34 MACKLEM 010 DIAMOND DRILLING TOWNSHIP: MACLEM REPORT NO:34 WORK PERFORMED FOR: Kidd Creek Mines Ltd. RECORDED HOLDER: Same as Above [xx] : Other [ ] Claim No. P 871612 P 871612 S P 871613 Hole No MC-25-1 MC-25-2 MC-25-3 Footage 384m 300m 251m Date Oct/86 Oct/86 Note (D (D Oct-Nov/86 (1) NOTES: (1) #278-87, filed in April/88.
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DIAMOND DRILLING TOWNSHIP: MACLEM WORK … MACKLEM 010 DIAMOND DRILLING TOWNSHIP: MACLEM REPORT NO:34 WORK PERFORMED FOR: Kidd Creek Mines Ltd. RECORDED HOLDER: Same as Above [xx]:
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34 MACKLEM010
DIAMOND DRILLING
TOWNSHIP: MACLEM REPORT NO:34
WORK PERFORMED FOR: Kidd Creek Mines Ltd.
RECORDED HOLDER: Same as Above [xx]: Other [ ]
Claim No.
P 871612
P 871612 S P 871613
Hole No
MC-25-1 MC-25-2
MC-25-3
Footage
384m 300m
251m
Date
Oct/86 Oct/86
Note
(D (D
Oct-Nov/86 (1)
NOTES: (1) #278-87, filed in April/88.
871612
MCS5 - Ol
MAFIC VOLCANIC
f rofne nto l
omygdo lo idol
teric i tic ol t ertd
intensely corbonotcO
KIDD CREEK MINES LTD.Explorolion Division Timmin*,ONTARIO
REMARKS MC-25-1 was drilled to follow-up gold values from MAC-85-1 and MAC-85-2, United Kingdom Energy (1985). - Casing left in hole.
Logged by Date October 28, 1986Properly
MacKlem 25
Depth
92m152m
212m272m
332m
Observed Azimuth
310NE
360NE
360NE
420NE
450NE
True Azimuth
0220
0276
0270
0330
0360
Dip
530
520
520
500
480
Hole No.MC-25-1
'f*zZi ii i ;: : ' : -;-.)-jJi:::;i .'t ti.'Wvj&X-'* 3'W
FROM - TO
g
35.0
v;.n
87.1
J
DESCRIPTION
OVFRRIJRDEN
MAFIC FRAGMENTAL
- fine grained, light green to dark greenish-black- 3 fragment types observed; i) 905! fragments are a distinct pale green,
fine grained, amygdaloidal and exhibit sharp contacts. Vary In sizefrom 1X2 cm, up to 20 cm li) 81 of fragments are highly amygdaloidal,up to 302! iii) 2 1 variolitic fragments. Subround coeleslng pale greenspots l-2mm
- 10* of unit is distinct fragments, recognition of other fragmentsis obscurred by alteration
- very strongly foliated at 350 to core axisALTERATION:
- moderate pervasive carbonate and 5-105! carbonate dumping in Irregularmasses from 0.5cm to 2cm in width.
- moderate pervasive chlorite throughout, 0.5mm to 5mm strongly chlori tic blebs elongated in plane of foliation occur locally.
- Sericite occurs locally varying in intensity from wispy streaks onfoliation planes to strongly pervasive zones
MINERALIZATION:- I t pyrite occurs locally, associated mainly with quartz/carbonate
veins and masses. Pyrite also occurs along foliation planes.VEINING:- minor quartz/carbonate veins averaging lcm occur in two general
orientations; i) 350-50U to core axis perpendicular to foliation( ii) 35U to core axis parallel to foliation
SAMPLE NO FROM TO
SAMPL LENOT
ASSAYS
LOGGED BY: J- K - Cecchetto DATE: Oc t 28/86 PROPERT.flacK1ein 25 HOLE NOMC-25-l PAGE NO 1
fci^i^ii-i^
FROM - TO
u
DESCRIPTION
- irregular shaped quartz/carbonate patches occur locally, approximately5-10* of unit
- thin 1mm carbonate veinlets sub-parallel to core axis occur locally- 35.0 - 36.5: weak sericite, moderate carbonate dumping- 36.5 - 38.0: as above, 53! lcm quartz/carbonate veins- 38.0 - 39.5: as above, strongly foliated- 39.5 - 41.0: as above
- 41.0 - 42.5: as above- 42.5 - 44.0: as above- 44.5 - 45.3: mafic dike?- very fine grained , spotty chlorite, 5* - ,5-lmm euhedral
carbonate grains. Very weakly foliated- 45.8 - 48.5: mafic dike?
