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2 . 3v2 3
Assessment Report
Prospecting In the
Buckland and Delmage Township Properties
Sault Ste. Marie Mining Division
Northeastern Ontario
NTS: 42 B/4
Written by;
OCT 0 3 2008
Claudia Wilck, RR 1, Parry Sound ON, P2A 2W7
September 26, 2008
For
Chalice Diamond Corp.
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TABLE OF CONTENTS
Introduction - ownership. description and overview Location and Access General Geology Personnel Prospecting Program Sampling Procedures Analytical Procedures Discussion Target Bu_06 overview, traverse / location map, field log Target Bu_12 overview, traverse / location map, field log Target Del_ 02 overview, traverse / location map, field log Target Del_03 overview, traverse / location map, field log Target Del_04 overview, traverse / location map, field log Target Del_09 overview, traverse / location map, field log Target DelIO overview, traverse / location map, field log Target Vtem_76 overview, traverse I location map, field log Target Vtem_77 overview, traverse / location map, field log Target Vtem_77(2nd pass) overview, traverse / location map, field log Recommendations Qualifying Statement References
Figures in back pocket
Figure 1: Chalice Diamond Corp. - Access & Target Location Map for Buckland and Delmage Township Claims
Figure 2: Key Location Map of Chalice Diamond Corp. Project Area
APPENDICES
Page 1 1 2 3 4 4
4-12 13-15
16-18
19-21
22-24
25-27
28-30
31-33
34-38
39-44
45-50 51 51 52
Appendix 1 - True North Mineral Laboratories Inc. I Actlabs: Geochemical AnalYSis Results with Certificate of Analysis
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Introduction - Ownership, Description and Overview
Golden Chalice Resources Inc of Vancouver, British Columbia holds a 100% interest in 8 claims being numbers: 4202041 (16 units/256 ha) and 4202053 (16 units/256 ha) both situated in Buckland Township and 4202034 (16 units/256 hal, 4202043 (16 unitsl256 ha), 4202044 (16 units/256 ha), 4202045 (16 units/256 hal, 4202054 (16 units/256 ha), 4202056 (16 units/256 hal, all situated in Delmage Township.
Golden Chalice Resources Inc and Chalice Diamond Corp. have an approved Plan of Arrangement in place since September 21, 2006 and as a result work may therefore be filed by Chalice Diamond Corp on Golden Chalice Resources Inc claims.
All of the above mentioned claim blocks are contiguous and are located @ 80 km northeast of Wawa in northeastern Ontario. See figure 1 - Access and Location Map for Buckland & Delmage Township Claims.
The prospecting program was conducted over portions of these claims during the summer months 2006 and 2008. A total of 9 target areas were prospected by teams of two (or more) in the search for diamond, gold and base metal commodities; Dedicated field crews located target areas using hand-held GPS instruments - logging waypoints, traverse routes and sample locations (See: Traverse way points and samples locations map accompanying each target area overview); prospecting notes and sample observations were recorded on formatted sheets. (See Field Logs accompanying each target overview and Fig. 1 for Target Location Map). Target areas BU_06, Bu_12 in Buckland Township and DeL02, DeL03, Del_04, DeL09, Del_10, Vtem_76 and Vtem_77 in Delmage Township were prospected (See: Target area overview for each target and UTM coordinates), 1 rock sample was collected in order to ascertain geochemical analysis for 1 E1, Au and PGEThe rock. samples were processed by True North Mineral Laboratories of Timmins, ON,
The costs associated with conducting the work program outlined in this report are to be applied to claims: 4202034 (16 units/256 ha) and 4202045 (16 units/256 ha) having imminent due dates of October 28, 2008.
location and Access
The claims are located @80 km northeast of Wawa in northeastern Ontario in the Sault Ste. Marie Mining Division. To access the property, from Wawa ON, take Hwy '101 about 65km east, turning north onto Hwy 651, drive about 27km to the Dalton Road (forest access road) and turn east. The target areas vary between 30 km and 45 km east along the Dalton logging roads. (See each target area for detailed access and location.) See figure 1 - Access Map to the Buckland and Delmage Township claims.
The town of Missanabie is located @ 56 Km north of Hwy 101 along Highway 651 and the field crews were based in Missanabie during the duration of the program, The prospecting teams traveled by truck and may have also used ATV to reach the target areas each day. See: Field Logs accompanying each target overview for traverse waypoints and sample UTM Coordinates.
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General Geology (after Bennett, Gerald, 1978, GR172 OGS)
The major lithologic units are of Precambrian age. The oldest recognized rocks are metamorphosed basaltic flows, intermediate to felsic pyroclastics and flows, detrital metasediments and minor iron formation which form a metavolcanic-metasedimentary complex of Early Precambrian age. The metavolcanics have been intruded by a variety of metamorphosed intermediate to felsic porphyries and metagabbros.
The metavolcanic-metasedimentary belt is folded into a shallow plunging, generally southeasttrending syncline. The metamorphic grade ranges from lower green-schist in the northwest to almandine-amphibolite in the south and southeast. A variety of syntec-tonic and post-tectonic granitic plutons intrude the metavolcanic-metasedimentary complex.
The presence of extensive areas of catazonal igneous and metamorphic rocks in the southern and southeastern parts of the area indicates considerable uplift relative to the northern part. This uplift may coincide with that of the Kapuskasing structures.
Numerous diabase dikes intrude all of the major lithologic units of the area.
A syenite dike and a few ultramafic lamprophyres are the youngest known rock types of the area.
