+50 to

10 to 34 29+00N and 31+50N to 34+00N. The first 2 sections show increased resistivity whereas the 3rd section has low resistivity.

Modest increase in 10 to 17 chargeability with low

resistivity.

Modest irregular increase in 8 to 12 chargeability with high

resistivity.

Approximately 1 00 m wide zone of high chargeability with

10 to 66 associated low resistivity. This zone contains the highest chargeability values obtained during the survey.

12


6. SUMMARY AND CONCLUSIONS

A total field magnetometer survey was carried out on 27 line-km of cut lines

spaced at 100 m in the eastern part of the Property. An earlier survey (Winter,

2009) indicated two magnetic domains on the Property, one with lower magnetic

susceptibilities to the north and one with higher magnetic susceptibilities to the south

with the boundary between the 2 domains trending northwest-southeast (330°). This

overall pattern also shows up in the current survey with the general boundary

between the 2 domains being at about 30+00N (UTM 5063000mN). In addition to

the 300° trend, two other trends, east-west and northeasterly are also present.

The IP survey chargeability results show 2 main zones of anomalous

chargeabilities/interest. The first area lies at and north of the baseline (29+00N to

34+00N) and from 17+00E to 25+00E. Within this area, anomalous zones show

northeasterly and east-west trends. The second area of anomalous values lies from

17+00N to 24+00N and between 19+00E and 25+00E, in the southeastern part of

the grid.

Previous work in the 1950's identified a number of radioactive showings, for the

most part hosted in pegmatite dykes. Some of these reported showings lie adjacent

to the anomalous chargeability zones, however, for other showings there appears to

be no correlation.

In summary, the magnetometer survey returned similar results to the earlier

survey (Winter, 2009) and within the area surveyed confirmed the presence of two

mqgnetic domains, an area of low magnetic susceptibility to the north and an area of

higher magnetic susceptibility to the south. Three general trends or patterns are

indicated by the magnetic survey, northwesterly (330°), northeasterly and east-west.

The IP survey identified two areas of anomalous chargeability values, one in the

north-central part of the grid and one in the southeastern part of the grid. The IP

anomalies also show the same 3 trends as shown by the magnetic survey.

13


At this point, there is no apparent direct correlation between the IP anomalies

and areas of known radioactivity.

7. RECOMMENDATIONS

At this point, it is considered to be important to determine, if possible, what is the

cause of the increased IP chargeability and if there is any relationship between areas of

known radioactivity and the IP and/or magnetic survey results. To this effect, it is

recommended that;

1. the Property be geologically mapped and,

2. all showings be cleaned out, mapped and sampled.

Based on the prospecting and sampling work from the 1950's, it is considered

that the Property has considerable potential to host uranium and rare earth element

(REE) mineralization of economic interest. Once the recommended mapping and

sampling are completed, the results can be correlated with the geophysical survey

results and then a comprehensive evaluation program can be implemented.

8. PERSONNEL

The surveys were carried out by Dan Patrie Exploration Ltd., Massey, Ontario

using the following personnel.

Mike Faulkner, Walford, Ontario

Gab Roy, Elliot Lake, Ontario

Mike Whalen, Walford, Ontario.

Bronson Ede, Sudbury, Ontario

Andy Desjardins, Espanola, Ontario

Tyler Gagan, Espanola, Ontario

Cliff Moffatt, Sudbury, Ontario

Matt Mandigo, Massey, Ontario

Brent Patrie, Val Therese, Ontario.

14


9.

1.

2.

3.

4.

5.

6.

EXPENDITURES

TABLE 3 GRIFTCO CORPORATION

BUTT URANIUM RARE EARTH PROPERTY EXPLORATION EXPENDITURES APRIL 2010

Line cutting: 27 km@ $650/km

Magnetometer Survey: 27 km @ $150/km

IP Survey: a= 25m; n = 6: 17 km@ $1600/km

Two mobilization trips; one for line cutting and

one for geophysical surveys@ $1600 each

Data Processing/printing maps

Report (6 copies)

Total

$ 17,550

4,050

27,200

3,200

2,000

2,600

$ 56,600

The expenditures were made on three (3) claims in the following proportions:

4246900

4214917

4214918

33.3%

42.6%

24.1%

Total 100.0%

L.D.S. Winter, P.Geo.

7 June 2010

15


1.

2.

3.

4.

5.

REFERENCES

Easton, R.M., 1992

The Grenville Province and the Proterozoic History of Southern and Central Ontario; p. 715-754, The Central Gneiss Belt, in Geology of Ontario, Part 2, MNDM.

