Report on Assessment Work Completed on the Cote-Two Rivers Property Thunder Bay Mining Division Beardmore Area, Ontario Mining Claims # 4229899, 4229900, 4230111, 4230113, 4222399, 4213482, 4228014, 4213507, 4229176, 4229835, 4222391, 4227926, 3008675, 4229184 & 4229178 Prepared by R. Therriault, M.Sc. on behalf of Sage Gold Inc. Prepared for The Ministry of Northern Development and Mines 3 rd Floor, 933 Ramsey Lake Road Sudbury, Ontario P3E-6B5 T: 1 -888-415-9845 April 11, 2009
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Report on Assessment Work Completed on the Cote …...Quartz veins range in texture from saccharoidal to drusy and contain variable amounts of coarse calcite, pyrite, pyrrhotite, chalcopyrite,
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Report on Assessment Work Completed on the Cote-Two Rivers Property Thunder Bay Mining Division
Prepared by R. Therriault, M.Sc. on behalf of Sage Gold Inc.
Prepared for The Ministry of Northern Development and Mines
3rd Floor, 933 Ramsey Lake Road Sudbury, Ontario
P3E-6B5 T: 1 -888-415-9845
April 11, 2009
TABLE of CONTENTS PAGE
SUMMARY 1
PURPOSE of WORK 1
LOCATION, ACCESS & TOPOGRAPHY 1
PREVIOUS WORK 2
GEOLOGY
Regional 2
Local 3
2008 WORK COMPLETED 4
INTERPRETATION & RECOMMENDATIONS 6
REFERENCES 7
FIGURES PAGE
Figure 1: Location of Property 8
Figure 2: 2008 sample locations and zinc (%) values 9
Figure 3: Property geology and 2008 gold (g/t) values 10
Figure 4: Cote – Two Rivers 1A Sampling and Geology 11
Figure 5: Cote – Two Rivers 1B Sampling and Geology 12
Figure 6: Cote – Two Rivers 2A Sampling and Geology 13
Figure 7: Cote – Two Rivers 2B Sampling and Geology 14
Figure 8: Cote – Two Rivers 3 Sampling and Geology 15
i
TABLES PAGE
Table 1: Property claims status 3
Table 2: 2008 prospecting assay highlights 5
Table 3: 2008 stripping assay results 6
APPENDICES
APPENDIX A – 2008 Cost summary AT END
APPENDIX B – 2008 Assay certificates AT END
APPENDIX C – 2008 Sample locations AT END
APPENDIX D – 2008 Work logs AT END
ii
SUMMARY
This report is submitted as a summary of work completed on the Sage Gold Ltd. controlled claims as outlined in Table 1 (the Property) located in the Thunder Bay Mining Division of Northwestern Ontario. The work completed on the Property between June 13 and August 15 of 2008 included reconnaissance-scale prospecting, overburden stripping at 5 locations on the Property and grab sampling of these stripped areas. Base and precious metal mineralization occurs within recrystallized drusy quartz-sulphide veins, sheared pyritiferous interflow iron formation/argillite and sulphidized chlorite retrograded amphibolites after mafic volcanic rocks. The primary sulphides consist of pyrite, pyrrhotite and minor sphalerite, chalcopyrite and galena.
Two new mineralization zones were discovered during the prospecting program. A grab sample from the DR1 showing yielded 2.98 g/t Au, 26.69 g/t Ag and 3.11% Cu while a grab sample from the DR2 showing produced 1.25 g/t Au, 840 g/t Ag and 1.71% Pb. Results from the stripping program were discouraging; however, several of the samples did yield anomalous levels of Au, Ag and Zn.
Given the favourable geology and assay results from DR1 and DR2, additional prospecting and sampling is recommended at and along strike with the mineralized systems. No additional work is recommended at the stripped locations at this time.
PURPOSE of WORK
The work completed on the Property was intended to locate new zones of mineralization along strike with existing zones reporting anomalous base and precious metal values that are situated along coincident geophysical anomalies. The primary target of the 2008 survey consisted of: a) iron formation hosted gold and spatially associated precious-base metal quartz-sulphide veins; b) structurally controlled quartz-sulphide precious-base metal veins.