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• Personnel
The following personnel worked on this property and conducting the following work activities summarized below:
Personnel Activity Dates Worked Man Days
Josh Guthrie Prospecting July19, 2008 1 day
Dakota Souliere Prospecting June 4,2008 1 day
Frank Longpre Prospecting October 5, 7, 8, 9 & 10/06 5 days
Ryan Brown Prospecting July 19/08 & Aug. 13/08 2 days
Katy Richard Prospecting July "9, 2008 1 day
Stephen Polson Prospecting Oct. 7, 8, 9, 10 & 12,2006 5 days
Roseanne Therrien Compiling Data August 10, 11, 12 & 13, 2006 4 days (in field office-Missanabie)
Dan Sullivan Prospecting October 4 & 5, 2006 2 days
Elizabeth Laidlaw Prospecting June 4,2008 1 day
Mark Dufualt Prospecting Aug. 13,2008 1 day • Terra Dittenhoffer Prospecting June 4,2008 1 day
Alain Sigouin Prospecting October 4 & 5, 2006 2 days
Erik Peterson Prospecting Aug. 13,2008 1 day
Jim Laidlaw Prospecting October 12, 2006 1 day
Graham Stone Logistics Oct. 4 & 5/06 & June 4, 2008 (in field office-Missanabie) August 10, 2008 4 days
Claudia Wilck Report Sept.19 to 26, 2008 8 days
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Prospecting Program
In the Buckland and Delmage Township claims possible kimberlite targets have been identified from the residual magnetic intensity data, based on the identification of roughly circular anomalies. This procedure was automated by using a known pattern recognition technique (Keating, 1995), which consists of computing, over a moving window, a first-order regression between a vertical cylinder model anomaly and the gridded magnetic data. Only the results where the absolute value of the correlation coefficient is above a threshold of 7S% were retained. The results are depicted as circular symbols, scaled to reflect the correlation value. The most favorable targets are those that exhibit a cluster of high amplitude solutions. Correlation coefficients with a negative value correspond to reversely magnetized sources. It is important to be aware that other magnetic sources may correlate well with the vertical cylinder model, whereas some kimberlite pipes of irregular geometry may not.
Keating Correlation Coefficients (modified from Ontario airborne geophysical surveys, magnetic data, Wawa area; Ontario Geological Survey, Geophysical Data Set 1009-Revised, 2003)
Keating magnetic anomalies were identified from Geological Survey of Canada 2001: First Vertical Derivative of Magnetic Field with Keating Coefficients Map Dumont R., Coyle M., Potvin J., Geological Survey of Canada, 2001 Ontario: Bolkow, NTS 42 B/4 Open File 4064 lOGS Map 81707
A total of 7 Keating anomaly target areas and 2 Vtem target areas were prospected by teams of two (or more) in Buckland and Delmage Townships. Dedicated field crews located target areas using hand-held GPS instruments - logging waYPoints, traverse routes and sample locations (See: Traverse waypoints and samples locations map accompanying each target area overview); prospecting notes and sample observations were recorded on formatted sheets. (See Field Logs accompanying each target overview). Each evening the prospecting team download their GPS into the main data base for the project and write up an overview on each target; prospecting notes and sample observation sheets are entered into the main data base at the Missanabie field office.
Sampling Procedures
Sampling methods of the rock is standard as with most methods of precious and base metal sampling. The objective is to collect a large enough sample to allow a complete geochemical analysis and retain a hand specimen. When enough rock was obtained, a sample number tag was enclosed within the sample and the sample bags were securely closed using double wraps of flagging tape or zip ties. Sample sites were flagged with sample number, sample location UTM Coordinates entered into a hand held GPS and general sample comments noted; such as Sample Number, Zone, Easting, Northing, Claim Number, Township and Sample Comments: i.e. sample colour, grain size, mineralization, magnetic and acid tests and landform characteristics. Samples were then promptly taken to the field office at the end of each working day. (See: Field Logs accompanying each target area overview) The samples were secured and controlled at the Chalice Diamond Corp field office located in Missanabie ON. Here the samples were inventoried as a double check against the field data notes so that all samples were accounted for. Subsequently, most of the samples were transported directly to True North Minerals Laboratories Inc. in Timmins ON.
Analytical Procedures Discussion
True North Mineral Laboratories Inc, located at 475 Railway Street, Timmins Ontario, P4N 2P5, telephone (705) 268-0303 was engaged to analyse the rock samples (to be crushed - RX2) for 1 E1, Au and PGE. True North Mineral Laboratories Inc. / Actlabs - geochemical procedure is as follows:
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• Sample Preparation
To obtain meaningful analytical results, it is imperative that sample collection and preparation be done properly. ACTLABS can advise on sampling protocol for your field program if requested. Once the samples arrive in the laboratory, ACTLABS will ensure that they are prepared properly. As a routine practice with rock and core, the entire sample is crushed to a nominal minus 10 mesh (1.7 mm), mechanically split (riffle) to obtain a representative sample and then pulverized to at least 95% minus 150 mesh (106 microns).
As a routine practice, we will automatically use cleaner sand between each sample at no cost to the customer. Quality of
crushing and pulverization is routinely checked as part of our quality assurance program. Randomization of samples in larger
orders (>100) provides an excellent means to monitor data for systematic errors. The d'3ta is resorted after analysis according to sample number. Please request Code Random (additional $1.00fsample) if you prE!fer randomization.
Samples submitted in an unorganized fashion will be subject to a sorting surcharge and may substantially slow tumaround time, Providing an accurate detailed sample list bye-mail will also aid in improving turnaround time and for Quality Control purposes, Additional charges may apply for poorly organized batches. Code CP2 - Sample list not provided for orders over 25 samples ($O.25/sample); Code CP3 Sorting chaotic shipments ($O.50/sample).
Rock, Core and Drill Cuttings
code RX1 crush up to 75% passing 2 mm, split (250 g) and pulverize (hardened sleel) to 85% passing 75;> « 5 kg:
code RX1 crush up to 90% passing 2 mm, split (250 g) and Terminator pulverize (hardened steel) to 85% passing 75)1 « 5 kg: code RX2 crUSh, split and pulverize with mild steel (100 g)
(best for low contaminatioF1l code RX3 oversize charQ.eQer kilOgram (if reguiredl code RX4 pulverization only (mild steel)
(coarse pulp or crushed rock) code RX5 pulverize ceramic (100 g) code RX6 hand pulverize small samples
Pulverization Contaminants Added (amount added depends on hardness of material and particle size required)
Mill Type
Mild Steel (best chOice) Hardened Steel
Ceramic Tungsten Carbide Agate
Contaminant Added
Fe (up to 0.2%) Fe (up to 0.2%), Cr (up to 200 ppm), trace Ni, Si, Mn and C AI (up to 0.2%), Sa, trace REE W( up to 0.10/01 Co, C, Ta, "'band 1i Si (up to 0.3%), AI, Na, Fe, K, Ca, MQ, Pb
Note: Larger sample sizes than listed above can be pulverized at additional cost.
