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Home My WebLink AboutGMC Data Report No. 320Summary results of short-wave infrared spectroscopy of the gold bearing drill cores from Centennial, Propalof, Red Cove, and of auger samples from the Orange grid; all of Popof Island of Southwest Alaska. v ~ Received 14 September 2005 Total of 17 pages in report Alaska Geologic Materials Center Data Report No. 320 Summary Results of Short-wave Infrared Spectroscopy, Popof Island, Alaska Analysis of Drill Core: Centennial, Propalof, Red Cove Analysis of Auger Samples: Orange Grid July 6, 2005 Prepared for: Bill Ellis Alaska Earth Sciences Inc. 11401 Olive Lane Anchorage, Alaska United States, 99515 PetraScience Consultants Inc. 700 - 700 West Pender St. Vancouver, B.C. V6C 1G8 Canada Phone: 604.684.5857 Fax: 604.222.4642 info@petrascience.com page 1/17 www.petrascience.com GMC DAl'A RCPORT 3 2 0 Mapping alteration with reflectance spectroscopy: Popof Island, Alaska Background Samples from several project areas on Popof Island, Alaska were analyzed on June 14, 2005. The samples are part of a collection stored at the Alaskan Geological Materials Repository in Eagle River, Alaska. Anne Thompson of PetraScience Consultants Inc., Vancouver, B.C., carried out the analyses on site at the warehouse. Sketch maps were available of the areas, but no site visit was made and the project geologist was not available for discussions regarding the samples. The analyses were carried out with aPIMA-SP spectrometer. Results were previously reported in excel spreadsheets via email. This report summarizes the basic variations observed. Also included is a brief description of the technique. Summary The analysis successfully helped to identify a variety of alteration minerals including the following: smectite (including montmorillonite, and likely beidellite), illite, chlorite, dickite, kaolinite, illite, kaolinite, prehnite, pyrophyllite, alunite (rare) and carbonate. In particular, the following observations were made for each of the areas: Centennial The alteration mineralogy observed in the Centenniel drill core is characterized by the presence of chlorite, illite, epidote and calcite. Prehnite was also observed in a couple of samples. Gypsum is common, likely as the result of weathering of fine pyrite in the core during storage. Where present the illite appears to vary in composition from phengitic to more potassic compositions as defined by a wavelength shift in the AI-OH position at approximately 2200nm. The majority of the illite is characterized by a wavelength position of 2212-2216nm (phengitic). A few samples, however, have much lower values, e.g. -2198nm. The lower wavelengths, in some deposits, may be associated with mineralization. Propalof Only a handful of samples were analyzed from the Propalof core. One drill hole (03) was available at the warehouse, and visual inspection of the core suggested much of it consisted of relatively fresh rock. Small zones of veining in the core contained quartz and carbonate (calcite and dolomite). Minor montmorillonite and kaolinite were also observed. Red Cove The alteration at Red Cove contains zones of advanced argillic minerals including pyrophyllite and alunite. Broadly the alteration includes zones of alunite, pyrophyllite-dickite, kaolinite, outwards to illite, and montmorillonite or beidellite -chlorite. Beidellite is an AI-rich smectite-group mineral. Orange Grid Montmorillonite, illite, kaolinite, dickite, chlorite, and likely carbonate are common in the auger samples from the Orange Grid. Dickite appears to group in an area within the grid, and may be of interest if it correlates with variations in the geochemistry. In general, the chip samples are more difficult to analyze, particularly as the majority of samples appeared inhomogenous, with both possible altered chips and fresh rock mixed together. The smaller the amount of clay present, the more reduced the signal will be, causing a flat and unresponsive pattern. Many of the samples shown as "?Silica" may be a reflection of a dominant amount of fresh rock in the sample. These samples essentially showed up as flat lines on the spectrometer. Page 2/17 6MC DATA REPORT 3 2 0 Anne J.B. Thompson, P.Geo. 2 Mapping alteration with reflectance spectroscopy: Popof Island, Alaska Reflectance Spectroscopy Short-wave infrared spectroscopy detects the energy generated by vibrations within molecular bonds. These bonds have bending and stretching modes within the 1300 to 2500nm region of the electromagnetic spectrum. The observed absorption features represent the first and second overtones and combination tones of fundamental modes that occur in the mid-infrared region. The positions of the features in the spectrum and their characteristic