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Osisko Windfall Infill Drilling Returns More of the Same

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Osisko Windfall Infill Drilling Returns More of the Same

 

 

 

 

 

395 g/t Au Over 2.3 Metres and 61.5 g/t Au Over 9.2 Metres

 

 

Osisko Mining Inc. (TSX:OSK) is pleased to provide new analytical results from the ongoing expansion and definition drill program at its 100% owned Windfall gold project located in the Abitibi greenstone belt, Urban Township, Eeyou Istchee James Bay, Québec.

 

Drilling is currently focused on the Lynx deposit. Osisko Chief Executive Officer John Burzynski commented: “Infill drilling at Windfall, and in particular Lynx, continues to progress well. Predictably, and with a familiar consistency, once again Lynx delivered on high-grade with our headline intercept of 395 g/t Au over 2.3 metres, and also on width with the very nice intercept of 61.5 g/t Au over 9.2 metres.”

 

The table below contains resource definition infill intercepts located inside the February 2020 mineral resource estimate wireframes (see Osisko news release dated February 19, 2020). Significant new analytical results are presented below and include 33 intercepts in 16 drill holes and 7 wedges.

 

Selected high-grade intercepts from the new results include: 395 g/t Au over 2.3 metres OSK-W-20-2292-W1; 61.5 g/t Au over 9.2 metres and 37.0 g/t Au over 3.0 metres in OSK-W-20-2256-W4; 55.5 g/t Au over 2.5 metres in WST-20-0350 and 40.1 g/t Au over 2.8 metres in WST-20-0013. Maps showing hole locations and full analytical results are available at www.osiskomining.com.

 

 

Hole No. From
(m)
To
(m)
Interval
(m)
Au (g/t)
uncut
Au (g/t)
cut to
100 g/t
Zone Corridor
OSK-W-20-2139-W12 905.3 907.9 2.6 28.5   Lynx_371 Triple Lynx
including 906.2 906.8 0.6 88.3  
OSK-W-20-2139-W9 886.7 893.0 6.3 15.4   Lynx_371 Triple Lynx
OSK-W-20-2252-W3 865.7 867.7 2.0 11.7   Lynx_371 Triple Lynx
including 865.7 866.0 0.3 58.6  
OSK-W-20-2256-W4 862.0 871.2 9.2 61.5 32.6 Lynx_361 Triple Lynx
including 863.0 864.0 1.0 281 100
and 870.0 871.2 1.2 171 100
  881.0 884.0 3.0 37.0   Lynx_361 Triple Lynx
including 882.0 883.0 1.0 86.2  
OSK-W-20-2275-W2 628.9 631.0 2.1 8.18   Lynx_365 Triple Lynx
including 628.9 629.8 0.9 18.5  
  800.0 802.3 2.3 3.65   Lynx_376 Triple Lynx
including 800.0 800.6 0.6 10.9  
OSK-W-20-2283 935.0 937.0 2.0 18.5   Triple Lynx Triple Lynx
including 936.0 936.7 0.7 49.6  
OSK-W-20-2292-W1 1040.7 1043.0 2.3 395 15.4 Lynx_374 Triple Lynx
including 1041.3 1041.6 0.3 3010 100
OSK-W-20-2292-W2 909.3 913.0 3.7 3.64   Lynx_375 Triple Lynx
OSK-W-20-2322 1090.3 1094.1 3.8 28.9   Lynx_334 Lynx
including 1090.3 1091.3 1.0 81.9  
WST-20-0011 74.3 76.4 2.1 4.68   Lynx_311 Lynx
WST-20-0012D 81.0 83.0 2.0 3.14   Lynx_311 Lynx
including 82.5 83.0 0.5 8.68  
WST-20-0013 140.0 142.8 2.8 40.1 31.5 Lynx_304 Lynx
including 140.7 141.5 0.8 130 100
WST-20-0014A 100.2 102.2 2.0 5.40   Lynx_304 Lynx
WST-20-0350 128.5 131.0 2.5 55.5   Lynx_359 Lynx
including 129.2 129.9 0.7 98.8  
WST-20-0352 32.3 36.0 3.7 16.2   Lynx_325 Lynx
including 35.0 36.0 1.0 46.8  
  97.0 99.0 2.0 5.95   Lynx_304 Lynx
WST-20-0394 35.1 37.3 2.2 11.7   Lynx_325 Lynx
  70.8 72.8 2.0 4.15   Lynx_311 Lynx
  107.0 109.3 2.3 24.2 23.2 Lynx_304 Lynx
including 107.0 107.7 0.7 78.9 75.7
WST-20-0395 50.0 52.0 2.0 6.45   Lynx_303 Lynx
WST-20-0420 79.4 81.7 2.3 4.11   Lynx_323 Lynx
including 81.4 81.7 0.3 29.1  
  150.0 152.1 2.1 19.0   Lynx_321 Lynx
including 151.2 152.1 0.9 43.5  
WST-20-0422 160 162 2.0 5.90   Lynx_328 Lynx
WST-20-0482 87.9 90.0 2.1 6.00   Lynx_323 Lynx
WST-20-0484 43.1 45.5 2.4 4.80   Lynx_325 Lynx
including 43.7 44.0 0.3 33.1  
  94.2 96.3 2.1 13.5   Lynx_304 Lynx
including 94.8 95.2 0.4 31.0  
WST-20-0485 106.3 108.3 2.0 5.55   Lynx_323 Lynx
including 107.9 108.3 0.4 27.2  
  119.3 122.0 2.7 12.6   Lynx_304 Lynx
including 119.3 119.7 0.4 60.5  
  143.2 145.3 2.1 16.3   Lynx_359 Lynx
including 144.3 145.0 0.7 48.4  
WST-20-0486 44.9 47.3 2.4 11.2   Lynx_325 Lynx
Including 46.8 47.3 0.5 34.8  
  51.5 54.5 3.0 14.9   Lynx_303 Lynx
Notes: True widths are estimated at 55 – 80% of the reported core length interval. See “Quality Control and Reporting Protocols” below.