Soils, Stream and Lake Bottom Sediments Biogeochemical Samples
code S1 drying (50°C) and sieving (-aO mesh) save all portions $3.25 code S1 drying and blending humus code S1 DIS drying.{60·C) and sievingJ-BO meSh), discard oversize $2.75 code B2 drying and macerating vegetation code S1-230 drying (60OC) and sieving (-230 mesh), save oversize $4.25 code B3 dry ashing code S1-230 DIS drying (60CC) and sieving (-230 meSh), discard oversize $4.00 code B4 washing vegetation code 82 lake bottom sediment preparation crush & sieve (-SO mesh) $6.50 code 65 samples submitted in plastic bags. add code S3 alternate size fractiOns and bracket sieving, add $2.00 code S4 Enzyme Leach"" or SGH drying (400 C) & sieving (-60 mesh) $3.50 code 85 wet or damp samples submitted in plastic bags, add $1.50 code 86 separating -2 micron material $65,00 Special Digestion Procedures
code S7 methylene iodide heavy mineral separation $50,00 specific gravity of 3.3 (250 grams) codeMDI Microwave digestion - closed vessel
Sample Storage and Disposal All soil, sediment and vegetation coming from outside Canada require incineration prior to disposal under CFIA regulations. All pulps and rejects will be returned to the client at cost. Disposal costs are additional. Pulps and rejects will incur a storage fee after 6 months.
RTRN Retum of all reject portions and/or pulps At cost INCIN Incineration of soil, sediment and vegetation samples from outside Canada $0.25
(for samples up to 0.5 kg; samples over 0.5 kg will have higher inCineration costs) STORE 1 Monthly storage of reject after 6 months $0.20 STORE 2 Monthly storage of pulps after I) months $0.08 STORE 3 Monthly storage of sieve rejec15 after 6 months $0.10
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$4.00 $5.25 $7.50 $3.50 $1.50
$35.00
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Precious Metal Geochemistry Gold and Silver Analyses
Code Method
1A1 Au Fire Assay-INAA (Qeochem) IA2 Au Fire Assay-AA Jgeochem) 1A2-50 Au Fire Assay-AA (QeocI1em)
Sample Weight
30 Q
30g 50 Q
Imperial Range
Metric Range
1-20,000 ppb 5-3,000 ppb 5-3000 ppb
Price
$16.00 $13.50 $15.00
IA3-30 AI.! Fjre Assay-Gsavimetric [Assay] 29.16 Q 0.001-30 QZJt 0.03-1 000olmT _$17.5Q 1A3-50 Au Fire Assay-Gravimetric (Assay) 50 q 0001-30ozJt 0.03-1 000 QlmT $18.50 1A3-Ag Au, Ag Fire Assay-Gravimetric (Assay) 29.16 9 0.001-30 ozJl (Au) 0.03-1,000 glmT (Au) $20.00
.. .. Code 1M or 1A4-1000 - A representative 500 gram or 1000 gram sample split is sieved at 100 mesh (149 micron),
with assays perfonned on the entire +100 mesh fraction and two splits of the -100 mesh fraction . It is important not to
overpulverize the sample too finely, as tests have shown gold will plate out on the mill and be lost. When assays have
been completed on the coarse and fine portions of the bulk sample, a final assay is calculateC: based on the weight of
each fraction. Price includes sample screening but not crushing and pulverizing .
• • Code 18 - Detection limrts for Pt are increased with high Au/Pt ratios and limits for other elements will be affected by
abnonnallY high Au, Sb and Cu content. Samples with high Au can be reanalyzed by Code 1C exploration or research.
Zn concentrates are not amenable to the nickel sulphide fire assay.
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Assay Products Code 8 - Assay Products
Assays provide quantitative determinations of elements in non-processed geological materials. Assays are usually required only when the client knows or suspects higher levels of metals in samples. Geochemical methods generally provide lower detection limits than assays. For lower levels, geochemical methods should be used. All assays are traceable to international reference standards. Prices listed in our fee schedule are for normal geologic materials and are not for metallurgical products. Metallurgical products such as heads and concentrates are handled separately to prevent contamination in the laboratory. These materials are charged at five times the prices listed in our fee schedule.
Element Price
Alumina - AI,O, $20.00 Antimony - Sb $20.00 Arsenic - As $20.00 Barium (Instrumental) - Ba $20.00 Barium (Gravimetric) - Ba $30.00 Beryllium - Be $2500 Bismuth - Bi $20.00 Boron - B $25.00 Bromine - Br $20 .00 Cadmium - Cd $18.00 Calcium (oxide) - CaO $20.00 Cerium - Ce $20.00 Chlorine - CI $25.00 Chromium - Cr $20.00 Cobalt - Co $10.00 Copper (total) - Cu $10.00 Copper (CN soluble) $11 .00 Copper (Acid soluble) $10.00 Copper (Ferric sulfate soluble) $11 .00 Copper (Sequential Oxide Analysis) $30.00 Fluorine - F $25.00 Gold -Au See Code 1A3 Gold-Silver (Au-Ag) See Code 1A3-Ag Gallium - Ga $25.00
Germanium - Ge $35.00 Insolubles $18.00 Iron (oxide) - Fe.O, $15.00 Lanthanum - La $15.00 Lead (total) - Pb $10.00 Lead (oxide) - PbO $20.00 Lithium - Li $20.00 Loss on ignition - LOI $9.00
Elements in brackets are optional, see noles. page 10·11 f oll!Y :;uiph:de s\J)phu( '::x{,~[1cte{j
The "Au+14" group of elements provides a high quality, low cost package for epithermal gold exploration [by INAA (Au, As, Sb, Ba, H9 and W), aqua regia ICP (base metals and sulphur) and optional cold vapour FIMS (Hg)]. A sample of -30 9 is used for Au analysis. An enhanced package (Code 1 EPI enhanced) with better detection limits for Au (2 ppb) and As (0,5 ppm) also is available for an additional $2.00 per sample. (35 9 required}. Sulphur (+\ from barite will not be reported. Iftotal S is required, see Code 4F-S. See Code 1E for notes on base metals.
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Trace Element Geochemistry Which digestion do I use?
1. AQUA REGIA DIGESTION - This leach uses c; combination of concentrated hydrochloric and nitric acids to leach sulphides, some oxides and some silicates. Mineral phases Which are hardly (if at all) attacked include barite, zircon, monazite, sphene, c;lromite, gahnite, gamet, ilmenite, rutile and cassiterite. The balance of silicates and oxides are only slightly to moderately attacked, depending on the degree of alteration. Generally, but not always, most base metals and gold are usually dissolved if the sample is ground finely enough.