Ferguson, S.A., 1971

Columbium (Niobium) Deposits of Ontario, ODM, Mineral Resources Circular 14, p. 49.

Hewitt, D.F., 1967

Uranium and Thorium Deposits of Southern Ontario, ODM, Mineral Resources Circular No. 4, p. 47.

Marmot, C. and Johnston, M., 1987

Mineral Deposits Studies in the Huntsville-Parry Sound-Powassan Area -A Progress Report, OFR 5647, OGS, Mines & Minerals Division.

Winter, L.D.S., 2009

Magnetometer Survey Report on the Butt Township Property, Butt Twp., Dist. of Nipissing, Ontario for Dan Patrie Exploration Ltd., 11 pages, 4 Figures, 2 Maps.

16


L.D.S. Winter

1849 Oriole Drive, Sudbury, ON P3E 2W5 (705) 560-6967

(705) 560-6997 (fax) email: [email protected]

CERTIFICATE OF AUTHOR

I, Lionel Donald Stewart Winter, P. Geo. do hereby certify that:

1. I am currently an independent consulting geologist.

2. I graduated with a degree in Mining Engineering (B.A.Sc.) from the University of Toronto in 1957. In addition, I have obtained a Master of Science (Applied) (M.Sc. App.) from McGill University, Montreal, QC.

3. I am a Life Member of the Canadian Institute of Mining, a Life Member of the Prospectors and Developers Association of Canada, a Registered Geoscientist in Ontario and in British Columbia (P.Geo.).

4. I have worked as a geologist for a total of 50 years since my graduation from university.

5. I have read the definition of "qualified person" set out in National Instrument 43-101 ("NI43-1 01 ") and certify that by reason of my education, affiliation with a professional association (as defined in Nl 43-101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the purposes of Nl43-101.

6. I am the author responsible for the preparation of the Geophysical Survey Report titled "Geophysical Surveys Report on the Butt Uranium Rare Earth Property, District of Nipissing, Ontario" and dated June 7, 2010 (the "Technical Report").

Dated this th Day of June, 2010

L.D.S. Winter P.Geo.

17

700 800 900 I "-- - ,-- -----"';"-----

1000 1100 "" 1-'' ---'-';"

0 0 N v

0 0 0 v

0 0 ro M

0 0 m M

0 0

;;\

0 0

"' "'

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0 0

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~~ 0 0 v N

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700 800 .. --'o---ccOc::--900 1000 1100 ' 1200 1300

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--o2occo"oc---2=-1"'oo ' 1400 ' 1600 1500 1700 1800 1900

2200 2300 T-----------· I

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55563 55528 55502 55479

55461

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55407 55397 55384 55373 55361 55351

55340 55331 55323

55312

55302

55292 55281

55270 55259 55249

55240 55231

55223 55213 55204 551 97 55188

55178 55166 55153

55136 55112

FULL COLOR SCALE BAR CONTOURED@ 100nT & 1000nT

Scale 1:5000 100 0 100 200 300 ~-- I

metres

MAP1

GRIFTCO CORPORATION L TO. TOTAL FIELD MAGNETICS SURVEY

BUTT URANIUM RARE EARTH PROPERTY 1--- ::_::__:_ DATUM SUBTRACTED; OnT

REFERENCE FIELD; 55256nT INSTRUMENT USED. SCENTREX ENVI SYSTEM

DAN PATRIE EXPLORATION LTD.

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?oon I --~. ___ ) __ _ ---'--· _ ___ I ~- · - . .1-.--. t___ I . ---- ·-· ' _ __J _ _ ,-J__ . .L---L-- I -~- ___ .J... ___ , ... I - - ··- ·· .--L-. . --L- .. ~ I 200G ()

Cha rgeabil ity

29+00 N .50r00 N 3 1+00 N :~?+00 N 33+00 N j4rQQ N j~·rOO N ."~6+00 N 37+00 N :>:> .6 23.9 u.~. 11 .4 13 .8 1o.7 1€- . 3 149 a.111 7 . i 4 6.0<~ -1-.95 3 . 74 ?.:2 :> . 4 1. 43

38r00 N .59 r 00 N 40+00 N fitter i8 n - 1

iiite'" Chargeability n~1

n~2

n-.1

n-:-4

fl-~)

,.,- 6

~t=2 2~

~ 1/

n-:j 15 11

1'•' 4 7

" j n .. !; ?