- very fine qrained, 5 1 - \-2im euhedral fractured controlled carbonategrains. 1 /21 pyrite
MAFIC VOLCANIC- fine grained, dark green to greenish-black- no observable fragments, although some may be obscured due to alteration- unit is variable and is likely made up of a series of similar flows- local variolitic patches occur between 103.7 - 172.5, < 2% of interval- carbonate amygdules occur throughout varying in density from < 4% to*30J!,
range in size from Imm-lOmm, are round to Irregular in shape and are gene rally elongated inthe plane of foliation
- pillow selveges are distinct locally between 178.0 - 182.0 and 276.0 -299.9. Possibly pillowed from 233.4 - 276.0
- where unit is distinctly pillowed selveges are 0.5m apart and 5-10cm wide,pillowyare amygdaloidal
- unit moderately to strongly foliated generally at 35 to core axis, butranges from 2b -45P to core axis
ALTERATION:- weak pervasive carbonate, locally moderate- carbonate dumping occurs throughout fronx2Z to 3011,- 1 mm wide crenulated carbonate veinlets , 0,5 - lcm apart and sub-paralle
- 2 general orientations are dominant; 1) 85* sub-parallel to foliation, 25to 450 to core axis 11) 153S 350-550 to core axis perpendicular to foliationThis group commonly cro^cn*-* thp first group.
- Crenulated carbonate veinlets are generally sub-parallel to core axis butmay assume any orientation.
- 5-105S quartz/carbonate masses occur throughout reaching 401 locally.Increased amounts are noticed in the highly sericitic zones
- 88.5 - 90.0: 52!*lcm quartz/carbonate veins
- 90.0 - 91.5: as above- 91.5 - 93.0: as above- 93.0 - 94.5: as above- 94.5 - 96.0: as above
- 96.0 - 97.5: as above
SAMPLE NO.
AD
5592
5593
5594
5595
5596
5597
FROM TO
m
88.5
90.0
91.5
93.0
94.5
96.0
90.0
91.5
93.0
94.5
96.0
97.5
SAMPL LENGT
1.5
1.5
1.5
1.5
1.5
i;s
ASSAYS
AuDDb
3
2
3
10
8
6LOGGED BY: j. K. Cecchetto DATE: Oc t 28/86 PROPERTY MacKlem 25 HOLE NO. ffc-25-1 PAGE NO.5
- sericite alteration zone from 305.0 - 314.0- zone is strongly seriticized and strongly foliated at 25-350 to core axis- quartz/carbonate masses up to 503!, with quartz dominant- original textures and structure completely obscured- n pyrite throughout as blebs in quartz and l-2mm crystals on foliation plane
FINISH ..PP.t. 27/86 . Grid Location: Latitude ..8.!991...... UTM: Lat. ??8.5??..... Surveyed: Let. .......... Mine Grid: Lat.
Departure .. A*.7.5.5..... Dep. 5367870.... Dep.
Elevation
COLLAR ATTITUDE Azimuth...2.^...... Dip-50
INCLINATION TESTS Rotodip/Acid Tests
Depth
297m
Dip
-400
LENGTH
Depth
CORE SIZE B
Compass Tests
Dip Depth
62m
116m
176tn
236m
Observed Azimuth
320SW
340SW
350SW
True Azimuth
2030
2050
2060
2090
Dip
-520
-500
-490
-450
REMARKS : MC-25-2 was drilled totest extension of gold bearing zone encountered by United Kingdom Energy in hole MAC-85-1, -2. - casing left in hole
togged by Date. 3/86 Property ...Ma?Klem 25 .