2. "TOTAL" DIGESTION - This acid attack is the most vigorous used in geochemistry. It will employ hydrochloric, nitric, perchlotic and hydrofluoric acids. Even \'f.~ this digestio y
: , certain minerals (barite, gahnite, chromite and cassiterite) may not go into solution. Other minerals including zircon, sphene and magnetite may not be totally dissolved. Most other silicates will be dissolved, however some elements will be erratically volatilizeel, including Si, As, Sb, Cr and Au. Total digestic,lS cannot be used for accurate determinations of REE, Ta, Nb, As, Sb, Sn, Hf, Cr, Au and Si.
3. FUSION TECHNIQUE· The most aggressive fusion technique employs a lithium metaborateltetraborate fusion. The resulting molten bead is rapidly digested in a weak nitric acid solution. The fusion ensures that tile entire sample is dissolved. It is only with this attack that major oxides including SiO, • REE and other high fielel strength elements are put into solution. High sulpnide bearing rocks may require different treatment, but can still be adequately analyzed.
N OTE: Results from aqua regia or total digestions may be lab de!)endent or lab operator dependent. Actlabs has automated this aspect of digestion using a microprocesso·· designed hotbox to accurately reproduce digestion conditions every time.
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Code 1 EPI/MS - The · Au+23" group of elements is similar to Code 1 EPI but includes a suite of elements by ICPIMS to provide virtually all elements Lsed for epithermal gold exploration. The multielement acid attack will only dissolve the soluble forms of barium, while INAA will provide the total barium concentration. The total Ba to soluble Ba ratio will be a direct indicator of barite concentration. Code 1EPIIMS Enhanced is available which offers Au - 2 ppb, As - 0.5 ppm. Sb - 0.1 ppm for an additional $2.00 per sample (35 9 required). See Code 1 E for notes on base metals.
Code 10 - The sample is encapsulated, irradiated and measured in a multielement mode by INAA for Au+34 elements. The elements in this package are determined non-destruclively and the total metals help the geologist determine rock types, alteration and pathfinder elements. The 30 g aliquot provides a representative sample size for gold analysis (0.5 to 30 g required).
Code 10 enhanced - This INAA package is similar to Code 10 but has enhanced detection limits. This package has become very popular for rock, soil, lake sediment and stream sediment samples (0.5 to 30 g required) .
Code 1E - This package determines a base metal suite and sulphide sulphur by an aqua regia eKtraction with an ICP/OES finish. I" accuracy better than +1- 10-15% is required for higher level samples we recommend assays (Code 8) (+1- 3%) for Cu, Zn and Ni over 10,000 ppm and certainly over 50,000 ppm. Assays are also recommended for Pb >5000 ppm and Ag >100 ppm due to potential solubility problems. Values exceeding these limits are estimates and are provided for information only. (0.5 g of sample required) . Prices: first element $5.00; each additional element $2.00.
Code ', E1 • This analytical package uses the same digestion as Code 1E. The same comments apply as in Code 1E for base metals. In addition, a variety of other elements are obtained non-quantitatively since chromite, barite, silicates, magnetite, sphene and some other mineral phases are not soluble with this digestion. Zinc in gahnite or sphene will not be soluble in aqua regia and all Ni in silicate phases may not be totally leachable. (0.5 g of sample required).
Code1 E2, 1 E3 - These are similar to Code 1 E1 , but offer an enhanced list of analytes. (0.5 g of sample is required). Code 1 F, 1 F2 - These packages uses a "near Iota I " digestion employing HF, HCIO., HNO, and HCI to get as much of the sample into solution as
possible without fusing the sample. The resulting metals are determined by ICP/OES. Sulphide sulphur is included. The sulphur associated with barite will not be dissolved. Other phases which may not be totally digested indude zircon, monazite. sphene, gahnite, chromite, magnetite, barite, cassiterite, ilmenite anc rutile. The same comments apply as in Code 1 E for base metals. (0.25 9 of sample required).
Code ULTRATRACE-1 - This partial extraction is analyzed by ICP/MS to provide lower detection limits. Upper limits are up to 20,000 times the detection limits. (0.5 g of sample is required) .
Code ULTRATRACE-2 - This combines ULTRATRACE-1 with Code 1E2 to provide a few additional elements from the ICP/OES as well as extend the upper limits of the ULTRATRACE-2 elements. (0.5 g of sample is required).
Code 1 H "Au+48" - This package provides a trace element scan for virtually all types of economic mineralization. It also provides useful information on alteration, rock types, and pathfinder elements. The Code 10 enhanced (INAA) and Code 1F (4-acid digestion ICP technique) provide 49 elements. The elements determined by INAA are Au, As, Ba, Br, Ce, Co, Cr, es, Eu, Fe, Hf, Hg, Ir, La, Lu, Na, Nd, Rb, Sb, Sc, Se. Sm, Sn, Ta, Th. Tb, U, W, Yb and Lu. The remaining elements are determined by the 4 acid ICP (Code 1 F above) technique. SiO, is not analyzed due to volatilization . (0.75 • 35 9 required depending on sample size yO\; wish to be analyzed for Au).
Code 1H2 "Au+53" - This package is similar to Code 1H but also uses ICPIMS on an acid digest solution to obtain additional elements. If Au is important, a larger sample size (up to 35 g) should be submitted.
Code ULTRATRACE-3 - This combines INAA, 4-acid digestion ICP and 'CP/MS analysis to provide the most comprehensive near total metal package available using an acid digestion. Note that this package is not suitable for chrondrite plots as not all REE are quantitatively extracted from zircon, monazite, etc. (1.0 to 35 g of sample required).
Code ULTRATRACE-4 - Near total digestion employing HF, HCIO., HNO, and HCI with ICP/MS finish (0.5 9 of sample required) This digestion may not be completely total if resistate minerals are present. As, Sb and Cr may be partially volatilized.
Code ULTRATRACE-5 - Combines INAA with a 4-acid digestion (HF, HCIO" HNO, and HCI) to attempt to give as total metal as is possible with acids. Some of the resistate elements are provided by INAA.
Lithogeochemistry for Exploration and Research All elements are in ppm except where noted.
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n Optional lements. see ode 4A
>+) Optional lements by INAA, ode 4BINAA
.) Optional ements by ,u/tlacid digestion :p. Code 4B1
PAGE
Code
AhO,
CaO Cr,O,
CuO FazO,
1<>0 MgO MnO Na,O
NiO P,O.