1 ,,.E; -·1

29+00 N 3o~oo N . F;l\er 22900 HOOO 8680

alcu lated Res1stiv:it¥~ 1

3 1+00 N 32+00 N JJ •OO N 3~+00 ~ 35+00 N 36+00 N 37•00 N 38~00 N 39f 00 N ~0+00 N Fill~a l culated Resistivi

39 n .... 1 :Jhrr1•r~•

Ohm•m .-;=2

n=J

n-4

o=6

o~2

'"" ~ n-.3 1~iJ~ 793~

n u~ 6858 B 56.51 .. <1.157 _ ..

.,,s 3015 23?0

ll -"t:i 1~63

Geosoft Software for the Earth Sciences

Pseudo Section Plot 17+00 E

Dipole-Pole Array

a na a

Pant-leg Filter

* * * *

* "

/ ' / ' / ' / ' / ~~

* * plot point

Logarithplif Contour-S .5, 2, 3, 5, 7 .5, 1 0, ...

-· []

0

50

INTERPRETATION Strong increase In polarization accompanied by marked decrease in resistivity.

Well -defined increase in polarization without marked resistivity decrease.

Poorly defined polarization increase with no resistivity s ignature.

Low res istivity feature.

Scale 1:5000 0 50 100 150 200 250

metres

GRIFTCO CORPORATION

a= 50 m

300

INDUCED POLARIZATION SURVEY

TT URANIUM RARE EARTH PROPE

Date: 22/05/2010 Interpretation:


TY

Calculated Re~H~lkillv!j~obi ity Ohm•rn

ChorCJ(>Al:Uxtl.iJJYJled Resistivity onm"rn

,··-·----,----.-----,---,----, ··-rl4()()()

r·l:woo

35 14()(j() --,-- I ·······.-- -r--· ,--, . . ·-r-·... - ···~- ······---.----~··

jQ :2000

-~-/~) 10000

20 ......

25 ·IOCOC

/0

35

3G

ROr>O· -·80GO ':5· "I!)

5000 ,. .... ~·'· 10 ......

-6000 10

5 4000· 4UUU 5

0 2000· ~--~--L--~--L- -?000 0

/.9i·OO N 30+00 N .11 +00 N J2100 N jjiOO N 34100 N 35~00 N 36+00 N 37+00 N jH+OO N .:'>CJ+OO N 4C+OO N 41 I 00 N Chargeability

Chorgeability Filter 31 5 n~1

29. I

r 2

,, _I

o-4

n-!)

1=6 9

29+00 N hlter 92'10

alculated Resistivit,y-_ 1

5140

n=3

n=4

n=5


.?C 9 16.R L\ 1 -~. 1 H .:s 13.9 9.95 9.54 6.78 5.42 3.77 3.23 3.32 2.46 :.81 2.53 ?. 55 ;I.'- 4 08 2.8 6.24 6.53 8.06 rilter

u=2

n=3

(1--1

'1-6

-(g l 11

A -6 4 2 I

-0

30+00 N :S1+00 N 32+00 N .D+OO N 34+00 N 35+00 N 36+00 N 37-fCO N 38+00 N 40+00 N 41+00 N Filt~alculated Resistivi 6640 10400 1.3!:>00 12500 1 0~00 9230 7220 3990 ~ 1 w :lo:lo 3St>O 3020 2()30 3520 3650 4050 4220 t:.580 4990 5850 6530

6/ n = 1 Ohrn•m

n-2 22771

I 9:.>22

n~:s /-.$!':> 6.)94

n=4 5662 B '·832 .590':>

n~5 :\T\6 261~

n=O 1605

4641

4~~r:.~ 6629

loiBim:,.-1'9-t-7~--? 2 35 4064 409 1 ~;, 3572 j.5'<9 j /

98-- 3190 3 126 3267 4205~~821

S518 3885 4 157 3778 ~:,t,-57

~7 3961 5032._ 4725 _5088 5249

3625 33 16 5196 48 7/\ :l453 5743 5629

401\fi.-- 4--100 40813 .3~ 81 .3656 4994-652-2--644


Dipole-Pole Array

a na a

Pant-leg Cj ru---Filter '

/ /

' /

' /

' /

* * ,,

* plot point

Logarithp1ip Contours .5, 2, 3, 5, 7.5, 10, ...

•

0

50

INTERPRETATION Strong increase in potarization accompanied by marked decrease in resistivity.

Well defined increase in polarization without marked resistivity decrease.

Poorly defined polarization increase with no resistivity signature.

Low resistivity feature.