LOCATION, ACCESS & TOPOGRAPHY
The Property is located in the Thunder Bay Mining Division in Northwestern Ontario. It is situated approximately 40 km north of Jellicoe, a small village located between Geraldton and Beardmore on Highway 17 (Figure 1). The Property is accessible via the Kinghorn Road and various logging roads which emanate west of the Kinghorn Road at approximately Kilometre 60.
Outcrop on the Property generally constitutes <5%. Overburden ranges from fine grained glaciolacustrine material to coarse grained glaciofluvial material and can be up to 10 m thick. The topography consists of moderate ridges and valleys that trend in a northeast-southwest direction. The valleys typically correspond to northeast trending lakes and drainage systems.
1
PREVIOUS WORK
A brief history of exploration on and adjacent to the Property is outlined below.
In 1951 an electromagnetic survey was carried out in the north-central part of the Property by McPhar Geophysics Ltd. The results were a number of east dipping southwest trending anomalies. A drilling program was recommended by the report’s author (AFRI #42L035SW0028).
Seven diamond drillholes were completed near Cote 2A/B by M. Church in 1961. Results of the drilling were not available to the author (AFRI #42L03SW0049).
In 1984 a geological mapping, soil & rock sampling program was carried out by Kerr Addison Mines Ltd. The program took place on an east-west trending block of claims with Conglomerate Lake toward the eastern boundary of the surveyed area. The results of both soil and rock sampling were discouraging and no further work was recommended by the report’s author (AFRI #42E13NE0038).
In 1990 a stripping, sampling and prospecting program was carried out on the southwest part of the Property by local prospectors. The program focused on a continuous iron formation unit with spatially associated quartz-sulphide veining. Results indicated only low gold values; however, the author’s report a value of 0.137 oz/t Au from previous sampling along strike of the prospected system (AFRI #42L03SW0005).
A stripping and prospecting program was completed by R. Cote in 1991 to the southwest of the Property along strike with showings on the Property. No indications of sampling/sampling results were given in the report (AFRI #42E13NE002).
In 1992 a stripping and sampling program was carried out by local prospectors near DR2. Resulting gold values were discouraging but local percent-scale Cu, Pb & Zn suggested base metal potential (AFRI #42L03SW0033).
In 1999 a prospecting program was carried out by Kornelia and John Zygmont north of Cote 1A. A magnetic anomaly was discovered and manual stripping and sampling was completed. No assay results are given in the report (AFRI #42L04SE2001).
GEOLOGY
Regional
The Property occurs toward the western boundary of the Onaman-Tashota belt where a package of mafic metavolcanic rocks borders a younger granitoid complex as described by Thurston (1980). The mafic metavolcanics are predominately basaltic flows interlayered with
2
their pyroclastic equivalents. Volumetrically minor amounts of felsic volcanics (primarily in the southeast) and oxide-silicate-sulphide iron formation (primarily in the northwest) are also interlayered with the mafic metavolcanic rocks. The granitoids in the west are predominately of a biotite quartz monzonite composition.
Local
The geology underlying the Property consists predominately of pillowed to massive mafic metavolcanic rocks. Subsidiary amounts of interflow argillite, oxide-silicate-sulphide iron formation, mafic volcaniclastic rocks and lamprophyre dykes are also present. The western part of the Property is dominated by granite.
The contact metamorphic effects of the bordering granite are obvious in both the metavolcanic and interflow metasedimentary rocks. The mafic metavolcanic rocks are at amphibolite grade which has subsequently been overprinted by retrograde chlorite. The metasedimentary rocks, particularly the iron formation, contain variable amounts of amphibole, garnet, epidote and retrograde chlorite. The effect of contact metamorphism on quartz veining was mobilization/remobilization of silicious fluids and precipitation into dilatant structures forming crustiform pods and discontinuous veins of coarse quartz, calcite and sulphides. It is not known whether preexisting quartz veins were remobilized/recrystallized or if new fluids were introduced at the amphibolite-greenschist isograd. The dilatancy zones typically occur along lithological boundaries that were sheared during an earlier deformation event.
Township Claim
Number Number of Units
Recording Date
Due Date Ownership
Martin Lake 4229899 16 2008‐Mar‐07 2010‐Mar‐07 Sage Gold Inc.
