* 31CMSWM31 63.2092 MADOC010

6 3-

Report on a Magnetometer Survey

of the Sager Claims, Madoc Township, Ont..

By Roy V. Beavon

I .INTRODUCTION

The Sager property lies five miles north of the village of Madoc via Rural Roflte 2. It may also be reached by the Hunt Club Road which tfoins "the north side of Highway No, 7 about 1-| miles east of the village. The property consists of five unpatented claims designated E.O. 107 - 109 inclusive and E.O. 33111 - 33112.

The mineral rights of these claims are held by Earl Sager of R.R. 2, Madoc, and are currently under option to Syngenore Explorations Ltd., of Suite 1500, 2 St. Glair Avenue West, Toronto. The field work was executed by the writer on January 9-11, 1967.

II METHOD

The survey was carried out with a battery power ed, direct reading, Nuclear Precession Magnetometer Model GM 102A, which has a sensitivity of 10 gammas. The total

magnetic field was measured and checfied by the same instru ment at three base stations at three times per day.

, i

III RESJJLTS

The results of the survey are shown graphically on the accompanying map. One linear anomaly (B) was encountered trending north-westwards in the eastern part of Claim E.O. 33112. A second linear anomaly trends north-eastwards in the southern part of Claim E.O. 33107, (C).

IV CeNCLUSIjOJNS

Exploration to date has included a geological,

an electromagnetic, and a magnetic survey. Anomaly 'B 1 ,which occurs in inetavolcanic greenstones, is also a moderate

conductor, and it appears from the profiles to be ' dipping

te' pr

KEY MAP A- 31680

SAGER BROS. CLAIMS

MADOC TOWNSHI P

Cone.XI

Q.

X

o:

>UJN -J

UJ

Owners of property mineral rights

Earl S ager

Gordon Sager

R.R.2 M ADOC

fc*.

steeply towards the south-west. According to Mr Sager this same zone was drilled by him to the east of the lines employed by the present survey. Disseminated pyrrhotite and pyrite were said to be present.

As a result of the work completed to date no further encouragement has been received, an no further work is atpresent contemplated.

Roy V. Beavon Geologist

for Synge n ore Explorat i ons.

31CUSWee31 63.2892 MADOC 020

Report on E.M. Survey of the

SAGER CLAIMS, Madoc Township, Ontario.

By; Roy V. Beavon

I INTRODUCTION;

The Sager property lies five miles north of the

village of Madoc via Rural Route 2. It may also be reached

via the Hunt Club Road which joins the north side of Highway

No. 7 about Ify miles east of the village. The property consists

of the five unpatented claims which are tabulated as follows:

Claim No. Concession Lot

E.G.33107 X EJ4 - 12

E.0.33108 X NEi* - 13

E.0.33109 X SEJ* - 13

E.0.33111 XI W)4 - 12

E.0.33112 XI W)4 - 13

The mineral rights of these claims, which are

held by Earl Sager and Gordon Sager of R.R.#2, Madoc, are

currently under option to Syngenore Explorations Limited of

Suite 1500, 2 St. Glair Avenue West, Toronto, which company

directed the work described in this report. The field work

was contracted to Moreau-Woodard 8. Company during December

1966. The following details were supplied by Mr. F. Scott

of Moreau-Woodard S, Co.

II METHOD:The survey was carried out with a modified

minigun, manufactured in Sweden by ABEM. The receiver employs

a ferrite coil and the transmitter was air cored with a battery

driven ascillator. The receiver measures the in-phase and

- 2 -

out-of-phase components of the vertical secondary field and

these are expressed in percentages of the 'normal 1 field for

the coil separation used.

The relative amplitudes of the in-phase and

out-of-phase readings may be used to approximate conductivity

and depth of an indicated anomaly* The coil spacing used was

200 feet and the frequency was 3.52 Kilocycles.

III RESULTS;

Two conductors were located which could represent

sulphides in the bedrock. These are designated by the letter

A 1 and 'B 1 on the geophysical plan.

Conductor *A*The ratios shown at this location are in the range

expected from weakly conductive overburden. However, the agree

ment with the strike direction of 'B 1 indicates the possibility

of a bedrock source.