Scale 1 :5000 0 50 100 150 200 250

metres

GRIFTCO CORPORATION

a=50 m

300

INDUCED POLARIZATION SURVEY TT URANIUM RARE EARTH PROPE

1-----·-·-----·--------------------1 Date: 22/05/2010

Interpretation:


TY

Chorgecrukiit~ted l~esistivi ty

;l()l 1tl

I()

I I,

OH'n•n

1 :?.-

10

~

6 ·

~ -

2

0 ·-··- -·~ I _ J .. ---··~--- 1

19-tUO N 20 +00 N 21+00 N 22~00 N 2.3-t·OO t-.1

Chargeability 11 . 2 12.1 10 . 2 11 . 9 14

n~4

n-6

19+00 N ~0+00 N 21 +00 N 22 100 N 2.3 100 N • F;ltcr :w~oo

olcu lated Res 1 stivit¥~ 1 19900 :wzou /.'>300 23700 / 0.500 1800C Hl/00 15600

n-5

n....:t)


l --L - '--- - L _: _ _ _ .._L • •• - I _ _J - I

24+00 N 2~ ~oo N ~ 6+CO N 2 / +00 N 28+00 N 29+0C N 1? 12 . 7 12 .2 8 .09 5 .88 6 . 12 7 . ~9 5 .94 8 . 15 9.49 13 .6 15 . 6

?6-+00 N 28+0[) N 2~J +OO N 9i00 10600 9~5C 91 90 15500 1 /900 15200 ., ~)300

)?952 7836

;);;.___';290 ~~~~?"

_ _ _ _ I -

30+00 N 15. 1 12. 4

Co1cu.oled Re~y.obilily Ql'lru• m

-- \ -,---- I --,--,-- .,.-,-.,.-------,--. . '-r-1 . I ' --r-·1- 1 l f/}>COO

~ 12COOO

........... . ·1!)()00

--- - - - - ___ - - -~- 11()000

--------- --- ----~===-=-=------------- -~-=-------------=----- 5000 ~~~-:;::.::;- ---------------- l J . _ _l_ l _ ____..... __ - - . L · --1 . I ·-'- ~ .l-. __1. -...,._ __I I - ·-· I . _.1 1.-.. ...L _ _ J •• _. ()

.32+00 N JJ+OO N 5'1+00 N J !.l+OO N JS+OO N J/+00 N 58+00 N .:59+00 N ?O •UO N 41-100"' 15 .. ~ 19.3 19 . 1 !2 . 7 17..7 5 . 5 7 ~ . 1/1 3 . 09 7. . 84 1.18 7. .83

u=- /

n-.3

n- ' ..

70

16

-10

t\

-lj

4

0

Chargeabll ity

30-IOG "J 3 1100 N 32 100N 33 ·10 0N 34 100 N 351·00 N .'36·100 N 37 100N 38 100N 391 00N 4C~OON 41100 N f'i l t~alculated Resistivi y

B

n=6


Dipole-Pole Array

a na a

Pant-leg Filter " ..

* " * *

/ ' / ' / ' / ' / ) ,

* " plot point

Log a rit'lf.'if Contours .5, 2, 3, 5, 7.5, 10, ...

• []

0

50

INTERPRETATION Strong· increase in polarization accompanied by marked decrease in resistivity.

Well defined Increase in polarization without marked resistivity decrease.

Poorly defined polarization increase w ith no resistivity s ignature.


Scale 1:5000 0 50 100 150 200 250

metres

GRIFTCO CORPORATION

·-f

a =50 m

300


T URANIUM RARE EARTH PROPE



TY

Chorgcclxilii!JDtcd r~esistivil y Ct: lculo I ed Rc!fit:ti'f'g~<Jbi !i l y

15

5

0

Ohm tr ·r Otun •in ~2000· - ·-···- : - ···- ··-,-····· - ···- o· ··--· ··-,-· ····· ·-- I - ·--·· r· ,--,-, - ---,,.-- - ,,----,- - , '''' ·r--···· ' I

?0.100 -- - ~ HSUOO- .-···- -·--\ ' ~ ~

.,- ·.......---.....---..-..,....--r---.--, --- -,--.-- .. , ' --~--...----,---~- 22000

!~~-1L-----: .-- --~ /-~------ ~ / ~ -- -----=~~-------- -, __ C\~100 -, ____ .. -- ' '. /' ''----------.,. "--········-··-····· ",. -·- ---------// .. / .. ' ',· .... ,, . ''·······-..... -----··

... '·-....... ,.,.... .... __ -·-- ........................ ------...__ --··-·- --·-------~/.... OtJOO

6000] .. _ ./ --------~-~==--- . ------------===-----======---- _/ . ~-000

7.00()()

1/lOOO

1500':)

14000

17000

10000

1\000

1000 - -- .. - ._ - - - ·------- -------------/.000- ·---'-- · - -·L- l - - L··-··-· 1---•--•--.. 1.-. 1 - -·..i.. '-- 1 - .. ··· - •--L---'- ' --1--.L---- · · ·\ L _.1 ·J:::=:=-:r-: I .J . .. --l- t-·-· 1 .. .L-- '--- L-- .... /()()0

2!.> 1-oo N :to+oo N 2 1 1 oo N 2S+co N 29+00 N .Ju 1 oo N .5 1 +OO \1 32+00 N

20

10

Filter

r. ~ 1

14 . 1

19•00 N 14.9 14.