SiO, liO,
LOI Ag
As Au
Ba Be B;
Br
Ca Cd
Co Cr Cs Cu Fe
Ga Ge Hf
In
Ir /IIio Na Nb Ni Pb Rb
S Sb
Sc
Se Sn Sr Ta Th T!
U V W
Y Zn Zr
La
Ce
Pr
Nd Sm Eu Gd Tb Oy Ho Er Tm Yb Lu
# Samples 1-10 11+
XRF INAA INAA WRA-ICP Trace Element WRA+trace Trace Element WRA+trace WRA-XRF XRF pressed pellet
Total IDENT Total IDENT Code 4E-expl. Code 4E-research
0.01%
0.01%
0.01%
0.01%
0.01%
0 .005%
0.01%
0.01%
0.01% 0.01%
0.01%
0.5
2 5 ppb
3 1
10
1 0.5
1
1
0.5
1
(5")
0.5
5"ppb
5 (2~')
1 5
20 (2"'"*) 0.2
0.1
3 (5' '') 2 1 05
0.5
5 3 1 1
4
0.5
3
5 0.1
0.1
0.5
0.1 0.05
$49.00
S45.00
0.01%
0.01%
0.01%
0.01%
0.01%
0.005%
0.01%
0 .01%
0.01%
0.01% 0 .01%
0.5
1
1 flpb 1
1
10 .. , 0.5
0.5
0.1
0.5 0.2 n
1 (5~') ,I
0.2
"
1 ppb
2 (2" ') C ;:., .)
1
5 10 (2"'1 '++1
0.1
0.01
0.5
(5**' ) I
2 0.3 I)
0.1 ," • J
0.1 , • '-+1
5
1
1
1
4 . ,- )
0.05 ." 1 -. , .. 1 .. _ I I
0.01
0.05 L~"" ) v )
0.1 .'" .' (; .. ,
c
. l'
0.05 . " 0.01 11'
S108.00
S100.00
Notes: Code 4A .. Both the exploration and research grades are determined by INAA.
A minimum sample weight of 2 g is recommended. REE chondrite plots are provided at no charge with the research grade or at $~ .00 per sample for the exploration grade. For elements indicated with t (Code 4A RESIMS) by fusion ICPIMS, add $28.00.
Codes 48, 482-STD, 482-RESEARCH, 4L1THO, 4L/THORESEARCH - Actlabs has developed a lithium metaborateltetraborate fusior ICP \l\Jhole Rock Package Code 4B and a trace element ICPIMS package Code 4B2 which is unique for scope of elements and detection limits. The two packages are combined for Code 4Litho and Code 4Lithoresearch. The quality of whole rock data in Code 4B meets or exceeds quality of data by fusion XRF Code 4C, the old standard in whole rock analysis. The fusion process ensures total metals particularly for elements like REE in resistate phases. (This may not be the case for acid digestions, particularly for heavy rare earths and other elements contained in refractory minerals like zircon , sphene, monazite, chromite, gahnite and severa, other phases. If refractory minerals are not digested, a bias may occur for certain REE and HFSE with acid digestions). Quality of data is exceptional and can be used for the most exacting applications. The trace element pac~age by ICPIMS, Codes 4B2-STO or 4B2-RESEARCH, on the fusion solution provides research quality data whether using standard or research detection limits. Eu determinations are semiquantitative in samples having extremely high Ba concentrations (greater than 1 %). This package is intended primarily for unrnineralized samples. Mineralized samples can be analyzed, however, data may be semiquantitative for chalcophile elements (Ag, As, Bi, Co, Cu, Mo, Ni, Pb, Sb, Sn, Wand In). When quantitative values for the chalcophile elements are required on mineralized samples, please indicate as Code 4B2-STDQUANT, 4B2-RESEARCHQUANT, 4L1THOQUANT or 4L1THORESEARCHQUANT, and a surcharge of $16.00 per sample will apply. A minimum sample weight of 5 g is required. Elements With (+) are available (Code 4B1) for an additional S8.25 per sample. Those indicated with (++) are available by INAA (Code 4B-INAA) for an additional $15.00 per sample. Please add 0.5 to 30 g depending on sample size you prefer to analyze for Au with this option. Values on replicates and standards are provided at no cost, as are REE plots.
Code 4C • The tried and true fusion XRF whole rock package. Samples containing high barite or high sulphide (greater than 1 %) should be analyzed with Code 48. A minimum sample weight of 3 g is required. We reserve the right to change analytical method to Code 4B if required by the sample composition .
Code 4C1 - This XRF pressed pellet method requires a minimum sample weight of 6 g. The XRF pressed pellet method is only suitable for low metal content of below 1 % for each element listed. Prices: 1" element - $10.00; each additional- $3.00; .. lot - $16,00; * lot$16.00. Each element not in * or " , add $3.00 per element.
Code 4E - This unique package uses ICP, INAA, tCPIMS and XRF technologies to completely characterize geological samples. Two different grades of analysis (exploration and research) are provided depending upon your reqUirements . This package is not suitable for analyzing concentrates or mill products. A minimum sample weight of 5 g is required).
Code 4E Options • Ga, Pb, Sn, Nb and Rb (Code 4E-XRF) indicated by C" ) by Pressed Pellet XRF add $18.00. This package can be added to Code 4E exploration or Code 4E research (please add 6 g of sample). • The Code 4E ICPIMS add-on option (detection limits indicated by .) can only be added to Code 4E researcn grade at an additional cost of $30_00. • Any selections from Code 4F can be added to Code 4E exploration or research
Code 4F .. Other analyses associated with WRA (can be added to any Code 4 package). Add 1 gram for each option chosen.