 

 

Drill hole location

 

Hole Number Azimuth (°) Dip (°) Length (m) UTM E UTM N Elevation Section
OSK-W-20-2139-W12 115 -52 1038 452980 5435549 420 3450
OSK-W-20-2139-W9 115 -52 1152 452980 5435549 420 3450
OSK-W-20-2252-W3 129 -53 1062 453241 5435694 415 3750
OSK-W-20-2256-W4 125 -51 1122 453160 5435686 414 3675
OSK-W-20-2275-W2 127 -49 1035 452886 5435584 409 3400
OSK-W-20-2283 135 -50 1151 452997 5435607 425 3500
OSK-W-20-2292-W1 125 -54 1149 453037 5435563 420 3525
OSK-W-20-2292-W2 125 -54 1002 453037 5435563 420 3525
OSK-W-20-2322 130 -54 1191 453608 5435713 404 4075
WST-20-0011 157 -54 451 453105 5435065 231 3325
WST-20-0012D 174 -62 465 453226 5435126 134 3475
WST-20-0013 171 -42 169 453357 5435208 154 3625
WST-20-0014A 137 1 124 453359 5435209 155 3625
WST-20-0350 142 -31 175 453359 5435209 154 3625
WST-20-0352 140 -10 177 453359 5435209 155 3625
WST-20-0394 152 -26 172 453358 5435208 154 3625
WST-20-0395 153 -16 169 453358 5435208 155 3625
WST-20-0420 155 -10 166 453450 5435264 116 3725
WST-20-0422 171 -26 177 453449 5435264 117 3725
WST-20-0482 165 -9 181 453449 5435264 117 3725
WST-20-0484 138 -26 160 453359 5435209 154 3625
WST-20-0485 148 -44 181 453359 5435209 154 3625
WST-20-0486 130 -37 162 453359 5435209 154 3625

 

Lynx Zone

 

Mineralization occurs as grey to translucent quartz-carbonate-pyrite-tourmaline veins and pyrite replacement zones and stockworks. The vein-type is associated with haloes of pervasive sericite-pyrite ± silica alteration and contain sulphides (predominantly pyrite with minor amounts of chalcopyrite, sphalerite, galena, arsenopyrite, and pyrrhotite) and local visible gold. Replacement mineralization is associated with strong pervasive silica-sericite-ankerite ± tourmaline alteration and contains disseminated pyrite from trace to 80% with local visible gold. Pyrite stockworks can form envelopes that reach several tens of metres thick. Fuchsite alteration is common and is spatially constrained to near the gabbros. Mineralization occurs at or near geological contacts between felsic porphyritic or fragmental intrusions and the host rhyolites or gabbros and locally can be hosted along the gabbro-rhyolite contact.