LU•OO N 21 <00 N 13.? 1J . 4 13./ 1)

<11 t-OO N 33 I 00 N . .5-'11·00 1\J .S!i-'-00 N .36+00 1\ 'J/ I uu N .JB+OO N .19+00 N '10+00 N 1.~ 4 .95 ~ . '/!> 1 .•17 1 .61 <;.7•1 10.1 995 :1.5 13.7 '1/.!) 1 .~. 1 11 14.3 13 .2 I .27 2.96 6.91 11. 3 H. H 6. /,S ~> ll6 1 . 22 3. 96 3 . .3') 3. 59 3. 13 .\. lil ') 19 S :55 2 . 5& .3. 09 '1. IS 2. 66 il. I Chargeability

Chargeability

12

19100 N 70+00 N 71+00 N 1 1 I 1 1 e 1 I t I t I I t

24100 N I I I I

, 2~1-90 .N , . 7?+~)0 1 N /!+~):1 .N 2R+OON . , 2?190 .N , . 39190 ,N .Sl+OON 7!>90 se 1c 1 0:~oo 16400 2

1

1200 ' ,s~oc' 16400 19Joo 1 7Coo 1 c~ll.'\J 1~1r)o ' ,Aoo' I' iller 1 OSOO 1 UDO 10/:i(JO 901 0 1 01 00 1 1800 alculatcd Resistivit:v~ 1

n-7.


I 4

6

:s/+OO N 3310o N .3410o N .J!:+OO N .)o+CO N 37100 N 38100 N , , .s?~·~>o ,N . , '~9+90 ,N. 4119o.N I 71

1

50 I 7410 561

101 48?l) I -'!4

1

/l() I ~ 1 /Q I .'S61fi{) I .'l460 I 2 i 90

1 2sso 1 30

170

1 J67Q 1 s/70

1

.lfi()(J H9() 41\;'>-:J 5880 6410 7050 ~520

590 1 3455 3659

3390 3954 :~9 1 7 4060 3939 .>7 17

n ·2

n - 5

n=4

n=::>

r-=6

1i ~ 12 10

6 , 3 2 c

1 ;n~alculated 9 4 r.=1

n= /

n-3

n= 4

?.7 1'-'8 ~ 162u· 1 2l9~ 1 0f>U6 900/. 7171 .. ~892 4Utl15 - · J2U9 / 154

B


Dipole-Pole Array

na a

Pant-leg Filter

* * * *

* * *

" ' " ' , ' " ' " "' plot point

Logarithmic Conto~r1"T.5, 2, 3, 5, 7.5, 10, ...

• D

0

.,

INTERPRETATION Strong increase in polarization accompanied by marked decrease in resistivity.

Well defined increase in _polarizatioo w ithout marked resistivity decrease.

Poorly defined polarization increase w ith no resistivity signature.

Low resistiv ity feature.

Scale 1 :5000 50 0 50 100 150 200 250 ~

metres

GRIFTCO CORPORATION

a= 50m

300 I



DAN PATRIE EXPLORATION L TO.

TY

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

7.4·1 22 ?() -

\8-

16

8·

I)·

4

Chargeability

1 7 +90 IN I . 1 ~ +yo . N f'iller i 6 . 1 '. 7. 6 /.?.. 3

n= 1

1 9~oo N ?O+OO N 1 /

1

0> 01

. ·/ :!c . 8 1

.) 1 I

n- ?

n.·-3

n - 0

l/1 00 N 18+00 N 19+00 N 20 100 N


2 1 +00 N 7.2; CO N 2.3+00 N 2.4 ,·00 N 25+00 N /6+00 N 21; 00 N 28100 N 29+0D N .30+00 N HI. ·16

1

.41 ls.5 · t

16 • 1 ~. 4 · 16.~, ~ 6.s9 ~ -, .'o l 1 i .. 1l 1

61

.38 . 6.!4 · 9 . 17~,· ::J .4 'H.1

721 7. :37 I/o 9.9?