Conductor !B !

The positive readings noted at the east end of

Line 46N show that this zone extends to the south east beyond

the limits of the grid. Although conductivities are below the

massive sulphide range, a definite bedrock source is indicated.

IV CONCLUSION;

Further work will depend on an appraisal of the

result of all methods used to date.

RVB/k Roy V. Beavon. January 25, 1967.

31CI1SWee31 63.2*92 MADOC 030

Report on the Geology of the

SAGER CLAIMS, Madoc Township, Ontario.

By Roy V. Beavon.

I INTRODUCTION;

The Sager property lies five miles north ,of the

village of Madoc via Rural Route 2. It may also be reached

via the Hunt Club Road which joins the north side of Highway

No.7 about lJ^ miles east of the village. The property consists

of the five unpatented claims which are tabulated as follows:

Claim No. Concession Lot

E.G.33107 X EJ* - 12

E.0.33108 X NEJ4 - 13

E.0.33109 X SE)* - 13

E.0.33111 XI W)* - 12

E.0.33112 XI W)4 - 13

The mineral rights of these claims, which are

held by Earl Sager and Gordon Sager of R.R.#2, Madoc, are

currently under option to Syngenore Explorations Limited

of Suite 1500, 2 St. Clair Avenue West, Toronto, which company

directed the geological work described in this report. The

field work was performed by the writer during the period

July 4th to July 8th, 1966.

II TABLE OF FORMATIONS;

At least four rock types underly the six claims

of the Sager property, and in view of the faulted nature of the

ground it is unlikely that the following table of strata

represents a continuous stratigraphic sequence:

. 2 -

(4) Limestones

(3) Dolomites

(2) Siltstones

(1) Amphibolites

These metasedimentary and metavolcanic rocks

belong to the Pre-Cambrian basement of Southern Ontario.

(1) The amphibolites form the bedrock of the eastern part

of the property. They are massive, foliated, coarse to fine

grained amphibolites, and banded hornblendic schists. The

foliated or banded types are by far the most abundant rock type

of these metavolcanics.

Black acicular hornblende or actinolite forms

the most conspicuous mineral of the amphibolites, occurring in

decussate sheafs with little evidence of preferred orientation.

Similar textures are evident in the foliated types and in the

hornblende schists, where they suggest post-kinematic meta

morphism.

The hornblendic schist has only been observed

at the western border of claim E.O. 33111. It is regarded by

the writer as a tectonic unit of no stratigraphic significance.

There is some evidence that hornblende has been

destroyed by late retrogressive or dynamic metamorphism adjacent

to the regional fault in claim No. E.O. 33107. The greenstone

is here strongly carbonated. Garnet and epidote are only rarely

seen in the amphibolites.

- 3 -

Primary volcanic structures are also rare, but

some well preserved amygdales can be seen in claim No. E.O.

33112, immediately to the west of the small pit containing

a narrow rust zone in phyllitic schist (see map). While no

pillows or pillow rims were observed, they are not completely

absent from the area further south.

The metamorphic banding of the amphibolites dips

steeply (60 0 to 80 0 ) south-westwards in all of the foliated

outcrops examined.

(2) Siltstones are present in the southern part of the

claims in the form of fine-grained thin to medium bedded pink

and grey sediments. Graded bedding is weakly developed* but

its facing is of little significance in view of the fact that

it is probably located in a fault lens, i.e. in the south part

of claim No. 33111 the beds appear to be overturned.

(3) Dolomites are restricted to the north-western part of

claim No. 33108. It is a light grey to buff, massive formation

showing abundant quartz veining, and variations in dip and

strike.

(4) The limestones form the western border of the claims.

They are thin bedded, fine grained, blue, grey and black

carbonates with occasional impure siliceous beds containing

moderate biotite.

Minor structures such as folds are fairly common

in these thin-bedded rocks, but cleavage has been obliterated

- 4 -

in many places by recrystallization. The minor folds usually

plunge south-east or south with a variable dip that suggests

more than one episode of folding.

III STRUCTURE;

The Sager claims straddle a regional north

west striking fault of considerable but unknown magnitude,

as shown by the fact that all of the metasedimentary formations

are brought into contact with the amphibolites. The dip of the

main fault has not been determined.

