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Osisko Windfall Infill Drilling Confirming Shallow Mineralized Zones

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Osisko Windfall Infill Drilling Confirming Shallow Mineralized Zones

 

 

 

 

 

Osisko Mining Inc. (TSX:OSK) is pleased to provide new infill drilling results from the ongoing drill definition and expansion program at its 100% owned Windfall Lake gold project located in the Abitibi greenstone belt, Urban Township, Eeyou Istchee James Bay, Québec. The 800,000 metre drill program commenced in late 2015. The program is now focussed on infill drilling within the main Windfall gold deposit and the adjacent Lynx deposit (located immediately NE of Windfall), and exploration and expansion drilling on main mineralized zones with several deep holes in progress to investigate the down-plunge areas in and around the Underdog and Lynx zones.

 

 

Today’s results, presented in the table below, include significant new analytical results from 59 intercepts in 37 drill holes and extensions focused on shallow infill drilling in the Windfall deposit all above 400 metres vertical depth.

 

 

Highlights from the new results include: 34.8 g/t Au over 4.3 metres in OSK-W-18-1614; 12.6 g/t Au over 10.7 metres and 27.0 g/t Au over 4.2 metres in OSK-W-18-1547; 37.9 g/t Au over 3.2 metres in OSK-W-18-1586; and 34.6 g/t Au over 2.0 metres in OSK-W-18-1510. 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
Type Mineralized
Area
OSK-OBM-16-662 395.0 400.0 5.0 4.25   infill Zone 27
OSK-W-18-1466 177.0 179.0 2.0 3.81   infill Zone 27
including 178.1 178.5 0.4 17.8  
OSK-W-18-1481 89.0 91.0 2.0 12.7   infill Bobcat
including 89.4 90.5 1.1 22.9  
OSK-W-18-1487 44.5 50.0 5.5 3.62   infill Caribou
OSK-W-18-1497 72.2 74.4 2.2 5.45   infill Caribou
including 72.2 72.8 0.6 14.1  
  91.3 94.0 2.7 3.84   infill Caribou
OSK-W-18-1505 46.0 49.0 3.0 9.78   infill Caribou
  196.0 198.0 2.0 3.07   infill Zone 27
OSK-W-18-1506 353.0 355.3 2.3 6.66   infill Zone 27
OSK-W-18-1509 14.8 17.0 2.2 6.23   extension Bobcat
including 15.5 15.8 0.3 38.7  
OSK-W-18-1510 304.7 306.7 2.0 34.6   infill Zone 27
including 306.0 306.7 0.7 75.1  
OSK-W-18-1517 81.7 88.0 6.3 4.24   infill Caribou
OSK-W-18-1518 71.6 74.0 2.4 5.39   infill Caribou
OSK-W-18-1534 338.5 340.5 2.0 4.38   infill Zone 27
including 338.8 339.2 0.4 18.5  
OSK-W-18-1538 279.0 281.0 2.0 5.69   infill Zone 27
including 280.0 280.4 0.4 24.9  
  302.1 304.1 2.0 6.60   infill Zone 27
including 303.0 304.1 1.1 11.4  
OSK-W-18-1543 207.0 209.3 2.3 8.15   infill Zone 27
including 208.5 209.3 0.8 19.0  