18

1

821 9 .. 11 1

131. 7

1

21 +00 N n•OO 1\i 2.3+00 N 24+00 N /5 ·1·00 N 26+00 N '2.7 100 N 28·~00 N 29+00 N 30 +00 N ,,,/CO zo·; co •. ~800 20800 19700

1/

31 +00 N -~L I 00 N ,5j I 00 N 34+00 N 35+00 N 36+00 N I 1.3

1

• I 1 l 1 6 1

! 11

• 7 1 h. 8 1

1(;1

5 I J I . l 1

101

8 1 i 0 . l I 7

1

!1~) 1 6. 52 I 5

1

72

.11+00 N 3<1 +00 N ~ 11\0 4~30

35+00 N 1171G 4' .. 30

36+00 N 2590

.5 7·t·OO N 5/:l·f00 N f .

1

02 I 9.72 I f..1

/' ;' 4. !9

37+00 N 38+00 N 27 <1.0 .Yi70 4080 .~940

777'2

Filter Chargea bility n~ 1

0"•2 29

i 19

n- 3 15 13

n...-4 ~ 1 10

n=~ ~ 6

n =6 2

Filt~a lc u loted Resistivi n-=1

n - 4

/!l41.3 ; 17190 IH68 12517 10941 B22U l_ 749~ . '311 ?R ·

1~n

B

Pseudo Section Plot 22+00E

Dipole-Pole Array

a na a

Pant-leg Filter

., *

* * * •

' / ' / ' / ' / ' / \-<

* • plot point

Logarithf.'if Contours .5, 2, 3, 5, 7.5, 10, ...

• 0

0

50

INTERPRETATION Strong increase in polarization accompanied by marked decrease in resistiv ity.




Scale 1 :5000 0 50 100 150 200

metres

GRIFTCO CORPORATION

a=50 m




TY

Chorg&t.nli.iiYJietl Rcsist ivi;y Colcu 1otcd Rc~g¥obility

241 ??

20

1A

16

1 ~

1:.1.

10

Chargeability

I - -.---.----~--~ ---r---.--- ~-- I - ~~---r---.---~---- 1 Ohm•m :::l'l I ; • ~ I I I I I

1~000 ~ / > .... ------·~ ..... 1200 __ / ""'-- -- - .- ··- ····· ·.::.::::., , ··, ·.,, __ _ - .. - -· ------. _____ ...... --- ~ .. - ------

1()0(;()-- ./ ""-, .... __ __ ______ •• --...... , .,_ - ·· _,----···-·········"""~ / - - -··· / ·......_ _____ , ,,, -- v ::1-- -- ... ·-. ------ .. _/ "--------- ... ____________ --------- __ ;·-----~ ----... _ //··-------------------------------- ---------/··-·-------------- <----., - ,_ /~- :::::,__ --- . -.:.~--2000 _ _ L. _, _J_ . I __ . ..L_ L .. _ .J I _ I__ ---'---·'-- J .... , ___ .l, 1 .. L . J.. .1 I. .1- --- I ----'-- .._ __ __ .! __ _,_ ___ : _______ ~ _ , .. :--~---L- :21_

16+00 N 17+00 N 18t00 N 19+00 N 20+00 N Filt~r 15

1. 7 . is .2 ·2C

1.3

1 ;6~ · ,6·.7 · .h .?. ' ;' 01. 1 . 17.4 1 1/~ '

21+0DN :n1·00N 2 j•OvN 2'1 ·•·00 N 25+00N 26+00N 2/• GON 7.R+OO N 29+00N jQ+OON 3l+OON .52 t OOt\l 3:-'>+00N j~•yo ,N .• 3~+90,NI 1

3?+QO .NI 13?+QC

1N _ . 3~+90_N_ I

1, 2' 4 ' 9.96 'a .'2L. ?14 ' s .'c7 ' 5.s5 · ~ .·66 . '1.6 1

5176 .741 'g'o:,' / . 7:s ' 1o 2 ' 9.35 ' g ~ g · :i .R6 · R1

91

11.4 ·,1·_,· 9.8 ·"·~· i oil ' ,,', g ' iz.:., ' 11· . ~ · 9.Hi tdll 11.1 7.33 7 35 r.~ 6 . 2 1 7 . 65 4 .5 5.75 4 . 54 12

n-4

N 'i7·00 N : s~oo N 6770 5090 4820 9250

4 1

t>1

n - 1 ~6 1 5 yg{).1 \.."'./

6 728 1336 8391

78~0 9758

n- 6 ?0018§.-"''IIM:4-•HH 52 8649 11611/ r;;;~S....,_ 9400


f!hm•fTl 1HuUO

1€0GO

HOOO

120GO

1GOGO

8000

5000

4 000

;.'()(){)

tiitcr

n- 1

n= 2

rt=4

n=5

:>~

2:i

20

- 18

16

11

·12

10

-H

6

Chargeobility

}j 17 1~ 11 10

9 R 7 ~ ?

: ;u~alculated Resistivi Ohrn~m

n = 7 ??010

i 16168

<1 =3 '1319G 1021:)

n= 4 8501 B /19.5 6157

n= tl 1871 3395

n= 6 2002


Dipole-Pole Array

a na a

Pant-leg Filter

* *

* *

' / ' / ' / ' / ' / ~'!'