FeO (0.1%) by Titration $15 .00
S (0.01%) by Infrared $15.00
SO· (0 .05%) by Infrared $20.00 CI (0.01%) by INAA $22.00 Hg by Cold Vapour FIMS $7.50 F (00 ': %) by ISE $10.00
/I
CO, (0.01%) by Coulometry H,O +/- (0.1%) by Gravimetric
C, S (0.01 %) by Infrared B (0.5 ppm) by PGNAA B (2 ppm) by PGNAA N (total) Thermal Conductivity
$15.00
$20.00
$20.00 $28.00 $18.00 $35.00
General Information ~ms and Conditions
All prices in this price list are exclusive of GST, are in Canadian dollars and apply only to clients submitting samples from Canada. These prices apply to most geological materials for routine analyses. A surcharge may apply for abnormal matrices or non routine analytical requirements. The client will be advised of any such conditions prior to performing the analytical work. A minimum charge of $75.00 will be effective on all orders. Payment should accompany the order unless credit has been established. Terms are net 30 days. Prices and packages are subject to change without notice. We reserve the right to subcontract work to affiliated laboratories. Clients can pay invoices by c'leque, bank draft, Visa, Mastercard or direct bank deposit (EFT).
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•
vials or glass bottles, ensure that they are taped shut and protected from breakage. Sealed plastic bags are best for shipping pulps. If using Bus Parcel Express, the bus station of destination is Hamilton, Ontario. For most efficient delivery, we recommend the use of couriers, or transport companies for heavier shipments.
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Return of Data Analytical reports can be returned via hard copy, CD-ROM, electronic mail (internet) or fax copy at the customers' discretion for no additional charge. Data is normally available in Excel format. Other formats are available on request. We have implemented a Laboratory Information Management System (UMS). Clients can track samples from sample reception and logging through to preparation, analySis and reporting.
~~l1around Time
.,osl analytical data is usually available within 2 weeks of receipt of samples. Certain analyses that may take longer periods of time, or abnormal
.olume of samples in thl;; laboratory may also slow turnaround time. Excessively wet samples may slow turnaround time, as will undocumented
PAGE
and unorganized shipments. If you require analyses by a certain date, please ensure that this is noted clearly on the request form, We will make every effort 10 meet your requirements, however, rush conditions may require payment of a surcharge and must be arranged in advance with the lab manager. We will contact you if we are unable to meet your requirements or if a surcharge is necessary.
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Location: BU 06 Name:(s); Jim Laidlaw & Stephen Polson Date : October 12, 2006 Datum : NAD 27 UTM Zone: 17U Easting: 295695 Northing: 5327120 Township: Buckland Claim # 4202041 Joint Venture: Kalahari Buckland
Comments: • Keating anomaly is located in a highland setting covered by level till. • Erratics overlie till. • Slopes are variable and this area has the appearance of a large scale topographic
stoss and lee feature. • Two small outcrop exposures of pink weathered quartz feldspar outcrops were
tound within the area of interest. • A very magnetic diabase float or sub-crop was located near anomaly centre, • A reference sample rx81702 was collected from this outcrop(?). • The cause of the Keating anomaly remains unexplained due to extensive till and
insufficient outcrop exposure within the target area.
Recommendations: • Take till samples down-ice for kim detection. • No grid and magnetometer surveying is recommended.
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Waypolntor Zone Nad27 Nad27 Rock or Sample Magnetic Acid Test Comments Twp Joint Venture claim date
Sample# NAD27 Eastlng Northing Type
JL_03S 17 295585 5326768 felsic gneiss Outcrop of felsic gneiss. Well exposed silty, sandy,
Buckland Kalahari
4202041 12-0ct-06 cobble I pebble till. Bu_06 traverse Buckland
Till slope at 10·N, -1soE with felsic gneiss erratics. Kalahari
JL_043 17 295S52 5327016 Large scale topographic stoss and lee feature. BUckland Buckland
CanMapi!!), DMTI spa.lt'.e DMTI Spatial logo are tmdemarks of DMTI Spatiellnc" Markham, Ontario, @Germln ltd, or Its su.es 1995,2004, e2003 DMTt Spatiatlnc.
L~_~ overzoom - .. '~ ... _. ~ "-_. ~ ~-- .
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Waypoint or Zone Nad27 Nad27 Rock or Sample Magnetic Acid Test Comments Twp Joint Venture dale
Location: Del 02 Name(s) : Frank Longpre & Stephen Polson Date: October 7, 2006 Datum : NAD 27 UTM Zone: 17U Easting: 292570 Northing: 5329201 Township: Delmage Claim # 4202034 Joint Venture: Kalahari Buckland
Comments: • The centre is located within a round depression occupied a cedar swamp. • The uplands bordering this feature are Gneiss. • Most of the Gneiss is rather felsic some xenoliths of a more mafic nature were
observed within the Gneiss. • One ultramafic boulder was sampled en-route to the target.(81613).
Recommendations: • Owing to the fact that the target occupies a round depression it ought to be
Waypointor Zone Nad27 Nad27 Rock or Sample Magnetic Acid Test Commente Twp Joint Venture datil
Sample# NADZ7 Eastillg Northlng Type
DAN_153 17 291065 5327071 granite
magnetic ·'ve gneiss and diabase contact De/mage Kalahari
4-0ct-06 gneiss Buckland
DAN_154 17 290790 5327097 granite
magnetic -'ve Delmage Kalahari
4-0ct-06 gneiss Buckland
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Location: Del 04 Name(s) : Frank Longpre & Stephen Polson Date : October 8, 2006 Datum : NAD 27 UTM Zone: 17U Easting: 292090 Northing: 5327720 Township: Delmage Claim # 4202043 Joint Venture: Kalahari Buckland
Comments: • The magnetic anomaly may be explained by the occurence of strongly magnetic
E/W trending diabase outcrops within a terrain of non magnetic, rather felsic gneiss.
• No samples taken.
Recommendations: • As the source of the magnetic response is diabase and no other rock types but
!:,:rneiss was observed, this target should not be followed up further.
FL_193 17 291699 5324256 granite non-magnetic -'ve ole/ by creek granite extenSive ridge strike 272c Delmage Kalahari
S-Oct-06 Buckland
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Location: DelIO Name(s): Frank Longpre & Stephen Polson Date: October 10, 2006 Datum: NAD 27 UTM Zone: 17U Easting: 294470 Norhting: 5324700 Township: Delamge Claim # 4202054 Joint Venture: Kalahari Buckland
Comments: • The centre is located at the lake shore and the lake could not be crossed, thus the
part of the target was explored. • One diabase outcrop was observed, the remaining outcrop (:overage was of felsic
gneiss. • Large areas are overlain by till with exceptional numbers of erratics. • No samples taken.
Recommendations:
• As the cause of the anomaly could not be ascertained due to water cover, this target should be gridded when ice cover is sufficient and magnetometer survey conducted.