.ji^f^r^^i!';!^l;'i'S(i!S^ J'
FROM - TO
0
47.3
47.3
246.0
tj
DESCRIPTION
OVERBURDEN
MAFIC VOLCANIC
- fine grained, colour ranges from light green to greenish-black- unit is generally amygdaloidal fronx29! to 51 throughout. Amygdules
are carbonate filled and average between 2mm - 8mm, they are Irregularto round in shape and are locally stretched in plane of foliation
- 47.3 - 64.4: appears to be void of amygdules, other sections in unitthat are amygdule void total < 5%. Three distinct, amygdaloidal sectionsoccur; i) 165.3 - 178.5: 15* subround amygdules from lm-5mm in sizeii) 185.8 - 201.8.^5* to^O* amygdules, 802 of interval has 20*amygdules iii) 236 - 246.0; 15-20* amygdules, 2-15mm in size
- distinct pillowswere not observed In this hole although one sectionbetween 171.0 - 201.8 has some pillow selvage looking features - Thisand other areas may exhibit pillow structures but are now obscured dueto alteration
- no apparent variolitic sections were observed- foliation ranges from moderate to strong dominantly at 350 to core axis,
however ranges from 250 to 450 to core axisALTERATION:
- weak to moderate pervasive carbonate. Carbonate dumping in irregularpatches generally 5-102, carbonate has a distinct purple-red stainingf hematite) throughout, however white carbonate is also present to alesser degree (approximately 70/30).
SAMPLE NO. FROM TO
SAMPL LENQT
j ASSAYS
LOGGED BY: J. K. Cecchetto DATE: NOV 4/86 PROPERTY MacKlem 25 HOLE NO. M0 '25 '2 PAGE NO. 1
8*31*
;:^:.;.^^
FROM - TO
-d
DESCRIPTION
- moderate pervasive chlorite and strongly chloritic blebs occurthroughout, blebs range in size from 0.5mm - 5mm can be subroundto highly angular and are commonly elongated in the plane offoliation.
- blebs compose up to 15-202 of the rock but average 1 01, they arehighlighted when the ground-mass is sericite
- weak sericite occurs locally throughout reaching levels of moderateto strong alteration insome instances
- weak to moderate hematization (7) occurs locally causing abrick-red colour to the rock.
MINERALIZATION:- mineralization is very minimal on the whole and generally reaches;
concentration of 13! or less.- pyrite is by far the most common sulphide, forming in fine
disseminations or as cubes from 1mm to 5mm is size. Very minoramounts of chalcopyrite and arsenopyrite exist locally. Thedisseminated mineralization commonly occurs at or near the interfaceof quartz and/or carbonate with the host rock as blebs ordisseminations along foliation planes. One Quartz/carbonate vein;contained 52 sulphides composed of pyrite, chalcopyrite, shalerite.and pyrrhotite
VEINING:- three types of veining occur; i) carbonate veins, general ly*:lX2cm
wide, range from 1mm - 4cm. Various orientations, but dominantly
SAMPLE NO.
AD
FROM TO
m
SAMPL LENGT
ASSAYS
Auppb
LOGGED BY: J. K. Cecchetto DATE: No V 4/86 PROPERTY MacKl em 25 HOLE NO. HC-25-2 PAGE NO. 2
FROM - TO
^ MBMIL-J
DESCRIPTION
conformable to foliation. 11) quartz/carbonate veins, the percen tage of each varies from vein to vein, range In size from lcm-5cm.Quartz/carbonate occurs also in stockworks and patches with irregu lar contacts to host rock. 111) quartz veins, range in size from1 cm to 50 cm, commonly exhibit sharp contacts
quartz/carbonate carbonate veins^quartz veins
- veins can exhibit any orientation the most common ones being;i) 30-450 to core axis parallel to foliation. 11) 35-500perpendicular to foliation
eLOGGED BY: J- K - Cecchetto DATE: Nov 4/86 PROPERTY MacKlem 25 HOLE NO. MC-25-2 PAGE NO. 3
^^ 'i -x' •?S. - .6*:"\''V-
FROM - TO
~*
DESCRIPTION
- 91.0 - 92.5: 10X carbonate dumping
- 96.0 - 97.5^53! carbonate dumping
- 107.5 - 115.0: sericite alteration zone- weak to moderate seritization, most intense from 109.0 - 110.0yellowngreen to light green in colour, in fringes occurs aspatchy zones. IX pyrite locally.fine grained.
- 106.5 - 108.0: weak to moderate sericite, 5S quartz/carbonatedumping
LOGGED BY: J. K. Cecchetto DATE: Nov 4/86 PROPERTY MacKlem 25 HOLE NO. Mc-25-2 PAGE NO. 4
w ^ t,^i^ai,^:;4,*.:..5:iH;i;:!ffi! ; .^^^
l
FROM - TO
^ V*WmWJfc
DESCRIPTION
- 137.8 - 138.4. 140.0 - 141.3. 141.5 - 142.3: Intervals of bleathina- bleached zones with a aranular texture comoosed of l-2mm white
ish flecks and dark chloritic flecks. At the contacts withunbleached rock the granular texture is less developed. Thecommon large chloritic blebs and carbonate amygdules areabsent in these zones.