plot point

Logarithf.ip Contours .5, 2, 3, 5, 7.5, 10, ...

• D

0

50

INTERPRETATION Strong increase in polarization accompanied by marked decrease in resistivity.




Scale 1 :5000 0 150 200 250

-.r:w .W metres

GRIFTCO CORPORATION

a=50m

300


T URANIUM RARE EARTH PROPE



TY

Chor<;(~UdJ-YJtcd l~esistivity OhrrHrll

Ca cu lot('d RcSJroillf~ JI Obilily Ohm"m

:?1 - .. ,-- , .--,-- ·- ··,----, --~--.--- --~-· ... ,--~ T --, --~-- ; - - ··· I --,---r--r-~-~--r--~---r- .lQ{)Q(j

2 2

201 i8

16

14.1 12

·.r.

H

6

~.-

Chargeabi lity

10000 : ------~//-. ...... ______ • ............ _ - .. "---.. --------·-----... ________ _ _..,///~/ - --~ ____ //~-==: ...... --·--·~-~-=-~-=.:-~~~==--~=---~ \. .... ___ .. -----·--· ________ ...... ·"\ soouj ·-- ----.. -------·-- -............~--------··-·--/~ ~ ··-- ·------------------ · 'i.- - ---~,

O 1. . • I~ 1 , _ L_ I _ _ •.. 1. L - _I_. _ l _L_ . - 1 - - 1 - ~ .

riua: 8;~~ .N h .4 1 ~;29~ .N lo.2 20~29~ · N; ' .3 2 ~ ;J~ .N A. s~ 2?;~~ .N 'l .9a 2?;_~~ .N 8.74

2~;~;. IN 5.74 21:.~~ IN 9 . 7 ~ 2?;~~ .N 6 9; 2 {;?~ I ~ io. 4

2?~?~ ,N Lu 291'~~~ IN 1o.3 39~2.~ ,N ; , . ~ .5) ;~~ .N 12.; .5{;7.~~ IN 1.d

3:;~~ .N 2?. .1 J~ ;,9~ '1-J 1o.s 3?;,9~ _N

36+00 N 37+00 N e s I t o o e I o 1 1

12 12 . 1 u .7 4.ro fi .H. r. = 1 &

n-=2

.. - .)

n - IJ

n= 6

18•00 N 19;00 N 20+00 N 2i +OU N 22+00 N 24+00 N ?.5+00 N 2/+0U N 28+00 N 29~-oo N 30+00 1\ J1 ~oo N .37..+00 N .),31·00 N 36!·00 1\i 37+00 N 169CO 7950 11100 14/00 13800 7?00 8j5Q 12:)00 14200 13600 !29UO 10900 I 1.~00 6tlt>O 4270 3900 4580 18/::lO ; 4200 16300 1.3600 I 1900 11900 1 I 700 '!0600 9140

4 .)1 11-2 10967~" ~ ~H)o~·a ~019 I

f:lter 206(}() 7MOO 24300 a leu Ia ted Resistivit¥_1

10176 12983 9~ /17~ ()067 911~~ 11059 12759 i"ro~ \~ H690 1

11418 13754 ~'-0 1763 l 707

03 14365 ~0~

Ohn1• 1T1 n - 2

n-6


·25000

/ fj()()()

15000

10000

!j()(;Q

·0

I iller

n-1

2/.

20

. ~ ll

1f:i

' ~

'o /

10

0

·I>

· 4

Chargeability

7.1 1 16 14 1.5 11 10

9 8 ?. ... ::>

Fin~alculated Resist ivi

n- 4

n-5

Chm• m

265:59 I 18419 \ '1261 11988 1a266 B H848 769/ 6600 .!!.961 .

:J J':Jj


Dipole-Pole Array

a na a

Pant-leg Filter

* * * *

/ ' / ' / ' /

',t'/

* .. plot point

Logarithmic Conto~r1' 1.51 2, 3, 5, 7.5, 10, ...