shapes are a function of the molecular bonds present in the mineral. A typical. spectrum consists of several characteristic features including the hull (background), wavelength position, feature depth and width. Variations in chemical composition may be detected as the wavelength positions of features shift consistently with elemental substitution. The SWIR range. is particularly responsive to a variety of molecules and radicals typical of alteration minerals, including OH, H2O, NH4, CO3, and cation-OH bonds such as AI-OH, Mg-OH and Fe-OH. Mineral identification is based on feature positions, Intensity and shape of absorption troughs and the overall shape of the entire spectrum. The short-wave infrared wavelength region is not suitable for most anhydrous silicates, however some important features may be visible for individual minerals in the VNIR, where variations in iron and chromium are observed. In order to accurately identify minerals, high quality reference data sets are required (e.g. Hauff, 1993). These references constitute empirical records of a mineral's characteristic spectra. Visual observation of a group of spectra for a given mineral will quickly show variations based on numerous factors, including mineral chemistry, temperature, mode of formation and other subtle changes. The positions of the features in the spectrum and their characteristic shapes are a function of the molecular bonds present in the mineral. Variations in chemical composition may be detected as the wavelength positions of features shift consistently with elemental substitution. SWIR spectroscopy is partly sensitive to crystallinity variations, but may not detect primary changes in the lattice structure. Atypical spectrum consists of several absorption features. Figure 1 below illustrates the various aspects of an absorption feature, including wavelength position, depth and width (full height, half width maximum). The outline of the hull or continuum is also shown. HWI ~, InON A FOYU10 Paltlan (OOU710t) 1700 1107 1000 II00 7100 WpdOrpth (nlll) NAM A Hull R ~~. ~OPIA f1N HM PaltlOn 1000 71pp 7Jd0 WaMIOnpM (nm) Figure 1, Elements of a reflectance spectrum, including hull, wavelength position and depth. GMC DATA REPORT 3 2 0 Page 3/17. Anne J.B. Thompson, P.Geo. Mapping alteration with reflectance spectroscopy: Popof Island, Alaska Each sample is typically analyzed twice and every analysis uses gold. reflectance calibration. Wavelength calibration was carried out approximately every 5°C change in temperature. Mineral identification was verified using references from the Spectral Library, SPECMINT"' and compared using overlays in FeatureSearch 1.6 (SIMIS Solutions). Representative plots in this report were made using SpecWin. Examples of the minerals identified in the samples are shown in Figure 2. Typically, in order to achieve high quality results, spectral variations at the deposit-scale must be observed and recorded by the user. Identification of complex mixtures requires geological context, user experience and establishment of reference samples with supporting mineralogical information from other analytical techniques. 1.20a4 1,OOe4 Q1 () 8000• C U 4- ~ 6000 O N G7 a- 4000• 2DD0• D.0 Wavelength {nm) D6000PI.DSP KAOLCUP2.OSP PYROGA1,dap ILLCUPI.DSP MDNTCAS.dep Figure 2. The spectra shown above are references (top to bottom); chlorite, dickite, kaolinite, pyrophyllite, illite, and montmorillonite. GMC DATA REPORT 3 2 Q ~~ CHI.RCAN1.dap Page 4/17 Anne J.B. Thompson, P.Geo. 4 1400 1600 1800 2000 2200 2400 Mapping alteration with reflectance spectroscopy: Popof Island, Alaska References Hauff, P.L., 1993, SPECMINT"" Mineral Identification System and Spectral Library, v. 1 & 2.: Arvada, Colorado, Thompson, A.J.B., Hauff, P.L., and Robitaille, A.J., 1999, Alteration mapping in exploration: Application of short-wave infrared spectrospopy: Society of Economic Geologists' Newsletter, v.39, 13pp. Thompson, A.J.B. and Thompson, J.F.H., 1996, Atlas of Alteration: A Field and Petrographic Guide to Hydrothermal Alteration Minerals: Geological Association of Canada, Mineral Deposits Division, 119p. GMC DATA REPORT 3 2 0 Page 5/17 Anne J.B. Thompson, P.Geo. v n --1 n m -v O w N 0 -v in rn V ~traScience Conrultants Inc. Centenniel 7/10!2005 Drill Hol Depth File Name Mineral 1 Mineral 2 Mineral3 Description CEN 01 21 AES_CEN00001 Prehnite Montmorillonite green, hematitic red AES_CEN00002 Prehnite Montmorillonite 0.17oz. Au, green, hematitic red ,white fracture fill, no-response ma 70 AES_CEN00003 Chlorite ?Calcite pale green white fracture fill, AES_CEN00004 Chlorite ?Calcite pale green white fracture fill, 95 AES_CEN00005 u/r pale Teen ,hard, minor white in vugs AES_CEN00006 u/r pale green ,hard, minor white in vugs 119 AES_CEN00007 