- The zones may represent alteration or an interfingering intrusiveevent.
The sericitic patches are separated by fine grained, greenishblack rock, specked with very fine yellow carbonate. Thesericitic patches commonly exhibit sharp contacts with the ;;other rock.
- 204.0 - 205.5: moderate to strong sericite, 10* quartz/carbonatedumping
- 205.5 - 208.0: weak to moderate sericite- 214.5 - 216.0: as above
- 216.0 - 217.5: as above, ^121 chalcopyrite- 217.5 - 219.0: weak to moderate sericite, 1/2* pyrite
- 213 - 236: sericite alteration zone- weak to moderately sericitic, moderately foliated at 400 to
core axis, ^2 amygdules, moderate pervasive chlorite,chloritic blebs, generally < 5% veining and dumping
- 219.0 - 220.5: weak to moderate sericite. < IX ovrlte crystals- 225.0 - 226.5: weak to moderate sericite- 231.0 - 232.0: as above, 15 cm quartz/carbonate vein with 5*
LOGGED BY: J. K. Cecchetto DATE: Nov 4/86 PROPERTY MacKlem 25 HOLE NO. Mc-25-2 PAGE NO. 6
..^^••i:^-'^.^
FROM - TO
246.0
266
266.0
300
-*
DESCRIPTION
MAFIC FRAGMENTAL
- black chloritic bands mixed with light green patrhec- moderate to strong pervasive carbonate, weak sericite.- common fragment types are ; 1) vellow-areen amvadaloidal with rhlnHtl
blebs ii) amygdaloidal fragments with varying amounts and sizes ofamygdules
- other fragment looking shadows occur but are obscured by alteration.Fragments range in size from 1 to 10cm.
- < l% pyrite crystal occur locally- moderate foliation ranginq from 35-500 to core a*1s.- 5% quartz/carbonate veining and dumping. Veins are cfflmonlv 0.5cm
wide ranging from 20-500 to core axis perpendicular to foliation
- 249.0 - 250.0:*2* quartz/carbonate veining and dumping- 250.5 - 252.0: as above, *UX pyrite crystals
MAFIC VOLCANIC
- fine grained, light greenish-yellow to green-black- pervasive carbonate ranges from weak to moderate- pervasive chlorite from weak to moderate- quartz/carbonate dumping from S-10%- generally weakly sericitic and*:lX finely disseminated pyrite though- 270.0 - 273.0, 282.0 - 287.0: unit is moderately sericitic
SAMPLE NO.
AD
204
205206
FROM TO
m
-240.5 .
249.0
250.5
4&A —
250.5
252.0
SAMPL LENQT
4rS
1.5
1.5
ASSAYS
AuPPb
4n
8
5
LOGGED BY: J- K. Cecchetto DATE: Nov 4/86 PROPERTY MacKlem 25 HOLE NO. Mc-25-2PAGE NO. 7
FROM - TO
-
300
~*
DESCRIPTION
-261.0-262.5: moderate sericite- ?6?.S - 264.0: as above- 265.5 - 267.0: as above, 8 cm quartz/carbonate vein- 270.0 - 271.5: moderate sericite- 271.5 - 273.0: as above, -;1X2J! pyrite- 273.0 - 274.5: as above- 2 74.5 - 276.0: as above, 5X quartz/carbonate dumping
REMARKS Drilled to test if a gold-bearing structure found In previousdiamond drilling (United Kingdom Energy, 1985} continued along strike. Casing left in hole
Logged by Date NP.X?^.1? ?P.'. ??.8.6, Property ..MacKlem 25.
Dep.
Elev.
Depth
154m214m
Observed Azimuth
030"NE
034"NE
True Azimuth
021U
025U
Dip
-57-55U
^^
FROM - TO
0
85.0
125.0
85.0
125.0
131.0
b*
DESCRIPTION
OVERBURDEN
REGOLITH (?)
Extremely weathered rock, may be composed of boulders and/or overburdenbut hard to determine due to extreme weathering. Becomes increasinglyconsolidate and rock-like downhole.- 20-302 lost core.
MAFIC VOLCANIC
- fine grained, light green to dark green- unit is usually amygdaloidal, generally ranges from 2 -101 amygdules
with an average of 5*. Amygdules range in sizes from 2-5mm andare subround to elongate.125.0 - 131.0: amygdules are larger than average (1.5cm) are subroundcarbonate filled and rimmed by hematite (?).