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Way point or sample location Sample
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Target Oel_10(low) Deimage Township October 10, 2006
Target Name: VTEM 76 August 13,2008 4202034 Delmage
Date: Claim#: Township: Joint Venture: Kalahari auckland Name(s): Erik Petersen, Mark Dufuah, Ryan Brown Center of Target: Zone: 17U Easting: 292770mE Northing: 5328506mN
NAD27 Datum:
Equipment used: Truck( I ), A TV
Access to Area: • Travel south on Hwy 65 J for 27 km from M issanabie to Dalton • Travel 19 km west on logging road • Travel 9 km South to closest spot to VTEM 76 • Travel 1.7 km southwest on foot to center ofVTEM 76
Comments: • Granite, granitic gneiss, and meta-sediments were the main types of rocks that were
found in the area. Some gabbro was found as well as a couple of diabase boulders as seen at EP 215.
• At Vl'pt EP _219, there is an outcrop of granite with a quartz vein that has visible cubic sulfides.
• The vegetation in the area was mixed bush w;th certain areas consisting of mainly jack pine or birch.
• Found large outcrop at MD_.234 facing and sloping to the north . Outcrop is granitic composed mostly of micas and quartz. Medium grained, non magnetic, and no reaction with acid.
• Moving north from the centre of the VTEM the elevation is drooping significantly. Once you get to the bottom there is a small creek flowing east.
• South of the target most outcrops are mica-rich meta-sedimentslbanded gneisses
Recommendations: VTEM 76 does not need to be prospected any further.
ASSAY TYPE
Waypoint UTM NAD27 NAD27 KIMS 18 lEl Caustic or Sample # Zone Easting Northing EP 21 4 17 292733 5328520 EP 21 5 17 292729 5328563 EP 21 6 17 292706 5328644 EP 217 17 292603 5328615 EP 21 8 17 292555 5328620 EP 21 9 17 292586 5328583 EP 220 17 292678 5328521 EP 221 17 292544 5328537 MD 233 17 292813 5328536 ._ .
RB_023 17 292844 5328402 very felsic coarse grained granite on top of mica rich
Oelmage Kalahari
4202034 13-Aug-08 gneiss. Buckland
so far around centre and just North of VTEM , have Kalahari
MO_233 17 2928i3 5328536 boulders only seen a few granite boulders, lots of moss and Oelmage Buckland
4202034 13-Aug-OB overburden on ground.
Found outcrop facing and sloping to the North. 3m
MO_234 17 292790 5328617 outcrop nonmagnetic negative high and mound shaped. Outcrop looks granitic
Oelmage Kalahari
4202034 13-Aug-08 composed mostly of biotite and quartz. Medium Buckland grained.
same outcrop formation (MO_234) , running East to Kalahari
MD_235 17 292819 5328635 outcrop West. Elevation drops as you move North and Delmage Buckland
4202034 13-Aug-08 be increases Moving South. f{
terrian flattens out a bit after a large increase,. Lots Kalahari
MO_236 17 292844 5328517 boulders of downed trees and mossy ground, finding Delmage Buckland
4202034 13-Aug-08 scattered boulders, granitic.
found granitic gneiss outcrop, 3m high mound Kalahari
MO_237 17 292903 5328511 outcrop nonmagnetic shaped, can see quartz, biotite, hornbland and Oelmage Buckland
4202034 13-Aug-08 feldspar ,mixed bush
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• Prospecting and Target Write-up
Target Name: VTEM 77 June 4, 2008 4202045 Delmage
Date: CI2im#: Township: Joint Venture: Kal,Llari Buckland Name(s): Terra Dittenhoffe~', Elizabetil Laidlaw, Dakota Souliere Center of Target: Zone: 17U Easting: 0291186 Northing: 5325019 Datum: NAD27
Equipment used: Truck (I), ATV's (3)
Access to Area:
Drove 27 Ian south on highway 651 fron M issanabie to Dalton Drove approx. 20 Ian east on Bolkow road. Turned off of Bolkow and headed 10 Ian south along logging road to Delmage township and within 200m of the target.
Comments:
Disseminated sulphides found in a schist (amphibolite?) outcrop 275m NNE of the target. (see WPT EL.(76) Rolling topography. Mixed coniferous and deciduous vegetation ranging from moderately thick stands of pine and birch to alder swamps. Swamp located in the NW section of the grid surrounding Della lake. Predominant rock type in area was granite. No samples taken.
Recommendations: The Cause of this anomaly was not found; The target centre is well removed from Della
Lake, and the signature form the VTEM indicates a nat lying to shallow dipping conductor. Dipping to the southeast. Disseminated sulphides were found in one outcrop but not enough to explain the anomaly. Follow up prospecting is recommended.
ASSAY TYPE
Waypoint UTM NAD27 NAD27 KIMS IH lEI Caustic or Sample # Zone Easting Northing DS 164 17 291493 5325832 DS 165 17 291484 5325746
=:--=-:1 ••• I. \ ..... /{ I 'It"L •.• ==--=1..::.64..:..1 \ OS 176 , \ . ,,- ./. .... ~ •.•• \
Dell ' -ke'" • . . ....... /1' ~ , I , • a La " EL 163" Ii \. -::::::.--. \0. .. . \ · . . Ti ' ~ :. J. • • J \' .".. !tEL l= ,e JEL 1741. ,_ \
T '-.-.. ~"'-~ ':t . • I ~ r • '~~.-'~~. ! .I lJDS 1711 i ~. ·l ~ ~\
,. EL 162 ~ } ~ , I ,;,
JI":J'""0~P=79="I , f \0 075 .~. j OS ''''J nO 067JEL 1661 ~ • ~l>S 1~5ij. • 451 \-~TO 0711 I I ~ ~. . · ./ ., I .... \ .)l1li • , ~ I " Yf". .! I • • • . ' • , • • • I
I . ../ ... ~ w. •. -. l ~ I I \ JI ~, •. no 0761 • i ~.~ "\iEL 1?31 '. 1· w.