Calcite ?Chlorite pale green ,hard, centred on white veinlet AES_CEN00008 u/r pale green ,hard, groundmass 150 AES_CEN00009 Chlorite (M pale, pale green ,groundmass, diss sulfides AES_CEN00010 Chlorite Mg pale, pale green ,groundmass, diss sulfides 169 AES_CEN00011 Epidote pale, pale green ,groundmass, diss sulfides AES_CEN00012 Epidote pale, pale reen ,groundmass, diss sulfides 179.5 AES_CEN00013 Prehnite Montmorillonite white to pale green groundmass of breccia, clasts red/grey AES. CEN00014 Prehnite Montmorillonite white to pale green groundmass of breccia, clasts red/grey 252 AES_CEN00015 u/r white to pale green groundmass, homogeneous, fine-grained AES_CEN00016 G sum minor white to pale green groundmass, homogeneous, fine-grained 258.5 AES_CEN00017 Chlorite white to pale green groundmass, green spots, fine-grained AES_CEN00018 Chlorite Epidote white to pale green groundmass, green spots, fine-grained 350 AES_CEN00019 Quartz white to pale green fracture surface, hard AES_CEN00020 G psum white to pale green hard, homogeneous 358 AES_CEN00021 ?tr Chlorite white veinlet in hard, rey, red spots AES_CEN00022 ?tr Chlorite hard, gre ,red spots 442 AES CEN00023 Chlorite Montmorillonite pale reen, white splotches AES_CEN00024 Chlorite Montmorillonite pale green, white splotches mostly white 499 AES_CEN00025 u/r pale green, hard, fine-grained AES CEN00026 Calcite pale green, hard, fine-grained fracture surface CEN 03 41 AES_CEN00027 u/r fine pink and green alteration, dominantly pink AES_CEN00028 u/r fine pink and reen alteration, white vug-quartz? 58 AES_CEN00029 Illite ?Quartz 2204 white to yellow-brown weathered AES_CEN00030 Montmorillonite Kaolinte 2210 white to ellow-brown weathered 101 AES CEN00031 Illite Kaolinte ?Chlorite 2210 green, white with hematite AES_CEN00032 Illite Chlorite ?Carbonate 2212 green, white with hematite broken surface 133.5 AES CEN00033 Chlorite ?Calcite green, minor white clear crystals, broken surface AES_CEN00034 Chlorite ?tr Calcite green, broken surface 155.5 AES_CEN00035 Illite G sum 2214 pale tan, to green, irregular stringers, unweath version 58 AES_CEN00036 Calcite Tr. G psum ,white patches irregular stringers, unweath version 58 AES_CEN00037 Illite G psum 2212 ,white patches irregular stringers, .scraped groundmass Anne J.B. Thompson, P.Geo. v -n-i D m -v O w N 0 v c~ V v I~traScience Cnnru/tantr Inc. Centenniel 7/10/2005 Drill Hol Depth F File Name Mineral 1 Mineral 2 Mineral3 Description 262 AES_CEN00038 ?G psum white, reen, homogeneous AES_CEN00039 ?G psum white, green, homogeneous 357 AES CEN00040 u/r green, homogeneous hard AES_CEN00041 u/r green, homogeneous hard CEN 07 43 AES_CEN00042 u/r green, grey homogeneous hard AES_CEN00043 Prehnite green, rey homogeneous hard outside surface 66 AES_CEN00044 u/r green, grey homogeneous hard broken surface AES_CEN00045 u/r reen, grey homogeneous outside surface 109 AES_CEN00046 ?Epidote/clinozoi site green, grey hom eneous fresh broken sulfides AES_CEN00047 ?Epidote%linozo isite green, grey hom eneous fresh broken sulfides 129 AES_CEN00048 Chlorite -Mg pale green, rey homogeneous broken surface AES_CEN00049 Chlorite -M pale green, grey homogeneous flat surface 194 AES_CEN00050 Chlorite - M pale green, grey homogeneous flat surface AES_CEN00051 Chlorite - Mg pale green, grey hom eneous flat surface 354 AES_CEN00052 ?Chlorite white, grey green, sulfides irregular AES_CEN00053 ?Chlorite white, rey green, sulfides irregular no fizz 485 AES_CEN00054 Illite ?tr G sum 2214 white, soft, re extremely altered AES_CEN00055 Illite G psum 2208 white, soft, grey extremely altered sawn surface 489 AES_CEN00056 Chlorite white,hard, sulfides, gre broken surface AES_CEN00057 Chlorite tr G psum white,hard, sulfides, greysawn surface 512 AES_CEN00058 Chlorite - Fe-Mg white,gre reen clasts, sulfides, dominantly green ctast AES_CEN00059 Chlorite - Fe white,grey green clasts, sulfides, fresh green clast 589.5 AES_CEN00060 Chlorite - Mg fine grained green AES CEN00061 Chlorite - M fine grained green CEN 11 26 AES_CEN00062 u/r fine grained green-pink (?K-spr) AES_CEN00063 Montmorillonite fine grained green-pink(?K-spr) 93 AES_CEN00064 ?Quartz fine grained green-pink ,white veinlet fizzes AES_CEN00065 Quartz fine grained green-pink ,white tan area 131 AES_CEN00066 Quartz fine grained green-white, homogeneous, sandy AES_CEN00067 G psum ?Quartz fine rained reen-white, homogeneous, sandy 274 AES_CEN00068 Montmorillonite Chlorite Quartz? fine grained reen-white, homogeneous, soft, sulfides AES_CEN00069 Quartz tr G sum fine grained reen-white, homogeneous, soft, sulfides 427 AES_CEN00070 Illite ?G sum 2196 fine grained, black AES_CEN00071 Illite ?G psum 2196 fine grained, black 508 AES CEN00072 Illite 2212 end of hole, white, soft, green clasts Anne