•

D

0

50

INTERPRETATION Strong increase in po larization accompanied by marked decrease in resist ivity.

Well def ined increase in polarizati on without marked resistivity decrease.



Scale 1 :5000 0 50 100 1SO 200 2SO

metres

GRIFTCO CORPORATION

a = 50 m

300


Date: 22/05/201 0 Interpretation:


TY

Chargw~xiiWtl)Zitcd i~e~;i st ivity ColculotecJ Re$ltltril'f(j~obili~y Chm-..,.,

.'01 25

~::1 \0

=~

o-

Ohrn1;t· , --,- i.l:ono

· 18000

16000

;::r-- ~ , -~ ~ _; -~-· ---,- --. ---. ----, ··-.-·· .--, ·- ·---. -~ ,- · -~- ·~ -~ .. . ~~~\····-·r-~-

H U00 j I ·········- --- -·-- ·······-· . --::~::: _____ ... ·--·-- I ····-·---... _______________ -------------······-··-.,, _________ _____ /--------·-········---.. / .... ______________ -----------------·--___ ......... / \ ___ .... -··············---- ·1 0000

- .................. ,1 -- ---- - --- ------- .---··

HOGO

::1 ---------......_=-)---------... ____ - . -·-·-···--·-·--- ----·-- ·------------- ·-·-... ________________ -------------- ---- ·.:::><:.... ..... ···-----...._ j' ~~:.:~: 4 ;)(){)-' - - - - -----///__...----... ___ '-_ - ··--- 4000

2Q(1()J ... . I 1.---1... - 1 .. ---L -L-- j -'----l.. • I •• I -· . .L_,_ - ·J.. -.J.__ -- ! .... l2Q0Q

r~: 125 ·20

1/-100 N 1~+00 N 19•00 N 20•00 N 21t00 N 22+00 N 2S·•OO "l /1.·100 N /.5+00 N 16.3 12 .!:1 7 9 10.2 9.96 !1 . ?.4 8 . 38 !>.73 4 . 77 4 . 43 5.5'1 6.'1 7.14 IU:il 5.17 6.35 I. II 7 . 04

2/100 N /R+OO N 29t-DO N 3/+00 N 8.f~ 6.31 7 .89 8 . 66 7.60 9 . 42 10 . :~ 10. i '•?. 6

33 •00 N .J-1 +00 N 1~ . ? 30 .8 30 . ~ 16. ·, 18.5 10.9 22. 1 Fi1tt!J

11'!":1

Chargeobility Chorgeability

9

~~~

7 6

5~~~8 :)' ,) 7 8 H

7 _.-- R c- i 9 9 G

( - 9 H 11 --.......J 10 9 10 7

1~a e. (7 ~~ a 9 a. 9 9

,_o.qe-- - a

6

7

6

n -. fi

1 7+CO f\1 18•·00 N 19•00 N 20+00 N 71 +00 N 22 +00 N 24; 00 N / 5+00 N 26+00 N /.8-00 N :.:i~le.'

alculoted Resistivit¥- 1

4500 50..10 ~i020 498C 1530C 18.10(} 19~0:.1 15100 1.S900 13500 10100 89JO 11200 9970

Ohm•m n-2

n-.l

n-4

n- 6


9

29+00 N .30+00 N Jl •·00 N ..52 •00 N 3.)+00 N 9/10 96.30 l.i6!i0 /74{j

5845 8 J!l() 798.~

19 ~ 91/0

8471~9A.1

~ · 2

' I-!)

.38 I ~7 11 9 fl

1 6 ~ 4

r•u¥a lculated Resistivi n-1

n=- 4

n-5

n-5

on,..,.,•m

22867 ~ 15.3 71 125~.5 ~ o·i l 1 91 3\ ... 8465 - . !7!:::1 -:-)9~5 -1583 -2981

B

Pseudo Section Plot 25+00E

Dipole-Pole Array

a na a

Pant-leg Filter .. "'

* "

/ ' / ' / ' / ' / '\-

plot point

Logarithf:llf Contours .5, 2, 3, 5, 7.5, 1 0, ...

• 0

0

50

INTERPRETATION Strong increase in polarization accompanied by marked decrease in resis ti'lity.

Well defined increase in polarization without marked resistiv ity decrease.

Poorly defined polarization increase w ith no resistlvlty signature.


Scale 1:5000 0 50 100 150 200 250

metres

GRIFTCO CORPORATION

a=SOm

300


TT URANIUM RARE EARTH PROPE



TY

Documents

Geophysical Surveys Report on the Butt Uranium Rare Earth