Castlewood Lake 4229900 15 2008‐Mar‐07 2010‐Mar‐07 Sage Gold Inc.
Coughlan Lake 4230111 15 2008‐Apr‐07 2010‐Apr‐07 Sage Gold Inc.
Coughlan Lake 4230113 3 2008‐Apr‐07 2010‐Apr‐07 Sage Gold Inc.
Coughlan Lake 4222399 12 2007‐Nov‐01 2009‐Nov‐01 Robert Cote (50%); Richard Cote (50%)
Coughlan Lake 4213482 16 2006‐Dec‐01 2010‐Dec‐01 Robert Cote (50%); Richard Cote (50%)
Coughlan Lake 4228014 14 2008‐Jan‐14 2010‐Jan‐14 Sage Gold Inc.
Coughlan Lake 4213507 12 2007‐Aug‐02 2009‐Aug‐02 Robert Cote (50%); Richard Cote (50%)
Coughlan Lake 4229178 14 2008‐Feb‐22 2010‐Feb‐22 Sage Gold Inc.
Coughlan Lake 4229176 9 2008‐Feb‐22 2010‐Feb‐22 Sage Gold Inc.
Coughlan Lake 4229835 8 2008‐Feb‐22 2010‐Feb‐22 Sage Gold Inc.
Coughlan Lake 4222391 4 2007‐Aug‐20 2010‐Aug‐20 Robert Cote (50%); Richard Cote (50%)
Coughlan Lake 4227926 16 2008‐Jan‐14 2010‐Jan‐14 Sage Gold Inc.
Coughlan Lake 3008675 16 2006‐Apr‐19 2009‐Apr‐19 Robert Cote (50%); Richard Cote (50%)
Coughlan Lake 4229184 9 2008‐Apr‐07 2010‐Apr‐07 Sage Gold Inc.
Table 1: Property claims status
3
Mineralization occurs in coarsely recrystallized quartz veins & pods, in sulphidized iron formation, and in sulphidized chloritic shear zones that cut through the mafic metavolcanic rocks. Quartz veins range in texture from saccharoidal to drusy and contain variable amounts of coarse calcite, pyrite, pyrrhotite, chalcopyrite, sphalerite and galena.
2008 WORK COMPLETED
All samples from the 2008 program were collected by hammer & chisel and sent to either Actlabs or Accurassy Laboratories, both located in Thunder Bay. The assay certificates can be found in Appendix B.
A four-person prospecting program was carried out on the Property between June 13 and July 26. Those involved in the prospecting program are listed in Appendix A. Highlights of this sampling program are shown in Table 2. Two new showings were discovered during the prospecting program (DR1 and DR2; Figure 1). The best grab sample from showing DR1 yielded 2.98 g/t Au, 26.69 g/t Ag and 3.11% Cu. The sample was from a fine grained mafic volcanic rock containing 5% disseminated pyrite and chalcopyrite cut by a quartz vein. The best grab sample from DR2 yielded 1.25 g/t Au, 840 g/t Ag and 1.71% Pb. The sample consisted of a quartz vein containing clotty chlorite and 5% pyrite & 3% galena. Additional nearby samples also produced anomalous results from similar rock types (Table 2; Figure 2). Sampling was also conducted at known showings (Thumper and Granite; Table 2; Figure 2). The best sample from the Thumper showing produced 0.14 g/t Au, 1.9 g/t Ag and 5.05 Zn from a sphalerite bearing carbonate vein while the best sample from the Granite showing yielded 1.64 g/t Au, 82.10 g/t Ag, 0.70% Pb and 0.38% Zn from a sulphidized quartz vein cutting quartz-potassium feldspar porphyritic granite.
A stripping program was carried out between August 2nd and August 11th at five locations on the Property (Cote 1A, 1B, 2A, 2B and 3; Figure 2). Personnel involved in the stripping program are listed in Appendix A. The purpose of the stripping program was to extend the strike extent of areas known to contain anomalous precious and base metals. Highlights of the sampling completed at the five stripped areas are shown in Table 3. A brief description of each of the stripped areas is given below:
Cote 1A (Figure 4): The stripping work uncovered an approximately 245o/80oN trending shear zone which hosts a quartz-carbonate-sulphide vein up to 30 cm wide. The vein and shear zone separates a massive plagioclase porphyritic flow to the north from a north topping plagioclase porphyritic pillow basalt to the south. A lamprophyre dyke has intruded along the northern boundary of the shear zone. The vein contains coarse quartz and calcite crystals along with variable amounts of pyrite, pyrrhotite, sphalerite, chalcopyrite and galena. The best grab sample from the showing yielded 0.26 g/t Au and 0.5 g/t Ag.