OSK-W-18-1545 189.6 196.3 6.7 3.31   infill Caribou
  240.0 242.5 2.5 5.33   infill Caribou
OSK-W-18-1547 108.6 113.2 4.6 4.86   infill Caribou
  286.4 288.8 2.4 3.67   infill Caribou
  294.6 296.8 2.2 3.60   infill Caribou
  338.0 348.7 10.7 12.6   infill Zone 27
including 342.0 343.0 1.0 93.7  
  371.0 375.2 4.2 27.0   infill Zone 27
  379.5 382.0 2.5 22.5   infill Zone 27
OSK-W-18-1552 101.2 103.5 2.3 5.98   infill Caribou
including 101.6 102.4 0.8 15.1  
OSK-W-18-1558 156.0 158.0 2.0 11.4   infill Caribou
  273.8 276.2 2.4 3.30   infill Caribou
  365.7 372.8 7.1 6.98   infill Zone 27
OSK-W-18-1559 256.0 258.0 2.0 3.43   infill Zone 27
OSK-W-18-1563 64.0 66.8 2.8 4.72   infill Caribou
  158.0 160.0 2.0 4.52   infill Caribou
  283.0 285.9 2.9 5.20   infill Zone 27
  302.0 304.0 2.0 4.67   infill Zone 27
OSK-W-18-1567 172.0 174.0 2.0 3.34   infill Zone 27
  187.2 191.0 3.8 8.56   infill Zone 27
including 190.5 191.0 0.5 40.5  
OSK-W-18-1572 206.6 208.6 2.0 3.44   infill Caribou
  532.0 534.0 2.0 6.61   infill Zone 27
including 532.0 532.6 0.6 21.4  
OSK-W-18-1577 88.8 91.2 2.4 8.83   infill Zone 27
including 89.5 90.2 0.7 30.1  
OSK-W-18-1580 15.0 17.0 2.0 6.47   infill Zone 27
including 15.0 15.7 0.7 18.1  
OSK-W-18-1586 52.4 55.6 3.2 37.9   infill Zone 27
including 53.2 54.0 0.8 83.7  
OSK-W-18-1594 166.9 169.3 2.4 3.53   infill Zone 27
OSK-W-18-1596 245.0 247.1 2.1 5.52   infill Zone 27
including 245.6 246.1 0.5 13.4  
OSK-W-18-1597 127.9 130.0 2.1 9.08   infill Caribou
including 127.9 129.0 1.1 17.3  
  205.0 207.5 2.5 5.08   infill Zone 27
OSK-W-18-1601 33.0 35.0 2.0 4.38   infill Caribou
OSK-W-18-1602 83.5 85.5 2.0 18.4   infill Caribou
including 83.5 84.5 1.0 36.4  
  140.7 143.1 2.4 7.94   infill Caribou
including 141.8 142.4 0.6 22.4  
  170.5 172.5 2.0 4.13   infill Caribou
OSK-W-18-1605 248.0 250.0 2.0 3.05   infill Zone 27
OSK-W-18-1607 202.0 204.0 2.0 3.89   infill Zone 27
OSK-W-18-1609 58.5 61.0 2.5 5.54   infill Caribou
including 58.5 59.7 1.2 11.4  
  257.8 260.5 2.7 4.69   infill Zone 27
including 258.8 259.3 0.5 22.2  
OSK-W-18-1611 82.0 84.1 2.1 5.19   infill Caribou
including 83.3 84.1 0.8 12.6  
  215.9 218.0 2.1 5.41   infill Zone 27
OSK-W-18-1614 71.0 73.1 2.1 6.47   infill Zone 27
  81.0 85.3 4.3 34.8 28.2 infill Zone 27
including 84.0 85.3 1.3 100 78.5
OSK-W-18-1617 151.7 154.3 2.6 3.49   infill Caribou
including 153.9 154.3 0.4 15.7  
OSK-W-18-1631 265.0 267.0 2.0 17.1   infill Zone 27
including 266.0 267.0 1.0 34.0  

 

Note:      True widths are estimated at 65 – 80% of the reported core length interval.  See “Quality Control and Reporting Protocols” below.

