41015SE8016 63.4731 ROLLO
010
A Brief Discussion of Terraquest's aerial E.M. Anomalies
on the 71-claim Rollo twp.i Ontario Property of
Rollo Resources Prospecting Syndicate
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Albert Hopkins Y
"Consulting Mining Geologist.
OM 35-123
In general, the most favourable type of E.M. conductor anomaly is the "Reverse
Quadrature", followed by "Normal Quadrature"* and the least indicative of metallic
mineralization is "In Phase Only". However* gold* our target* often occurs 1n very poor
conductors such as the quartz veins of the Swayze Gold Belti with only Sparse or rare
sulphides. Therefore no conductor anomaly may be considered unfavourable for gold in
this area of greenstone volcanics and Keewatin sediments, and the strongest Normal or
Reverse Quadrature anomalies may not contain the best gold mineralization.
The Rollo Resources Synd. property contains 9 EM. cOnduCtOr'anomalies, of which 3,
in my opinion, are drill targets. These three locations should be examined on the ground
for signs of mineralization and/or alteration* These 3 conductors would be easily
located on the ground by using the one-man Geonics EM. 16 equipment.
The following anomalies or EM. conductors are listed frt order from N. to S.
(see attached composite photo mosaic map of the Rollo Resources property):Anomaly "T";. ;: , Y ^: YiYY*^ .;'.;, ,
"Reverse Quadrature". 200 long on Rollo's N. boundary tt I ts NE. corner,
extending W. on dry land from the shore of Rollo lake. It Should be examined on the
surface at or near the W. shore of Rollo lake for mineralization and/or alteration, but .
it is probably of little interest at this time, in my opinion.
Anomaly K;Normal Quadrature. Only 100 long on the Rollo Resources property, under
Rollo lake, striking NE. It is thought to be of little interest at present.
Anomaly U:Reverse Quadrature. This is only 275 long, in the mid-Eastern part of the
Rollo Resources property. It is deemed to be of little Interest at this time by this
writer.
Anomaly "0":"In Phase Only", it has a length of only 70 inside the Rollo Resources
property boundary, being mainly on the Rollover Resources Synd. property. This is
thought to be of no Interest at the present by this writer. Of course, 1f significant
gold mineralization is found on this or neighbouring properties* all these minor
anomalies would then assume greater potential.
Y
Anomaly V;-
Y
. . YYY . : Y^^Y^YYY .vV.'".
.../'.'
Reverse Quadrature, This 650 long anomaly CoffiMdeS With the DestorPorcupine Fault, and might be very important. It also proves that the "D-P" Fault (itself
displaced many}times by N-S cross-faults in its 200 km. length)* extends" as farWSW.
v as Rollo lake. This anomaly is Hopkins' priority #1 Oh the Rollo Resources property.
Anomaly W:-
;Y^
Reverse Quadrature. This 350 long conductor strikes NW-SE* normal to Anomaly
"V" (the D-P Fault) in the S.-Central part of Rollo Resources' property. It should at
least be examined on the ground for signs of mineralization and/or alteration, and is
Hopkins 1 drill priority #3 for Rollo Resources.
Anomaly "X";-
YY
Reverse Quadrature. This 375m long conductor alSo Strikes NW-SE to Rollo
Resources' S. boundary. It is not of much interest at present.
Anomaly Q:-
Y*
Reverse Quadrature. This conductor begins on Rollo Resources' S. boundary,
and extends 550 ENE. to Rollover's boundary* and then on another 100 ENE. on Rollover's
property. It is Hopkins 1 drill priority #2 for Rollo Resources. It should be tested
by a joint borehole with Rollover Resources, along their common boundary.
Anomaly T ;-
y Y
;
Reverse Quadrature, Only 125mo3ohg9ehHlii Rollo Resources property*
striking NW. from Rollo Resources' N. boundary, near the propertyis"NHli corner. This
anomaly is deemed to be of little interest at the present time.
'•t-vf'
m*-:
Recap, of Hopkins' Drill Targets for Rollo Resources
Priority f
Anomaly
j^
l
W
•X",
Total:would cost
250 meters
Respectfully submitted*
TORONTO, Canada,
April 1986.
Consulting HIrtlritj Geologist,
and 105K Interest holder In the Syndicate.
900
-noisseaaie 53.4731 ROLLO
THIS SUBMITTAL CONSISTED OF VARIOUS REPORTS, SOME
OF WHICH HAVE BEEN CULLED FROM THIS FILE. THE CULLED
MATERIAL HAD BEEN PREVIOUSLY SUBMITTED UNDER THE
FOLLOWING RECORD SERIES (THE DOCUMENTS CAN BE VIEWED
IN THESE SERIES):
l)
RppoH an cur\ rt ir borne,
j V LF-E/
f-Ti
mcun o-ice
71-cMiin property ni Hoi l D Ki'smiri.es ProH.ect.uri Syndicate.
INTERPRETATION
ROLLO TOWNSHIP - ONTARIO
N.T.t NO:
•CAL!
41
0/15
1 : 10,000
DRAWING NO.
D A Tl:
February
A- 533
4
1986
TERRAQUEST LTD.
LEGEND
UTHO1OGV
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9
Contact
Diaba** dykes
Fautt
Blottte and Hornbtend-Btotrt* qu*rQ monzonite
Property Boundary
Mafic Inatruslv*
VLF-BM Conductor Axos
t
t
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f ••-.l----i
normal quadrature
3
reverse quadrature
2m
Metaaedimenta; greywacke, quartzite, slate
Magnetic units within
2
Fvtsic to intermediate metavolt anic*
In phase only (no quadrature)
j
1m
j
Magnetic unrta within
1
1
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Mafic to intermediate rrwtavolcanic*
47 54'N
6814
1002
47 5TN
74P.8
1004
ROLLOVf R RF SOURCES PHOSPECTING SYNDICA
ROI i O RF- SOURCES PROSPECTING SYNDICATE
HANSON IAKF PROSPECTING SYNDICATE
Kt NTY OPTIMISTS SYNDICATE
LEGEND
Terrain Clearance
100 mot c: r s
Line Sp;ic my
100 meters
AIRBORNE MAGNETIC SURVEY
1000 q;
TOTAL MAGNETIC FIELD
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ROLLO TOWNSHIP - ONTARIO
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DATE:
V 10,000
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February 1986
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LEGEND
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iANSON l AKf- PHOvSF'F CM INC) SYNDICA1F
Kf NIY OfMIMISIS SYNDICA
AIRBORNE MAGNETIC SURVEY
VERTICAL MAGNETIC GRADIENT
Calculated From Total Field
ROLLO TOWNSHIP - ONTARIO
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SCALE
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DRAWING NO,
DATE:
TERRAQUKW LTD.
A
F ebruary
533
1986
2
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47 54'N
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1004
HOLLOVi.R HeSOURGES FJ HOHF'EC l INCi SYNDICATE
ROl LO RESOURCFS PROSPECTING SYNDIGA'H
HANSON IAKE PROSPECTING SYNDICATE:
KENTY OPTIMISTS SYNDICATE
LEGEND
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DATE:
February
TERRAQUESTim T
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1986
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LEGEND
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K.)l i O Mr- SOURCE S PROS P CliNti SYNDICAI
1ANSON AKI PHOSFTGIINC; SYNDICAI
LITHOLOGY
INTERPRETATION
K| NIY O P
Contact
M SIS SYNDICAI
f,-i LI It
Property Boundary
H i o! 11 c- ;ui d Mom li le t id Biotite quart/ niuM/
VII LM C onductor Axes
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ROLLO TOWNSHIP - ONTARIO
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