Cote 1B (Figure 5): The resulting stripping exposed a 20 cm wide drusy textured quartz-calcite vein containing pyrite, pyrrhotite and sphalerite which cuts a rusty mafic volcanic breccia. The
4
thin breccia unit is bound to the north by poorly pillowed mafic volcanics and to the south, first by a breccia dyke and next by an argillite/lean iron formation unit. The breccia dyke trends approximately 250 o and contains clasts of quartz-potassium feldspar granite and sulphidized mafic volcanic rock. The best assay from the showing yielded 0.2% Zn.
Cote 2A (Figure 6): Stripping exposed a rusty graphitic argillite/iron formation cut by a bluish coloured pyritic quartz vein. The unit trends approximately 225o dipping steeply to the north. Small (10 cm) sections of the vein contain semi massive pyrite while the overall width of the sulphidized zone is 8-10 m. The best assay result from the stripping yielded 0.11% Zn.
Cote 2B (Figure 7): Stripping revealed a quartz vein up to 1 m wide in a zone of rusty stockworked argillite up to 3 m wide. The pyritic argillite has been sheared along 245o/80oN. The veins contain up to 20% pyrite, while pyrrhotite and chlorite occur along the vein selvedge. Veins show signs of shearing, but also crosscut the primary fabric in the shear zone. The best grab sample from the stripping yielded 2.05 g/t Ag and 0.17% Zn.
Cote 3 (Figure 8): The stripping work exposed a 255o/80oN trending package of mafic volcanics and interflow argillite. The approximately 4 m wide argillite package separates massive to brecciated flows to the north from plagioclase porphyritic pillow basalts to the south. Based on pillow tops, the package tops to the north. The argillite package has been sheared (sinistral movement) and injected with 5-10 cm wide drusy textured quartz veins containing pyrite, pyrrhotite and minor amounts of sphalerite and chalcopyrite. The best assay result from the stripping yielded 0.11 g/t Au, 5.60 g/t Ag and 0.29% Zn.
Sample Location Au (g/t) Ag (g/t) Cu (%) Pb (%) Zn (%) H096558 DR1 2.98 26.69 3.11 0.00 0.04
H096569 DR2 1.25 840.00 0.00 1.71 0.00
H096580 W of Cote 2A 0.06 29.90 0.06 1.12 1.93
H096606 NE of Cote 3 0.01 0.00 0.02 0.00 1.31
H096613 N of DR1 0.17 52.11 0.06 0.01 0.01
H424507 Granite 1.64 82.10 0.03 0.70 0.38
H096655 Thumper 0.59 5.80 0.01 0.00 1.04
H096659 Thumper 0.01 0.50 0.08 0.00 2.81
H096660 Thumper 0.04 0.80 0.09 0.00 1.61
H096713 Thumper 0.14 1.90 0.09 0.00 5.05
Table 2: 2008 prospecting assay highlights
5
Sample Stripping Au (g/t) Ag (g/t) Zn (%)
96663 Cote 1A tr tr 0.29
96664 Cote 1A 0.26 0.50 0.08
96724 Cote 1B tr tr 0.20
97185 Cote 2A tr tr 0.11
96509 Cote 2B tr 2.05 0.17
97211 Cote 3 tr 1.90 1.26
97209 Cote 3 0.11 5.60 0.29
Table 3: 2008 stripping assay highlights
INTERPRETATION & RECOMMENDATIONS
The bulk of the mineralization on the Property occurs within coarse quartz-calcite veins & pods that contain variable amounts of pyrite, pyrrhotite, sphalerite, galena and chalcopyrite. The veins & pods are largely structurally controlled, occurring at lithological contacts and/or shear zones. The contact metamorphic aureole of the bordering granite has prograded the surrounding rocks to amphibolite facies and remobilized/recrystallized the quartz veins into dilatant zones. These are typically located along at least three kilometre-scale geophysical anomalies that correspond to sheared interflow metasedimentary rocks.