 

 

 

Hole No. Azimuth (°) Dip (°) Length (m) UTM E UTM N Section
OSK-OBM-16-662 330 -53 435 452423 5434665 2550
OSK-W-18-1466 344 -47 300 451979 5434531 2075
OSK-W-18-1481 322 -46 108 452706 5434972 2925
OSK-W-18-1487 332 -46 57 452341 5434658 2475
OSK-W-18-1497 331 -52 363 452350 5434664 2475
OSK-W-18-1505 328 -45 342 452350 5434661 2475
OSK-W-18-1506 329 -53 417 452366 5434643 2475
OSK-W-18-1509 329 -51 228 452907 5434997 3125
OSK-W-18-1510 325 -58 405 452279 5434572 2375
OSK-W-18-1517 330 -49 348 452385 5434672 2500
OSK-W-18-1518 330 -54 393 452266 5434569 2350
OSK-W-18-1534 332 -45 396 452462 5434676 2575
OSK-W-18-1538 330 -55 351 452253 5434616 2375
OSK-W-18-1543 327 -52 294 452251 5434639 2375
OSK-W-18-1545 332 -49 522 452452 5434662 2575
OSK-W-18-1547 330 -62 441 452299 5434640 2425
OSK-W-18-1552 332 -52 366 452308 5434640 2425
OSK-W-18-1558 316 -47 459 452462 5434664 2575
OSK-W-18-1559 331 -53 330 452299 5434661 2425
OSK-W-18-1563 334 -46 330 452297 5434656 2425
OSK-W-18-1567 328 -48 213 452238 5434684 2375
OSK-W-18-1572 333 -50 558 452469 5434627 2550
OSK-W-18-1577 325 -45 153 452235 5434845 2475
OSK-W-18-1580 327 -46 60 452264 5434853 2500
OSK-W-18-1586 146 -52 117 452270 5434955 2550
OSK-W-18-1594 140 -50 270 452212 5434966 2500
OSK-W-18-1596 333 -45 339 452328 5434668 2450
OSK-W-18-1597 325 -47 254 452276 5434661 2400
OSK-W-18-1601 330 -49 273 452266 5434629 2375
OSK-W-18-1602 330 -47 261 452276 5434661 2400
OSK-W-18-1605 329 -45 345 452328 5434668 2450
OSK-W-18-1607 332 -47 261 452244 5434627 2375
OSK-W-18-1609 334 -45 315 452312 5434665 2450
OSK-W-18-1611 328 -46 270 452278 5434651 2400
OSK-W-18-1614 146 -47 279 452157 5434953 2450
OSK-W-18-1617 329 -47 245 452273 5434674 2425
OSK-W-18-1631 330 -45 315 452356 5434670 2475

 

 

OSK-OBM-16-662 intersected 4.25 g/t Au over 5.0 metres in Zone 27. Mineralization consists of up to 1% disseminated pyrite within a strong sericite altered andesite in contact with a felsic dike.

 

 

OSK-W-18-1466 intersected 3.81 g/t Au over 2.0 metres in Zone 27. Mineralization consists of 2% disseminated pyrite and stringers within a strong sericite and chlorite altered andesite in contact with a felsic porphyritic dike.

 

 

OSK-W-18-1481 intersected 12.7 g/t Au over 2.0 metres in Bobcat. Mineralization consists of up to 3% pyrite stringers and quartz-tourmaline veins within a strong silica and moderate sericite altered felsic porphyritic dike.

 

 

OSK-W-18-1487 intersected 3.62 g/t Au over 5.5 metres in Caribou. Mineralization consists of 2% pyrite stringers and trace sphalerite within a strong sericite and silica altered felsic porphyritic dike.

 

 

OSK-W-18-1497 intersected 5.45 g/t Au over 2.2 metres and 3.84 g/t Au over 2.7 metres in Caribou. Both intervals contain up to 10% pyrite stringers at the contact between a strong silica altered rhyolite and a felsic porphyritic intrusion.

 

 

OSK-W-18-1505 intersected 9.78 g/t Au over 3.0 metres in Caribou and 3.07 g/t Au over 2.0 metres in Zone 27. The first interval contains 10% pyrite stringers within a strong sericite altered felsic porphyritic dike. The last interval contains up to 5% pyrite stringers within a strong sericite altered rhyolite.