J.B. Thompson, P.Geo. n D b m O ~v -1 w N 0 v m ao v RtraScience Conrultantr Inc. Centenniel 7/10/2005 Drill Hol Depth F File Name Mineral 1 Mineral 2 Mineral3 Description CEN 14 39.5 AES CEN00073 ?Calcite u/r grey reen fine-grained sandy AES_CEN00074 ?Calcite ?Chlorite ?lllite grey green fine-grained sandy sawn surface 89 AES_CEN00075 Chlorite Calcite Montmorillonite grey green fine-grained sandy broken surface, fine cc veinlet AES_CEN00076 Chlorite Calcite Montmorillonite grey green fine-grained sandy broken surface, fine cc veinlet 121.5 AES_CEN00077 Montmorillonite Chlorite clast in sandy matrix,white green no fizz AES_CEN00078 G psum clast in sand matrix,dominantly matrix material 149 AES_CEN00079 Calcite Montmorillonite ?Chlorite grey green fine-grained AES_CEN00080 Calcite tr Montmorillonit ?Chlorite grey green fine-grained sawn surface 207 AES_CEN00081 ?Chlorite grey reen fine rained sawn surface, volcanoclastic? AES_CEN00082 Chlorite ?Montmorillonite Calcite rey green fine-grained fresh surface, fragments, gentle fizz 282 AES_CEN00083 Chlorite white, grey-gm soft with sulfides fragmental AES_CEN00084 Chlorite white, grey-gm soft with sulfides fragmental fresh surface 378 AES_CEN00085 u/r grey green, fragmental fine fractures AES. CEN00086 Montmorillonite Chlorite 2210 grey green, fragmental sawn surface 483.5 AES_CEN00087 lllite Chlorite 2216 white grey, extremely soft minor sulfides? AES_CEN00088 G psum Chlorite lllite 2214 white gre ,extremely soft minor sulfides? strong fizz in brown staff AES_CEN00089 lllite Chlorite G psum 2216 white gre ,extremely soft minor sulfides? strong fizz in brown staff 499 AES_CEN00090 u/r black, fine-grained AES_CEN00091 u/r black, fin rained fresh 555.5 AES CEN00092 _ Chlorite - Fe pale green sand, end of hole AES_CEN00093 Chlorite - Fe pale green sand, end of hole no fizz CEN 41 17 AES CEN00094 lllite ?G psum 2210 white, yellow, weathered AES_CEN00095 lllite 2210 white, yellow, weathered 24 AES_CEN00096 lllite 2210 white, grey clasts, moderately soft AES_CEN00097 lllite 2210 white, grey clasts, moderately soft 41 AES_CEN00098 lllite G psum ?Quartz 2214 white, grey clasts, grey matrix, 0.066 Au opt, soft AES_CEN00099 lllite 2216 white, grey clasts, grey matrix, 0.066 Au opt, fracture white surface 48 AES_CEN00100 lllite Chlorite 2216 clasts, fragmental white, grey AES_CEN00101 lllite Chlorite 2214 clasts, fragmental white, grey 73 AES_CEN00102 Chlorite lllite 2216 green, white, bleached AES_CEN00103 Chlorite lllite 2216 reen, white, bleached 78 AES_CEN00104 lllite G psum ?Carbonate 2212 green, white, bleached, brown stain with fizz AES CEN00105 lllite G sum ?Carbonate 2216 green, white, bleached, brown stain with fizz 111 AES_CEN00106 Montmorillonite Chlorite 2212 ?fragmental, pale green, white, AES_CEN00107 Montmorillonite Chlorite 2208 ?fragmental, pale green, white, 131 AES_CEN00108 lllite 2214 adjacent min zone, pale white, grey, sandy bleached fragmental AES_CEN00109 lllite Chlorite 2210 ad~acent min zone, pale white, grey, sandy bleached fragmental Anne J.B. Thompson, P.Geo. r~ n n m 0 ~v -i r~ N 0 v sv rp V IltraScience Conrultantr Inc. Centenniel 7/10/2005 Drill Hol Depth F File Name Mineral 1 Mineral 2 Mineral3 Description 147 AES_CEN00110 Illite Chlorite 2214 adjacent min zone, ale white, soft grey, bleached fragmental AES_CEN00111 Chlorite Illite 2214 adjacent min zone, pale white, soft grey, bleached fragmental 167 AES_CEN00112 Montmorillonite ?Chlorite 2208 white, green, hard AES_CEN00113 Montmorillonite ?Chlorite 2202 white, green, hard 200 AES_CEN00114 ?Quartz tr. ?Montmorillo green grey, homogeneous, hard AES_CEN00115 ?Quartz tr. ?Montmorillo green grey, homogeneous, hard 248 AES_CEN00116 Chlorite G psum green grey, homogeneous, hard, sandy AES_CEN00117 Chlorite G psum green grey, homogeneous, hard, sandy fresh surface no fizz CEN 57 10 AES_CEN0o118 Chlorite - Fe ?Kaolinite tan, yellow-green moderately soft AES_CEN00119 Chlorite - Fe ?Kaolinite tan, yellow-green moderately soft minor fizz 18 AES_CEN00120 Chlorite - Fe tan, yellow-green moderately soft AES_CEN00121 Chlorite tan, yellow-green moderately soft 24 AES_CEN00122 Quartz ?tr Chlorite tan, yellow-green moderatel soft ,irregular green zone AES_CEN00123 Quartz tan, yellow-green moderately soft ,irregular tan zone 35 AES_CEN00124 Illite 2204 white, virtually pure clay zone AES_CEN00125 G psum Illite 2212 grey zone with ?sulfides 10cm away 45 AES_CEN00126 Chlorite Montmorillonite grey-green homogeneous AES_CEN00127 Chlorite Montmorillonite 2212 grey-green homogeneous sawn surface, filed 58 AES_CEN00128 G psum ?Chlorite grey~reen fragmental, broken end AES_CEN00129 Chlorite grey-green fragmental, filed flat surface 86 AES_CEN00130 Chlorite grey-green fragmental, filed flat surtace AES CEN00131 