Based on the geochemical data from historic and current work and examination of existing showings, the Property does not hold much potential for precious (Au-Ag) metals. The reason for the lack of precious metals in the system may relate to its high metamorphic grade - although gold deposits are known in amphibolite-grade rocks, they are not overly common. Despite this, the moderate gold values obtained from DR1 and DR2 do warrant additional investigation into the Properties precious metal potential. Furthermore, the granite hosted vein at the Granite showing opens up possibilities for an intrusion hosted system to the west which may bear resemblance to the Golden Mile district to the south.
The potential for any significant base metal mineralization is also considered to be rather low. This is in part due to the narrowness and poor strike extent of the individual veins and the (typically) low base metal values, with Zn being the most anomalous. Despite this, the various systems can be traced discontinuously along strike for several kilometers, warranting additional exploration at the prospecting level.
Given the favourable results at DR1 and DR2, additional prospecting and mapping should be completed to extend the strike extent of the mineralized zones. Of particular interest is the elevated Au, Ag, Pb, Bi, Te and W at DR2. If additional grab sampling and mapping reveals a system of reasonable strike extent and similarly elevated precious-base metal values, than a stripping program should be completed. No additional work is recommended at any of the stripped locations at this time.
6
This report was prepared and submitted by Ronnie Therriault on behalf of Sage Gold Inc. The information contained within this report is known by the author to be accurate and true.
Clark, L. 1990. Summary of the Coughlin Lake area project. AFRI #42L03SW0005.
Cote, R. Cote property Onaman River area. 1991. AFRI #42E13NE002.
Goodman, D. 1992. Brennan Lake property. AFRI #42L03SW0033.
Syme, J.A. 1951. Report on electromagnetic survey on Hopkins #2. AFRI #42L035SW0028.
Thurston, P. 1980. Geology of the northern Onaman Lake area, District of Thunder Bay. Ontario Geological Report 208. 81p. Accompanied by Map 2411, scale 1:31 680 and Chart A.
Wahl, J.A. 1984. Kerr Addison Mines Limited. Report on the reconnaissance exploration Conglomerate Lake area Northwestern Ontario. AFRI #42E13NE0038.
Zygmont, K and Zygmont, J. 1999. Property submission for assessment credit. AFRI #42L04SE2001.
~ J\CCURJ\SSJ\Y 1 0~ Gorh<l:rl St r 'C' t T I: (807) 626 ·1 630 www.accurassay.com l"' 8O~A T o n l[S Thunder £l ily, ON r "" (807) 6/2-757 1 Jssaytroi!CCWJS-lla;y com
C~nMI" P7B 5XS
Certificate of Analysis Friday. Augusl 15, 2008 ~
1'" Sage Gold Inc.
G 0v
Suite 500, 365 Bay St. \' Toronto, ON, CAN M5H2V1 Ph#: (416) 204-3170 FaX#: (416) 260-2243 Email#: [email protected]
The results Includod on this report relate only to the itoms tested The Cortlflcale of Analysis should not be reproduced excopt in full, without the written approval of the laboratory
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rJe ACCURASSAY 1046 Go,ha In Street Tel: (807) 626· '630 'JlvVw .(lC(t.JrtlSS(]Y,(om
L. ... aORAfOIl.[$ ThundN Bay, ON F"x·,8071622·7571 (] S5dY(~.\1('u! assay_c.om Canod" P7B 5X5
Certificate of Analysis Friday. August 15.2008
Sage Gold Inc. Suite 500, 365 Bay St. Toronto, ON, CAN M5H2V1 Ph#: (416) 204-3170 FaX#: (416) 260-2243 Email#: [email protected]
The results Included on this report relate only to the Items tested The Certificate of Analysis should not be reproduced except in full, without the written approval of the laboratory
AL917 -0384-0811512008 3:09 PM
Page 2 of2
ACCURASSAY 1046 Gor ha m Stree Tel: (807) 626· 1630 '.'I\"/V/,aCCu(.HsJ.ycom