... ~w I . • ~'. v i \ • ( " • • it I • • w' I w1 • \ \ I. w ~ I \ . :. ~ ~ ~.. 'JEL 176\ \t j EL 1721 .it ~ • • .~ ~TO 0761 .. \ , r" j EL 167\ I i ~ EL 161 ;. \ / ·l . JOS 166\ I l . ,. I.' i ~ • , I r I r ! . ~ ) w ·'t fOS 164\
TO_073 17 291197 5326219 bog bog , lots of moss jackpine tree stand. Delmage Kalahari
4202045 4-Jun-08 Buckland
marsh bog approx 100m W oflake marsh bog area , lots of Kalahari ~
TD_074 17 291059 5326188 nonmagnetic negative Oelmage 4202045 4-Jun-08 "" area moss coverage, granite boulders covered by moss Buckland
TD_075 17 291078 5326021 granite
nonmagnetic negative granite boulders, tag alders. Delmage Kalahari
4202045 4-Jun-08 boulders Buckland
TO_07S 17 291056 5325891 granite
nonmagnetic negative granite boulders 1 m x 2m x 4m. Delmage Kalahari
4202045 4-Jun-08 boulders Buckland
TO_077 17 290923 5325673 granite
nonmagnetic negative jackpine tree stand . Delmage Kalahari
4202045 4-Jun-08 boulders Buckland
TO_078 17 290891 5325952 granite
nonmagnetic negative granite boulders x 7 ,1m x 1 m , area of mixed
Oelmage Kalahari
4202045 4-Jun-08 boulders forest. Buckland
TO_079 17 290935 5326032 nonmagnetic negative swampy bog area tall grasses tag alder 3 jackpine ,
Oelmage Kalahari
4202045 4-Jun-08 swampy area small granite boulders. Buckland
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Target Name: Date: Claim#: Township: Joint Venture: Name(s): Center of Ta rget: Datum:
Equipment used:
Access to Area:
Prospecting and Target Write-up
VTEM_77 - tol\OIUUf -(2nd 'PQ.~s) July 19,2008 4202045 Delmage Kalahari Buckland Katy Richard, Ryan Brown & Josh Guthrie Zone: 17 Easting: 0291160 Northing: 5325935 NAD27
Truck( 1), Al-V
• Travel 27 km south on Hwy. 651 to Dalton • From Dalton, travel 20 krr_ east on Goldie River Rd _ • At junction, tum south on Bolkow Rd. for 13.5 km • Another old logging road was traveled for 800m heading east to the access point where
prospecting by foot began; the target center is located 170m south of the road .
Comments: • Vegetation was primarily mixed forest of a middle age; however, in places there were areas
consisting almost exclusively of balsam, jack pine, and spruce. Most of the bush surrounding the anomaly was very open and free of undergrowth .
• Topography was variable with small hills and small wet areas. • Based on a series of subtle features shown on the EM profile, it was thought that a conductor may
surface somewhere on the northwest facing slope of a large hill (summit approx 350m east of the target center). A sweep of this area revealed both large boulders and some outcrop composed granite pegmatite with patches of quartz. Sulfides were present in a few cases (disseminated, and sometimes rimming mafic fragments within the rock). No massive sulfide indications were found.
• Granite and gneiss were the predominant rock type encountered as well as several large diabase dykes found south of the VTEM anomaly.
• Approximately 60m NE of the target center, an elongated gabbroic outcrop (40m) was encountered. One particular section contained felsic inclusions/mineral clusters and very few sulfides. This rock was non-magnetic nor reactive to acid.
• Southeast of the anomaly, several flat-lying granite, granitic gneiss, and banded gneiss outcrops were found with boulders of similar material scatterec on top. Outcrops run east-west. On one of these outcrops several boulders of granit( pegmatite were found containing massive chlorite inside.
• West of the anomaly a granite pegmatite erratic was found with 20cm-wide quartz veins; upon further inspection, the vein was barren as no sulphides or other minerals of interest were visible.
• One flat-lying diorite outcrop containing 0.5cm, sheeted, pyroxene crystals was found running east-west approximately 85m west of the anomaly 's centre.
Recommendations:
• No conductive material-- Dnly granite, granite pegmatite, gneiss and diabase were found surrounding the VTEM; therefore, the anomaly remains unexplainec. Because of this, perhaps the target should be considered for drilling.
ASSAY TYPE
Waypoint UTM NAD27 NAD27 KIMS IH lEI Caustic or Sample # Zone Easting Northing JO 208 17 0291492 5325999
45
• JO .. 209 17 0291497 5326056 J0210 17 0291397 i 5326127 J0211 17 0291352 5326100
KR_521 17 290956 5325933 boulder granite pegmatic erratic 1 m X 2m X 3m, mixed
Delamge Kalahari
4202045 19-Jul-08 bush, 200m West ofVTEM_77 Buckland
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Rock Sample Results
A total of 1 sample was run for analysis by True North Mineral Laboratories Inc, located in Timmins ON. Samples are presented in: Appendix 1: - True North Mineral Laboratories Inc.Actlabs - for the detailed analysis of each sample and the attached Certificate of Analysis
For the current work report the rock sample sites are plotted on Traverse waypoints and samples locations map accompanying each target area overview.
ReCCllmmendations
Comprehensive interpretation and presentation of all the geochemical analysis data; combined with the interpretation of VTEM airborne survey flown in winter of 2007-2008.
The results and interpretation of the above noted compilations will dictate the approach to further field work.
Qualifying Statement
I, Claudia Wilck, residing at RR #1, Parry Sound, ON, P2A 2W7 state the following with respects to this report:
I wrote this report and produced the accompanying tables and maps based on information provided by Chalice Diamond Corp. of 771 - 675 West Hastings Street Vancouver, British Columbia V6B 1 N2.
That I hold no beneficial interest in these properties held by Chalice Diamond Corp. as stated in this report.
Respectfully Submitted
~lJhL Claudia Wilck Geological Technician
51
in Parry Sound, ON 26, September, 2008
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References
First Vertical Derivative of Magnetic Field with Keating Coefficients Map Dumont R, Coyle M., Potvin J., Geological Survey of Canada, 2001 Ontario: Bolkow, NTS 42 B/4 Open File 40641 OGS Map 81 707
Ontario airborne geophysical surveys, magnetic data, Wawa area; Ontario Geological Survey, Geophysical Data Set 1009 - Revised 2003
Bennett, Gerald, 1978: Geology of the Crooked Lake Area, District of Sudbury; Ontario Geological Survey Report 172, 46p. Accompanied by Maps 2380 and 2381, scale 1 inch to % mile
The following analytical package was requested: Code 1E1 Aqua Regia ICP(AQUAGEO)
REPORT A06-4496
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.
Notes: Values which exceed the upper limit should be assayed for accurate numbers.