Chlorite rey-green fragmental, filed broken surface 115 AES CEN00132 Chlorite Montmorillonite 2208 grey-green fragmental, broken surface AES_CEN00133 Chlorite Montmorillonite 2209 grey-green fragmental, filed sawn surface 136.5 AES_CEN00134 Chlorite ?Epidote grey-green fragmental, filed sawn surface AES_CEN00135 Chlorite ?Epidote ?Montmorillonite gre -green fragmental, broken surface 156 AES_CEN00136 u/r grey-green, grey cores, hani, green matrix AES_CEN00137 ?tr Chlorite grey-green, grey cores, hard, green matrix, minor fizz 162 AES_CEN00138 u/r grey-green, sandy, homogeneous AES_CEN00139 u/r gre reen, sandy, homogeneous 168.5 AES_CEN00140 ?Montmorillonite ?Chlorite grey-green, homogeneous hard AES_CEN00141 Prehnite ?G sum grey-green, fracture surface AES_CEN00142 Prehnite grey-green, fracture surface 196 AES_CEN00143 u/r grey-green, sandy, fragmental AES_CEN00144 u/r gre -green, sand ,fragments sawn surface 229 AES_CEN00145 u/r grey-green, broken surface, hard AES CEN00146 u/r grey-green, sawn surface G7r n n m -v O w N 0 Anne J.B. Thompson, P.Geo. 3 n m -v O u N 0 v cn 0 V IltraScience Consultants Inc. Centenniel 7/10/2005 Drill Hol Depth F File Name Mineral 1 Mineral 2 Mineral3 Description 259 AES_CEN00147 u/r grey-green, end of core ' AES_CEN00148 u/r gre reen, filed, flat ' ~ 287.5 AES_CEN00149 ?Calcite grey-green,fracture surface with ?cc AES_CEN00150 ?Chlorite Montmorillonite grey reen, filed surface CEN 58 17 AES CEN00151 Chlorite - M grey green sandy ~ 38.5 AES CEN00152 AES CEN00153 ` u/r ?Chlorite ?Montmorillonite - grey green sandy, filed grey green-yellow sandy CEN00154 AES ?Chlorite ?Montmorillonite grey green-yellow sandy 71.5 AES CEN00155 G psum ?Illite 2222 grey reen fragmental, sandy AES CEN00156 G psum ?Illite 2222 grey green fragmental, sandy 100 AES CEN00157 ?G psum gre reen fragmental, sandy AES_CEN00158 ?G psum grey green fragmental, sandy 134 AES_CEN00159 u/r grey green fragmental, sandy CEN00160 AES u/r grey green fragmental, sandy 153 _ CEN00161 AES Zeolite grey green, white multiple veinlets _ AES_CEN00162 Zeolite grey green, white multiple veinlets, end of core 169 CEN00163 AES ?Zeolite? grey green, minor white veinlets _ CEN00164 AES ?Zeolite? rey green, minor white veinlets 201.5 _ AES_CEN00165 ?Quartz dark grey, fragmental AES_CEN00166 ?Quartz ,dark grey, fragmental 222 AES_CEN00167 ?Quartz pink, crystalline vein AES_CEN00168 ?Quartz pink, crystalline vein light AES_CEN00169 ?Quartz pink, crystalline vein fizzes 232.5 AES_CEN00170 Illite Chlorite 2210 gre green, sandy fragmental AES_CEN00171 Illite Chlorite grey green, sandy fragmental 271 AES_CEN00172 Chlorite - Fe tr Illite 2214 grey green, mottled., with hematite pink AES_CEN00173 ?Chlorite grey green, mottled, with hematite pink 301.5 AES_CEN00174 ?Chlorite grey green, mottled, with hematite pink AES CEN00175 u/r grey green, mottled, with hematite pink 7 a r w N Anne J.B. Thompson, P.Geo. n n-~ -v O -~-~ w N d v c~ V IdtraSciexce Coxrultaxtt Inc. Propalof 7/10/2005 Drill Hole Depth FT File Name Mineral 1 Mineral 2 Mineral3 wvlgth Description PR 03 11 AES PR 00001 ?Montmorillonite 2210 pale reen, dark green spots AES PR 00002 ?Montmorillonite 2210 pale reen, dark green spots 91 AES PR 00003 ?Kaofinite dark re ,fine-grained AES PR 00004 ?Quartz dark gre ,fine-grained, white veinlet AES PR 00005 ?Quartz Calcite (fizz dark gre ,fin rained, white veinlet fizzes! 125 AES_PR_00006 Calcite Quartz 2336 breccia veinlet in dark- re reen host AES_PR_00007 u/r dark- re reen host 168 AES PR_00008 Quartz ?Montmorillonite 2202 white banded veinlet AES PR_00009 Quartz white banded veinlet AES PR 00010 Chlorite ?Kaofinite dark gre reen host cock 198 AES PR_00011 Calcite Quartz 2336 white banded vein in dark gre -black host AES PR_00012 Quartz Calcite 2332 reen-grey fragment in cc veinlet 256 AES PR 00013 Calcite ?Dolomite 2334 white veinlet, pod in green fine-grained host AES_PR 00014 Dolomite ?Calcite 2324 reen fine-grained host 291 AES PR_00015 Chlorite Illite 2212 pale green-grey with disseminated p AES PR 00016 Chlorite Illite 2214 pale green-gre with disseminated p end of hole Anne J.B. Thompson. n n° a O ---~ w N O v a ca m N v IltraSciente Conrullantt Inc . Red COVe 7/10/2005 Depth FT File Name ~ Mineral 1 Mineral 2 Mineral3 AI-0H wvl th Descri lion 52 AES RC 00001 Kaolinite white, re soft AES RC 00002 Kaolinite white, re soft 74 AES RC 00003 ro h Ilite white, re soft, slick AES RC 00004 ro h Ilite ?Kaolinite white, re soft, slick 103 AES RC 00005 Alunite 1482 white, re soft AES RC 00006 Alunite 1482 Kaolinite white, re soft, broken end 136.5 AES RC 00007 ro h Ilite white, re pale allow stain, soft AES RC 00008 ro h Ilite ?Kaolinite white, re pale ellow stain, soft 171 AES RC 00009 Beidellite 2192 re pale ellow stain, mottled