The results Included on this report relate only to the items tested The Certificate of Analysis should not be reproduced except In full, without the written approval of the laboratory
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Pnge lof4
~ ACCURASSAY 10·) Go rham S\r~et Te l: (80 7) 626- 1 (; 30 \V\.~}W.Q ((u r d~)Jy.com
lA.110RllO rf l(S Thu,vlc , Bay, ON f~" (80 7) 622-75 7', dl SS(l,Y@ i:l CCLH,)S(,03Y com CJoJda P7 B SX5
Certificate of Analysis Wednesday. July 30. 2008
Sage Gold Inc. (j<C Date Received: Ju13,2008 Suite 500, 365 Bay 8t. Date Completed: Ju128,2008 Toronto, ON, CAN M5H2V1 Job #: 200842203 Ph#: (416) 204-3170
Reference: F ax#: (416) 260-2243 Email#: [email protected] Sample #: 75 Rock
The results Included on this report relate only to the Items tested The Certificate of Analysis should not be reproduced except in full, without the written approval of the laboratory
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d't:D ACCURASSAY 1046 Gor ham Street Tel. ',807) 626-1630 I,vwV'/.accuras,ay.cam
lA. 90RATOR1 ( S Th under 80). ON Fax~ (807) 622 -757 1 Js,ay,<" JCc 'J' assJy.cor1 (anJd ~ P7{; 5X5
Certificate of Analysis Wednesday, July 30, 2008
Sage Gold Inc. Suite 500, 365 Bay St.
~r Toronto, ON, CAN M5H2V1 Ph#: (416) 204-3170 Fax#: (416) 260-2243 Email#: [email protected]
The results Included on this report relate only to the items tested The Cortiflcate of Analysis should not be reproduced e'tcept In full, without tho written approval of the laboratory
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Page 3 of 4
..
Wednesday. July 30. 2008
Sage Gold Inc. Suite 500, 365 Bay St. Toronto, ON, CAN M5H2V1 Ph#: (416) 204-3170 FaX#: (416) 260-2243 Email#: [email protected]
The results Included on this report relate only to the Items tested The Certificate of Analysis should not be reproduced except in full, without thewrttten approval of the laboratory
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1046 Gorham SHeet Thuncler 8a)'. ON Canaaa P7B 5X5
Tel 180716261630 Fa., 18071622 7571
ww ... accurassiI\.com ilSSit~'aCCUrilSSil¥.com
Certificate of Analysis Monday.August18.2008
Sage Gold Inc. Suite 500,365 Bay St. Toronto, ON, CAN M5H2V1 Ph#: (416) 204-3170 FaX#: (416) 260-2243 Email#:[email protected]
Date Received: Ju18, 2008 Date Completed: Aug 18,2008
Job #: 200842301 Reference:
Sample#: 101 Rock
Rh Ag Co Cu Fe Ni Pb Zn ppb ppm ppm ppm ppm ppm ppm ppm
1.29 222 29 102 <1 56 21 50
1.60 52 32 77 2.05 133 44 1663
<1 19 15 35 <1 14 15 31 <1 18 17 39 <1 7 9 16
1.48 70 34 143 1.59 76 33 137 1.87 68 36 118
<1 296 20 213 <1 140 19 490
2.76 244 64 2632
The results Included on this report relate only to the Items tested The Certificate of Analysis should not be reproduced except in full, without the written approval of the laboratory
AL917-0384-08/181200B 4:49 PM
Page 50f5
Quality Analysis ... Innovative Technologies
Sage Gold Inc
408 Bay St Orillia Ontario L3V JX4 Canada
Date Submitted: 28·Jul-08
Invoice No.: A08-4533 (i)
Invoice Date: 21·Aug-OB
Your Reference:
-j K( ~, ~ < ' ! ",vJ J C,.lJ"V .l
AnN: Ulrich H. Kretschmar
CERTIFICATE OF ANALYSIS
48 Rock samples were submitted for analysis.
The (ollowing analytical packages were requested : Code IA2-Tbay Au - Fire Assay AA Code 1 E3 Aqua Regia ICP(AOUAGEO)
REPORT A08-4533 (i)
This report may be reproduced without our consont. If only selected ponions 01 the report are reproduced. permiSSion must be oblalned If no instructions were given at lime of sample submittal regarding excess malena!. it Will be discarded within 90 days of this report . Ourtiablhty IS limited sotely to the analytical cost of these analyses Test results are representative only of malerial suominea for analysis.