 

Triple Lynx

 

Mineralization in the Triple Lynx zone is vein-type, quartz-carbonate-pyrite-tourmaline veins, associated with pervasive sericite-pyrite ± silica alteration and contain sulphides similar to the main Lynx Zone, pyrite dominated with minor other sulphides, ranging from trace to up to 70% locally, and local visible gold. Locally fuchsite is present when proximal to the gabbros. Mineralization is hosted in or at the contacts of felsic porphyritic dikes with rhyolites (locally bleached) or gabbros.

 

Qualified Person

 

The scientific and technical content of this news release has been reviewed, prepared and approved by Mr. Louis Grenier, M.Sc.A., P.Geo. (OGQ 800), Project Manager of Osisko’s Windfall Lake gold project, who is a “qualified person” as defined by National Instrument 43-101 – Standards of Disclosure for Mineral Projects.

 

Quality Control and Reporting Protocols

 

True width determination is estimated at 55-80% of the reported core length interval for the zone. Assays are uncut except where indicated. Intercepts occur within geological confines of major zones but have not been correlated to individual vein domains at this time. Reported intervals include minimum weighted averages of 3.0 g/t Au diluted over core lengths of at least 2.0 metres. All NQ core assays reported were obtained by either 1-kilogram screen fire assay or standard 50-gram fire-assaying-AA finish or gravimetric finish at (i) ALS Laboratories in Val d’Or, Québec, Thunder Bay, Ontario, Sudbury, Ontario or Vancouver, British Colombia, or (ii) Bureau Veritas in Timmins, Ontario. The 1-kilogram screen assay method is selected by the geologist when samples contain coarse gold or present a higher percentage of pyrite than surrounding intervals. Selected samples are also analyzed for multi-elements, including silver, using a four acids digestion -MS61 method at ALS Laboratories. Drill program design, Quality Assurance/Quality Control  and interpretation of results is performed by qualified persons employing a QA/QC program consistent with NI 43-101 and industry best practices. Standards and blanks are included with every 20 samples for QA/QC purposes by the Corporation as well as the lab. Approximately 5% of sample pulps are sent to secondary laboratories for check assay.

 

About the Windfall Gold Deposit

 

The Windfall gold deposit is located between Val-d’Or and Chibougamau in Eeyou Istchee James Bay, Québec, Canada. The mineral resource defined by Osisko, as disclosed in the news release dated February 19, 2020 and supported by the technical report entitled “An updated mineral resource estimate for the Windfall Lake Project, Located in the Abitibi Greenstone Belt, Urban Township, Eeyou Istchee James Bay, Québec, Canada” and dated April 3, 2020 (with an effective date of January 3, 2020), and assuming a cut-off grade of 3.5 g/t, comprises 4,127,000 tonnes at 9.1 g/t Au (1,206,000 ounces) in the indicated mineral resource category and 14,532,000 tonnes at 8.40 g/t Au (3,938,000 ounces) in the inferred mineral resource category. The key assumptions, parameters and methods used to estimate the mineral resource estimate disclosed in the February 19,2020 news release are further described in the full technical report prepared by Micon International Limited and BBA Inc, in accordance with NI 43-101 available on SEDAR (www.sedar.com) under the Corporation’s issuer profile. The Windfall gold deposit is currently one of the highest-grade resource-stage gold projects in Canada and has world-class scale. Mineralization occurs in three principal zones: Lynx, Main Zone, and Underdog. Mineralization is generally comprised of deformed sub-vertical zones plunging to the northeast. Vein-type or pyrite replacement-type styles of mineralization crosscut syn-volcanic host rocks and syn-deformation felsic porphyry intrusions and are spatially associated with the contacts of the intrusions. The deposit is well defined from surface to a depth of 1,200 metres and remains open along strike and at depth. Mineralization has been identified 30 metres from surface in some areas and as deep as 2,000 metres in others, with significant potential to extend mineralization down-plunge and at depth.

 

About Osisko Mining Inc.

 

Osisko is a mineral exploration company focused on the acquisition, exploration, and development of precious metal resource properties in Canada. Osisko holds a 100% interest in the high-grade Windfall gold deposit located between Val-d’Or and Chibougamau in Québec and holds a 100% undivided interest in a large area of claims in the surrounding Urban Barry area and nearby Quévillon area (over 2,700 square kilometres).

 

Posted November 5, 2020

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