AES RC 00010 Beidellite 2188 re ale ellow stain, fresh surtace 177 AES RC 00011 ro h Ilite ou e, re AES RC 00012 ro h Ilite G sum ou e, re 199.5 AES RC 00013 Illite ?G sum 2197 re , ale ellow, white veinlets AES RC 00014 G psum Illite 2197 re , ale ellow, white veinlets psum 226 AES RC 00015 Illite G psum 2198. re , ale ellow, white veinlets sum AES RC 00016 re ale ellow, white veinlets sulfides 259 AES RC 00017 Beidellite 2188 re , ale ellow, re fractures AES RC 00018 Beidellite 2192 re ,pale ellow, re fractures 276 AES RC 00019 Illite 2194 re ale ellow, re fractures, hard fra mental AES RC 00020 Illite ?Kaolinite 2198 re , ale ellow, re fractures, hard fra mental 312 AES RC 00021 ?Beidellite re , ellow-oran e, sulfides; re fractures, AES RC 00022 Beidellite 2184 re , ellow-oran e, outside core 22.5 AES RC 00023 Kaolinite Smectite re , ri ,soft to of hole AES RC 00024 Smectite Kaolinite re , ri ,soft to of hole 352 AES RC 00025 roph Ilite ?Dickite re , ri ,mottled with minor hematite AES RC 00026 roph Ilite Dickite re , ri ,mottled with minor hematite AES RC 00027 roph Ilite Dickite re , u le veinlet 362 AES RC 00028 Beidellite ?G sum 2192 fra ment with pale ellow fs r, mod soft AES RC 00029 G sum end of core AES RC 00030 Beidellite ?G sum 2190 sawn surface, re - ellow 373 AES RC 00031 Beidellite Kaolinite G sum 2186 banded, tan tuffaceous material AES RC 00032 Beidellite Kaolinite 2188 banded, tan tuffaceous material end of piece 422 AES RC 00033 Kaolinite G sum ?Dickite fine rained, re -pink AES RC 00034 Kaolinite ?Dickite fine rained, re -ink fresh surface 451 AES RC 00035 Kaolinite Beidellite 2180 fine rained, re tan fra mental AES RC 00036 G psum Beidellite. 2180 fine rained, re tan fra mental white veinlet 473 AES RC 00037 G sum Kaolinite white veinlet in re mottled rock with fine re veinlets Anne J.B. Thompson, P.Geo. c: O -~-i N 0 v rn w V ~~ I~traScience Consultants Inc . Red Cove 7/10/2005 Depth FT File Name Mineral 1 Mineral 2 Mineral3 AI-0H wvl th Descri tion AES RC 00038 Illite G sum 2194 re mottled rock with fine re veinlets 504.5 AES RC 00039 G psum Kaolinite re mottled rock with fine sulfide AES RC 00040 G sum Kaolinite re mottled rock with fine sulfide end of core 613 AES RC 00041 Chlorite - M Beidellite hard, re , ink irre ular zones AES RC 00042 G sum ?Beidellite white cket hard, re ink irre ular zones 663 AES RC 00043 Beidellite Chlorite 2184 soft, whit re with sulfide AES RC 00044 Beidellite Chlorite 2184 soft, whit re with sulfide broken end core 680 AES RC 00045. Chlorite - M Beidellite 2182 soft, white- re with sulfide end of hole AES RC 00046 Chlorite - M Beidellite 2183 soft, white re with sulfide end of hole 27 AES RC 00048 ?Zeolite Chlorite re reen, moderate) soft -same as revious 38 AES RC 00047 Chlorite re reen, moderate) soft 47 AES RC 00049 Chlorite Illite 2208 re reen, moderate) hard, homo eneous AES RC 00050 Chlorite Illite 2204 re reen, moderate) hard, homo eneous 89 AES RC 00051 Chlorite ?Beidellite 2194 re reen, moderate) hard, homo eneous, rite veinlet 112 AES RC 00052 Dickite Quartz white, brown vu oxidized AES RC 00053 Dickite . Quartz white, brown vu oxidized 118 AES RC 00054 Dickite Kaolinite white, sand ,with 'te AES RC 00055 Dickite Kaolinite ?tr Alunite white, sand , with p rite 141.5 AES RC 00056 Chlorite ?Smectite 2202 re reen, fin rained AES RC 00057 Chlorite Smectite 2202 re reen, fin rained 175 AES RC 00058 Chlorite-M Beidellite 2188 re reen, fin rained fsprs AES RC 00059 Chlorite-M Beidellite 2192 re reen, fin rained fsprs .200.5 AES RC 00060 Chlorite Illite/?Smectite 2198 re reen, fin rained fs rs AES RC 00061 Chlorite Illite/?Smectite 2198 urple, dark fracture coatin 228 AES RC 00062 Beidellite Chlorite 2192 li ht re reen AES RC 00063 Beidellite Chlorite 2192 li ht re reen 257 AES RC 00064 u/r dark black, fine rained sulfide AES RC 00065 u/r dark black, fine rained sulfide 285 AES RC 00066 Chlorite Smectite/?Illite 2194 re with ellow stain irre ular veinlets AES RC 00067 Chlorite Smectite/?Illite 2204 re with ellow stain irre ular veinlets 311 AES RC 00068 Chlorite Beidellite 2190 re with ellow stain diss p rite AES RC 00069 Chlorite Beidellite 2191 re with ellow stain diss p rite 333 AES RC 00070 roph Ilite Kaolinite Dickite re -white, soft white minor p rite AES RC 00071 ro h Ilite Dickite ?Kaolinite re -white, soft white minor p rite 376 AES RC 00072 Chlorite Beidellite 2192 re reen, minor ellow stain AES RC 00073 Chlorite Beidellite 2194 re reen, minor ellow stain n n° a m -v O W N 0 Anne J.B. Thompson, P.Geo. I~1raScience Canrultantt Inc . Red COVe 7/10/2005 Depth FT File Name Mineral 1 Mineral 2 Mineral3 AI-0H wvt h Description 416 AES RC 00074 Illite Beidellite 2198 re reen, homo eneous AES RC 00075 Beidellite 2194 re -reen, homo eneous 467 AES RC 00076 Beidellite Chlorite 2192 re -reen, homo eneous AES RC 00077 Beidellite Chlorite 2194 re reen, hom eneous 490 AES RC 00078 Chlorite Smectite 2200 re reen, homo eneous AES RC 00079 Chlorite Smectite 2200 re reen, homo eneous n m -o 0 ---1 w N O '~ cQ cn -P V Anne J.B. Thompson, P.Geo. u's O 0 C O N a E 0 tm d c d` m E d Ol 7 Q N O) C O c r .