Apart from the minor folding of the limestones

there is little information on the major structure in the small

area covered by the six claims.

IV SUMMARY OF EXPLORATION TO DATE;

Syngenore's exploration has so far been as follows:

Phase l Geological mapping on 200' scale photographs.

Phase 2 Electromagnetic Survey (December, 1966)

Phase 3 Magnetic Survey (January 9 - 11, 1967)

No detailed study has been made of the narrow

quartz veins which were prospected in the early part of this

century.

V CONCLUSION;

Further work will depend on an appraisal of the

result of all methods used to date.

RVB/k Roy V. Beavon. January 25, 1967.

JL

CONCESSION XI

Lot 13

CONCESSION

E. O. 33108E.O. 33112

E.O. 33109

TOTAL MAGNETIC FIELD

59,000 g.

C. ---- 58,000 g

Only the three middle

digits are shown on '

this mop. eg. (5)875(0).

E.O- 33111

L.

KEY MAP h 31680

SAGER BROS. CLAIMS

MADOC TWP.

Cone. X

"i ^

Lot 13

Lot 12

\ ^

Ast.fJ.

1

f C one XI

i - ~ -

*

CL

1-

or

LU

LU

Lot 12

MAGNETOMETER SURVEY

of theSAG E R

MADOC

CLAIMS

TOW N S H l P

Surveyed wi'th Nuclear Precession Magnetometer

Sensitivity 10 gamma.

SCALE OF MAP l" ^ ZOO*

l

31C11SW0031 63.2892 MADOC 200

CONCESSION X

ot 1 3

CONCESSION X

E.G. 33109

N-PHASE READINGS ...LEFT

OUT-OF-PHASE

ALL READINGS '/0 of normalcalibrated to zero

^ ^ MODERATE CONDUCTOR

INDEFINITE CONDUCTOR

FREQUENCY 3520 c ps.

COIL SEPARATION - 200 feet . . lot 12

MINIGUN ELECTROMAGNETIC SURVEY

by

MOREAU , WOODARD S Co. Ltd

for S YN G EN ORE EXPLORATIONS LTD

SAGER OPTION

Madoc Townshi p

SCALE l INCH

Ontario

200ft. DRAWN i R.VB- JAN. 1967

SURVEYED 14 - 16 D EC. I 96G OWNERS - SAGER BROS., R.R.2 MADOC.

31C1ISKW31 63.2092 MADOC 210

To QueensboroR.R.a MADOC

SANDalders

E. O. 33 1 08 aiders '

marsh

E.O- 33112

SANDFINE SAND

cultivated

a l d e r s marsh i

H quartz

o l d e r s

rusty zone phyl l it ic

garnets' \E.O. 33 109

open parklandcedar ' SAND

c u 11 i v o t e d

pine 3h o r d w o o

E.G. 33! l lE. O. 33I07a l d e. r s

L E G E N D

hornblende

Strike of b eddingFINE

carbonated zone

cultivatedDip S strike of bedding

5 A N D

c u t t i v a t e d FINE SAND

PRECAMBRIAN

METASEDIMENTS

- Limestones

- Dolomi tes

4. - S i Itstones

Dip S strike of meta morphic f oliation.

M ETAVOLCANICS

a. Amphi bol i tePlunge of minor folds

N Ast.

::"Y jraded beds

Pit

CLAIM BOUNDARY

o

SCALE IN FEET

500 IOOO

Trench

Py Pyrite

KEY MAP l- 31680

SAGER BROS. CLAIMS

MADOC TOWNSHI P

Cone. X ' Cone.XI

CL

xCO

ot-

cc

LU Kl-J

LJ

Owners of property .mineral rights

Earl S age r

Gordon Sager

R-R.2 M ADOC

SYNGENORE EXPLORATIONS LIMITEDGEOLOGICAL MAP

SAGER OPTION

MADOC TOWNSHIP, ONTARIO.

Scale -- l inch = 200feet

\;

l

Geology by : R.V-Beovon 8.Se., Ph.D.

Drawn by; R, V. B.

Dato : Dec. 2 7 1 966

3IC11SWCa3) 6 3.2*92 M ADOC