NOles : If value exceeds upper limit we recommend reassay by fire assay gravimelric-Code lA3 Values which exceed the uppar limit should be assayed for accurate numbers.
ACTIVATION LABORATORIES LTD.
CERTIFIED BY :
Ehtsa Hrischeva. Ph.D,
Quality Conlrol
IlJ6 S.MM 0"'0, Ano.,"or Onlano Can"", L9G 4V5 rElEPHONE. I ~05 84B 961 I or -, eaa :!:!B 5227 FAX -I 90564896'3
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Page 2 of 5
Report: B. B, -, ppm
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Page 5 of 5
CERTIFICATE OF ANALYSIS
Innovative Technologies Quality Analysis ...
Invoice No.:
Invoice Date:
Date Submitted:
Your Reference:
27-Oct-08
Painted Turtle
18-Aug-08
A08-5240
Sage Gold Inc
365 Bay StreetSuite 500Toronto Ontario M5H 2V1Canada
Bill LoveATTN:
This report may be reproduced without our consent. If only selected portions of the report are reproduced, permission must be obtained. If no instructions were given at time of sample submittal regarding excess material, it will be discarded within 90 days of this report. Our liability is limited solely to the analytical cost of these analyses. Test results are representative only of material submitted for analysis.
E-MAIL [email protected] ACTLABS GROUP WEBSITE http://www.actlabsint.com
Elitsa Hrischeva, Ph.D.
CERTIFIED BY :
REPORT A08-5240
Notes:
181 Rock samples were submitted for analysis.
Code 1E3-Tbay Aqua Regia ICP(AQUAGEO)Code 1A2-Tbay Au - Fire Assay AA
If value exceeds upper limit we recommend reassay by fire assay gravimetric-Code 1A3Values which exceed the upper limit should be assayed for accurate numbers.
Quality Control
The following analytical packages were requested:
Activation Laboratories Ltd. Report: A08-5240Au Ag Cd Cu Mn Mo Ni Pb Zn Al As B Ba Be Bi Ca Co Cr Fe Ga Hg K La MgAnalyte Symbol
Activation Laboratories Ltd. Report: A08-5240Na P S Sb Sc Sr Ti Te Tl U V W Y Zr Zn Ag PbAnalyte Symbol% % % ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % g/tonne %Unit Symbol
Activation Laboratories Ltd. Report: A08-5240Na P S Sb Sc Sr Ti Te Tl U V W Y Zr Zn Ag PbAnalyte Symbol% % % ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % g/tonne %Unit Symbol
Activation Laboratories Ltd. Report: A08-5240Na P S Sb Sc Sr Ti Te Tl U V W Y Zr Zn Ag PbAnalyte Symbol% % % ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % g/tonne %Unit Symbol
Activation Laboratories Ltd. Report: A08-5240Na P S Sb Sc Sr Ti Te Tl U V W Y Zr Zn Ag PbAnalyte Symbol% % % ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm % g/tonne %Unit Symbol
Au Ag Cd Cu Mn Mo Ni Pb Zn Al As B Ba Be Bi Ca Co Cr Fe Ga Hg K La MgAnalyte Symbolppb ppm ppm ppm ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm % ppm ppm % ppm %Unit Symbol
Au Ag Cd Cu Mn Mo Ni Pb Zn Al As B Ba Be Bi Ca Co Cr Fe Ga Hg K La MgAnalyte Symbolppb ppm ppm ppm ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm % ppm ppm % ppm %Unit Symbol
Au Ag Cd Cu Mn Mo Ni Pb Zn Al As B Ba Be Bi Ca Co Cr Fe Ga Hg K La MgAnalyte Symbolppb ppm ppm ppm ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm % ppm ppm % ppm %Unit Symbol
Au Ag Cd Cu Mn Mo Ni Pb Zn Al As B Ba Be Bi Ca Co Cr Fe Ga Hg K La MgAnalyte Symbolppb ppm ppm ppm ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm % ppm ppm % ppm %Unit Symbol