~ GMC DATA REPORT 3 2 0 c 0 a o ~ p p O - ~ N N 'O c C C ~ a ~ ~6 ~ C 9 C y y y C C ~ d C C c ~ C V C C C $ N y ~ N ~ y C ~ ~ E ~ ~ ~ O ~ V C C « ~ ~ ". R C w C S r rN• y ~i O Bi X E ~ •E ~ .~S ~ X ._ L" ~ s O ~i O ..+ c C O ~ t C ._ N N N y crS E O - E O y ._ v y ._ v L .~ v ~ ~ m y v y v ~ l4 • ~ ~ • 11C m N N ~ K E x E c i9 c .~. E ; E ; N ~ E ~ ~ ~ p N ~ d ~ X ~E _ C c O cLi . ". O O ~ cLi ` m c t0 {0 p C o c o C ~ C c ._ c ._ ° N o ft/l ~ t C7 d 'Ni' o S . ~ $ s O d X E X E X •E ~ O d .~ E .~ E d 4 ~ c N N d O O c ~ d ~ a ~ ~ Y u Y d ~ o N N ~ 9 N 'o S r ~ C ~ L ~ y .. d N r ~ ~ ~ C ~ C ~ C ~ C ~ '~ C C ~ C C " ~ ' c ~ ~ L~ L " 7 7 p 30 ~ 'p 3 o ~ i 3 o ~ ~ ` c ~ f~w0 ._ ~ ._ L p C c N y L ~' ~' L ~ f ~' L ~' ~' L ~' E' L L ~' L L C ~' L d ~' ~' ~ , o C a ~ L g `.4 g `.9 g '.9 L a a V * ' ~ g ,_ E d d O g ' ~ ~ d ~ ~ ~ 9 ` N ~ v L .~ ~ d d d d d d ~ . d d d {~ Y a t0 ~ ~ 47 t0 E . a t0 E co ~ . c G c 4. . - N t V r r d d N d N m d co N co A m ~ ~ m m '~ c~a ~o R '~ ~o co - m ~ d d eo ~ c-~o ~o 'm m L aEi ~ c ' . ~ i a y y c ~ ~ c ~ c 0 ~ ' c O e ~ r c c O c O ~ y O C y L 9 L ~ S N Vl 'O L L . . , . O . . « V O i . . i N .N N 07 0 OD 0 O~ 0 00 0 h O N CO ~ ~ l0 C N O r' W O O ~ O '- N ~ !O ~ O r 00 O O r 00 O O O r _ N N N N N N N N N ( ~ N ( ~ N N N N N N N N N N N N N N N N N N N N M d 'C c ` V d N ~ ~• O ~• U ~• d ' a; ' 4' ' d ' c o c o c 0 c 0 N Y 'C d C d C d C N r ~ • S C .O. _ C ~ ~ C 'C ' .d. C .d.• C .d. y _ 'C ,~. ~. C NN N C « c r C G1 C _ O . O . O . O l0 ~ /9 7 C t S C SZ O s L C Q W 7 C Q L +~ C S C 0 d p O O L U O L U t6 7 a _ c ~ O ~ O ~ C C ~ O ~ O ~ ~ ~ ~ ~ ° ~ ~ ~ ~ ~ ~ ° ~ ~ ~ ~ ~ ~ ~ ~ ~ a ~ ~ o Q Q o 0 0 ~ ~ ~ o cO o o _o d 'C 0 ~ CC 'C 0 ~ 'C 0 ~ 'C 0 ~ 'C C 0C L 'C 0 ~ O ~ ° 'C O ~ ~~pp U ,~ ~p U U ~ 'C ~p U d 'c C O ~ y ~ ~ 'C S 'C y ~ ~~pp t5 'C CO ~ ~~pp U {{p~ .Y g+ c l~ .Y .~ ~p C7 ~p CJ 'C O ~ 'C ~ c •~ 'O" r 'C OFF A 'C O ~ c ~p 1) ttpp .Y C7 'C O ~ .. c ~ ~ o ~ 0 ~ 0 ~ 0 ~ o ~ g c~• : c r? - ~ ~ 4% c y r• N c~• y n• ~ c~ " = c U y ~• t U o ~ f U °: = ~% = ~ U t U c U N ~• o f L ~ i~ ~• ~ o- ~ ~ ~• '- 3 2T> ~• <n r cn n• o ~ ~ N ~• ~ C Y O o ~ ~ y ~• t~ ~• l~ ~• ~ ~ 0 O 0 0 ~ 0 N 0 M 0 0 If1 0 0 ~p 0 0 P 0 0 CO 0 0 p~ 0 0 O ~ 0 ~- ~- 0 N ~- 0 M ~ ~ '- IA ~ tp ~ l~ .- W .- O) ~ p N ~ N N N M N ~ N M N ~p N I~ N OO N Of N O M ~ M N M 0 M M 0 aa C~ 0 ~A M ~p M 0 f~ M 0 0 Ol 0 O ~ ~ ~ N M ~ tq ~ f0 f~ 00 ~ 0) ~ `b' o o o° o g o° OO $ °°o °o °o o° o ~ ~ ~ o 0 OO O 0 ° 0 S $ o 0 8 ~ 0 $ 0 $ 0 0° 0 o° 0 o o g B S 0 ~ o° ~ ~ ~ $ g ~ °o °o °o ~ ~ OO °o d ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ii 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 C ~ N O ~ M p 0 Q ~ V 0 M 0 ^ 0 M p 0 ~ O ~ O N eOe~~ ~Op ~ ~ ~ O ~ O ~ QQQop a M ~ pOO M O N ~ pMpp M p S M ~ p $ a 0 ~ 0 7 ~ 0 p $ M O S M ~ O ~ ~ M C °Q O a O a N ~ O ~ '-° 0 0 ~ 0 0 ~ O N O N c ~ e} c 7 N 7 l'7 1 l' V e e 7 c '1 r M < t0 Z C .7 N O O O 1A CC 0 0 pp 0 0 O 0 0 pp 0 0 N 0 0 ef) 0 0 IA 0 0 1n 0 10 0 0 0 pp O 0 C O 0 O 0 O tfJ N 0 O O 0 ~p ln Cp ~ 0 p l 0 p o 0 p ~ 0 p n 0 O pp O N O O t~ N O O C O 8 O p 1n O O M O 0 O 0 O LfJ 00 0 O 0 O 0 O 0 p In to N t[> 0 p 0 0 O 0 M c+f M M C'~ M M M M ~ A O ~ d' O tt O a O d' d' ? 4 ~ fi a t ~ tn ? a I ~ to 'a ln ~ tO Q 4~ ~A 1d ~ ~ ~ 1~ ~ ~ n ~ n t~ l~ o~ a0 W GMC DATA REPORT 3 2 0 Page 15/17 C O N O. E O d a E N 01 7 Q d O1 C O ti v c fi e .~ O O « C L d y L ~ N N N O N 7 d y C y y L L O 9 H ~ c d N ~ 'v ~ 'v 'v E m L L w o C ~° L w L w ~ c L E w w C y O d ' ~ ~ ~ O C « C a~ .A. C y :p N ,«_ O C C O O C N C y C a0+ d N :Q N t w N L w N L w N L w N C N C y .t' ~ ~ i ~ E C L _ ~ « ~ O C O r y "~ ~p a C C ~. C ~ O L y O ~ = L y c c C ~ .~ y r ~ ,C d ~; d r d = y ~ y ` •. ~ S 'l~. 77 L _ '~ y E E t C •E «c E y C E C y C p p C ~. ~ C b Q y O C L « •_ y ._ L ~ ~ ~ ~ C ~i C ~ O r d C ~ L N t V ~ ~ C y «. p~p C d ~ L C •- E c .y ~: ~ E _ y ~ C ~ y 0 ~ ` ' ° ~ ~ ~ f r o ~ v y v C 0 n0. ._ U 3 E ~ ~ y o w o ,.tJ ~ y O t ~ O C ~ 0 r ~ .9 . : ~ ~ ~ « •_ .~. E C C a . a ~. d ~ d `. ~ c O L w ° L t w u c C ° c c ~ m N pp 67 e w d « o $ «Li ' _ N C ~p C ._ L 0 .. 0 .. 0 .. o ~+ ~ +~= c d t y d f, 7 •- y y pp C y N m y y g~ '- E a~ ~ L _ C ~ ~ .. i L ~ . m y L ~° ~° = c o c ° ~ • ~ L ~ ° ° w d L L L ~ ~ ~ c ~ l6 '= ~ L t E - - ' :: m o u v; vi y L E ? R L c B ~ ~' E 7 ° y 7 ° y 7 ~ ~ " y 7 E N • ~ C ' ~ ~ ~ w y 7 .- L v « ~ N 7 N 7 N 7 L ~ ~ A ~ ~ y 7 .