- pillow selvages are not evident, however some questionable featuresoccur locally and in places the unit may be pillowed
- foliation ranges from weak to moderate, dominantly moderate, at 30-401to core axis
- 125.0 127.4: moderate hematization occurs in patches giving the roclc abrick-red colour. Hematite (?) also is found colouring carbonatethroughout the hole.Veining:
- minor veining occurs throughout from 2-5!6, three types occur; i) carbonateveins - most irregular of the veins types in nature, from 1mm to 10mm.Multiple orientations with no distinct patterns. Also occur as 1mm widecrenulated veinlets spaced 0.5 - lcm apart ii) quartz/carbonate veins -various orientations. Commonly 0.5 - lcm wide iii) quartz veins - generalllargest in size (2-5cm) although they are the least commonMineralization:
- pyrite and minor amounts of chalcopyrite occur locally from 1/21 to IXmaximum. Pyrite occurs as blebs and disseminations generally foundassociated with quartz and/or carbonate and along foliation plane butcan also be found in groundmass with no obvious structural control.
MAFIC FRAGMENTAL (?)- unit appears compositional y the same as unit from 125.0 to 131.0. but
appears fragmental . Fragments are not highly distinctive and the appearammay be due to alteration. Fragments are the same composition and the unitmay represent a flow top or flow bottom breccia.
- moderate to strongly foliated at 300 to core axis1 - alteration and veininq are the same as 125.0 to 131. 0 T hnw*wv cnmo
SAMPLE NO.
AD
5221
5222
5223
FROM TO
m
125.0
126.5
128.0
126.5
128.0
129.0
SAMPL LENGT
. ..
1.5
1.5
1.0
ASSAYS
Auppb
25
6
13
LOGGED BY: J. K. Cecchetto DATE: November 10, 1986 PROPERTY Mac K1 em 25 HOLE NO. MC-25-03 PAGE NO. 2
FROM - TO
138.0
195,0
195.0
215.0
tn
, . , -.. —— . —————————————————DESCRIPTION
fraqments are weak to moderately sericitic
- 134.0 - 135.5: moderate sericite, 10cm quartz vein at 450 to core axisperpendicular to foliation. No observed sulphides.
MAFIC FRAGMENTA! f?)- highly amvadaloidal- very stronqly foliated at 35 to core axis- up to 201, amyqdules, irregular shaped and elongated stronalv 1n the Plane
f O f foliation AmvgHillp S17P anrf fkmtitj/ i/ariot rjreaJ-Jy p^tch piay — . _
SAMPLE NO.
AD
5224
52Zb
52265227522852295230523152325233
5214-
FROM —— TO
m
134.0
WT.F-143.0149.0150.5153,5156.5170.0173.0186.5
T94.0
135.5
"14370"
144.5150.5152.0155.6158.0171.5174.5188.0
TOTIT
SAMPL LENGT
1.5
"TT5~
1.51.51.51.51.51.51.51.5
r.Q
j ASSAYSAuppb
22
~20j
385
358
1253
3
LOGGED BY: J. K. Cecchetto ^ATE: Nov. 10/86 PROPERTY MacKlem 25 HOLE NO. MC-25-03 PAGE NO. 3
FROM - TO
215.0.
251.0
u
DESCRIPTION
represent various fragments.-. two fragments exhibit verv sharp contacts at 205. O r the fragments are 5cm
and 8cm in size.- alteration is generally the same as unit from 125.0 - 131.0, although
carbonate dumping is more intense at 15-202- this unit is only distinctly (?) fragmental at 205.0m. The high percen
tage of amygdules and carbonate dumping and the intensity of foliationdecreases towards 195.0 and 215.0. Some of the Interpreted amygdulesmay actually be secondary carbonate masses.
- 12 pyrite locally
203.0 - 204.5: strong foliation1 , 105! carbonate dumping204.5 - 206.0: as above206.0 - 207.5: as above, 2-5cm quartz/carbonate veins
MAFIC VOLCANIC- same as unit described from 125.0 to 131.0- unit may be pillowed locally, faint selvage - like features appear throu
ghout although they may be the results of alteration- a yellow-green mineral occurs at 241.1 - 241.2, 242.8 - 242.9 and 246.2 -246.3 which does not appear to be epidote or sericite