- L y' 7 « > y 7 • ~ w y ~ w y 7 ~ « ~ «? L ; ~ •- ~. w C y ~ L w L w L w w C y N 7 y 0 N 7 w d L y d w C L • ` w an O d ~ ~ L w ~ d t ` ~ m Q y w d ~ g~ ~ a~ ~ m Q m ~ f9 ~ w y w ~ ~ y w d O y m ~ d 3> Q m V a ~ {~ ~ -. d ~ d ~ d Q m ~ " ~ +O„ w u ~ E q E a~ E o ~ ~ E ~ E E E ~ ~ ~ ~ E E c E ~ E E ~ ~ ~ .~ .~ E E ~ ~ x c E E E ~ ° i D c •N C C O C c E ~ •N C •W 9 N 0 0 0 C ~ ~ E c N c V! C •N C ~f/1 C ~tA c c ? E E E E E > ? E E E 'N C C C Z ~ ~ _ Op NON O ~ CO NO CO NO CO O O ~" O N~ O ~ 00 NO Cp NO O NA pp NO 00 NO W O N~ ~p N6 N N0 00 N0 Op N0 OD N0 NO~ NO GO ~Oy ~ N N ~Oy a NA O NO 10 O N ~ ~ N N ~ N O NON N N N N N N N N N N N N N N N N N N N N N N N N N N N d M d 'C C ~ A C ~~pp ~.J L C O O U O r •Q C U C l0 ~ ~ h f ~• ~ O O O 4 O O O O O O N ~ :' C C ' O .L" C ~ « , C r = r C ~ , C QC V 'C ' O . -y •. _ C ~ d ~ 0 ~ « C ;Q « C ; ~ C ,« C « •~ «O-. « . S C ~ _ C ~ « . S O ~ N C CO t « ~ OF ti cO b pFC F ~p U ~ Q Q Y 1 Q l p t Q t p ~ Q e p Y e p ({ pJ f Q M { p { ~ Q ( p ~ ( p ~ l ~ ~ Y C~• Y ~ Y Y ° Y Y L`~ f ~• CJ ~ G~• ~ Y Y Y ~ Y O Y f~• ~ Y U ~ ~ Y ~ ~ ~ C~• N « « « d ~ N « « « « C O C O C O C _O C _O C O C O C O C O C O C O S ` d 'C O ~ r 'C O ~ °~ Y °~ .Y ~ P• 'C O E 'C ~ 'C O ~ ~ Y 'C gg 5 r Y 4f .5 ~ ~% ~ « .E - « .5 _ O ~ - O 5 - ~0 ~ ~ ~ 'C O ~ « ;c m ]~ 0 « .- - ~ ~ 'C O ~ ~ d Y d r G7 :~ `~ « Y :; Y d c ~ O 'c ~ d ;c ~ 'C 0 ~ 'C 0 ~ C 'C 0 .~ C m V ~ 'C O ~ C `~ ~~ ~ C Y C C C C C ~ ~ VS cA J) ~ ~ . V _ ~ ~ C ~ ~ V ~ V ~ ~ ~ ~ ~ ~ ~ ~ r ~ ~ ~ = ~ ~ ~ Te ~ 0 ~ 0 0 3 ~ ~ ~ 0 ~ O O Y Y Y N r• n• O ~• c 0 O O ~ ~ d O pN O '- SA O N Ln ppO M ~p S ~ $ iA 1p $ ~p 1f1 O l~ 1n O 1ppn O Of 1n S O O .- O N O O M ~pp O ~a} (O O ~A ~p p op 10 ~ f~ ~ pp <O pp Of tO pO O f~ pp '- f~ pO N 1~ 8 M ~ O ~ ~ p O ~ ~ p O tO ~ pp f~ ~ pp ~0 n pp 07 n $ 0 O °O ~ O °O N O p O M O g ~ O ~A O O ~p 00 O l~ O p° pp CO °° Of O O O 01 O ~ p~ p o N ~ M O O Lf7 O O I~ O) O N pp~ O O) pp~ O ~ 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 O O O O O S O O O O O O O O O O O O O O O O O O 0 0 0 0 0 0 C 0 d ' ~ ' ~ a' ' ~ Q' Q' ' ' Q' Q' 2' Q' Q ' d' d' Q' Q' Q' Q' 2' ~ d' a' Q' Q' Q' Q' ~ Q' Q' Q' ~ R ~ Q' Q ' Q' Q' ~ ~ Q' Q ' Q' ~ Q' d' ~ ii Q 0 Q 0 Q 0 0 0 a 0 0 0 0 Q 0 Q 0 0 0 0 0 . 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 . 0 0 0 0 0 0 0 c ° N gga o M o°~ ~ °o V °o ~ °o N ~ °o M °o M pQ° °o p°o °o ° o ~ ~ ~ °o ~ oN° °o ~ °o ~ ~°op o°~ ~ °o ~ eo°~ °o M ppp° ~ Mp° °o N o M °o N Ch C ~ to i O ~7 t A 1n f~7 to C 7 V 2 G a O o O o g 8 N ~0 ° O ° °° O ~ O ° O ~ O u4i O O u4i O ~ O °o $ $ O i°n O ~°n Q ~ ° g O ° O ~ ° ~ O a O v~ O o O 0 S 0 r r ~ .- .- ~ ~ r W GMC DATA REPORT 3 2 0 Page 16/17 pC N a E 0 t I- m m c c Q a~ E d 7 Q C d O) C O ti .p a N N L U y E C ~ g L y N N ~ E 7 L ~i c ~ j LU Y ~ ~ ~ N C ' L «_ ~ N V N LyZ; c E - t N E = Q N .- 0i ~ ~ E N ~ r L ~ C L U N O C O C C y C t9 g •- vi 9 C N C N N V E C E C U o ~ E N N ~ 'O C y t ~ Q y y V y ~ G « m y« N G c d C ' N L U N L c L U d y O ~ ~ 7 L ~ ° d N .- L U .- L U c E E U L G L w N U y _ _ t y .- ~ }' C ~ N L U N x U L ,~ ,~ d E o ~ ~ o ~ c c ° ~ £ 3 c ~ c ~ v ~ ° o $ ~ - ~ ~ o •c :: u ° e m E ~ « d E m ~ R 3 - « ~ ~ ~ ~ E o - N m .. o o N ? c ~ c a~ o L c c - '.g ~ E e; ~ R .. c v 3 L ' ~ g ~ ~ E E d ~ o « o ~ o - ~° o , _ « ~ = ~ :3 ~•-c c « c « c ~° o c « ~ ~ « o ~ E o ~ E t " ~ L E ~ d c `.9 ' ~ 3 e m ~ ~ Q c « o $ c E > ~ E ? ~ ~ ~ ai ~ ~ > > g ~ ,o, Y ~' ~ E 3 Q L '~~ L m - ~ ~° ` ~ ` ~ ~e ~ ? 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' _ 'C ~ _ 'C ~ d C « C G ~ d d C ° U C ~Ot~ ~ G O /6 C.1 C O - e° C O Z • G S L O ~O Y _ Y .52 _ ccp O ~ .Y O cO~pp Y C O ~ ~ c l0 U l~ U + ,4 Y U O ~tp -• ,. ~C U ~ ~p Y C C O N r O et~p O ccpp « - Y - C ° ~ d ~ o ° o o ¢~ o c 4 0 0 ° c o o o g o ,r- 'C •~ O 'C Oy •FC°F ~C •Q , g ~p •p •C •C N C d N ~p CO O C ~p O O O O ~~pp ~p c e ~ :: o ~ o ~ o :; r: N tn ° c o 0 0 0 c y o c v ~ ° r~ m o _ _ = :: v ca :: «? :: = ~ O o o ° o 0 0 0 0 0 0 ~~pp O n O W O O O O r r r N r M r ~ r lA r l0 r f~ r o0 r 0) r O N r N NN N M N a N iA N (O N h N O~ N ~ pp M r M N M M M ~} C~ ~O M ~p M h M 00 M 0) M ~ r ~ N 7 M ' C tai d' 1~ ~ y e r O. r O S S r O r O r O 3 r S r O o r O c r O O r O 0 r O o r S 8 r S r S r O O r O O r S r S r O O r O O r O C r S r S B r S r S r O c r S r S r S r O c O c r O c r O c r O c r S r S O c r O c r O c r S r O O r S r O c d c ~ O ~ ~ ~ 0 ~ 0 ~ 0 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ii 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 a t[ ~ p a po6 p ~ O ~ O pp O ~ } ~ 5 N M M ~ o6p '' ~ . M M ~ l0 M ~ C ~ Kf N M ~ et N f Y N N M f ) 2 X ' 0 0 0 0 0 0 o 0 O O O C C O 0 O 0 O O o O O O $ o ~ O O O O O O O $ O O 0 O O 0 O S O O O ~ O O M O G ~ O O O O O O S ~ O O M A ~ 0 ~ 0 ~ tCy r ~ r ~ r r E r O fV O fV O fV O CV N GV fV CV N fV M CV M M M M M M M M ~f ~ ~? Q W r r r r r r r r r r r r r r r r r r r r r GMC DATA.RFpORT 3 2 0 Page 17/17