 

 

OSK-W-18-1506 intersected 6.66 g/t Au over 2.3 metres in Zone 27. Mineralization consists of up to 10% disseminated pyrite and 3% pyrite-tourmaline veins within a strong sericite and weak silica altered felsic porphyritic intrusion.

 

 

OSK-W-18-1509 intersected 6.23 g/t Au over 2.2 metres in Bobcat. Mineralization consists of 3% disseminated pyrite included in silica flooding hosted in a moderate silica and weak sericite altered felsic fragmental dike. The interval extends the Bobcat zone 25 metres north-east from OSK-W-17-1251 (8.89 g/t Au over 3.0 metres, reported January 25, 2018).

 

 

OSK-W-18-1510 intersected 34.6 g/t Au over 2.0 metres in Zone 27. Mineralization consists of up to 10% pyrite stringers, locally semi-massive, hosted in a weak sericite and fuchsite altered andesite.

 

 

OSK-W-18-1517 intersected 4.24 g/t Au over 6.3 metres in Caribou. Mineralization consists of 10% pyrite clusters at a faulted contact between a moderate sericite altered gabbro and a rhyolite.

 

 

OSK-W-18-1518 intersected a vein returning 5.39 g/t Au over 2.4 metres. Mineralization consists of disseminated pyrite within the monzonitic “Red Dog” dike.

 

 

OSK-W-18-1534 intersected 4.38 g/t Au over 2.0 metres in Zone 27. Mineralization consists of up to 7% quartz-tourmaline stringers, 1% pyrite clusters and ptygmatic tourmaline veins within a strong sericite altered felsic porphyritic dike.

 

 

OSK-W-18-1538 intersected 5.69 g/t Au over 2.0 metres and 6.60 g/t Au over 2.0 metres in Zone 27. The first interval contains 2% disseminated and stringer pyrite within a moderate sericite altered felsic porphyritic intrusion. The second interval contains up to 3% pyrite stringers and 1% disseminated pyrite and quartz-tourmaline veins at the contact between a strong silica and sericite altered felsic porphyritic dike and a chlorite altered andesite.

 

 

OSK-W-18-1543 intersected 8.15 g/t Au over 2.3 metres in Zone 27. Mineralization consists of local visible gold, up to 7% pyrite with quartz-tourmaline veins and trace chalcopyrite hosted at a strong sericite altered contact between a felsic porphyritic intrusion and a rhyolite.

 

 

OSK-W-18-1545 intersected 3.31 g/t Au over 6.7 metres and 5.33 g/t Au over 2.5 metres in Caribou. Both intervals contain up to 10% pyrite, disseminated or in clusters, and trace pyrite-tourmaline stringers hosted in a moderate sericite altered rhyolite.

 

 

OSK-W-18-1547 intersected six intervals: 4.86 g/t Au over 4.6 metres, 3.67 g/t Au over 2.4 metres and 3.60 g/t Au over 2.2 metres in Caribou and, 12.6 g/t Au over 10.7 metres, 27.0 g/t Au over 4.2 metres and 22.5 g/t Au over 2.5 metres in Zone 27. The first interval contains 15% pyrite stockwork within a moderate sericite altered rhyolite. The second and third intervals contain up to 7% pyrite stringers, locally semi-massive, and trace tourmaline stringers within a strong sericite altered felsic porphyritic dike. The three Zone 27 intervals contain up to 15% pyrite stringers, locally semi-massive, pyrite-silica flooding, local visible gold, trace sphalerite and chalcopyrite hosted in strong silica altered felsic dike.

 

 

OSK-W-18-1552 intersected 5.98 g/t Au over 2.3 metres in Caribou. Mineralization consists of up to 7% pyrite stringers at the contact between moderate sericite altered rhyolite and a felsic porphyritic dike.

 

 

OSK-W-18-1558 intersected three intervals: 11.4 g/t Au over 2.0 metres and 3.30 g/t Au over 2.4 metres in Caribou and 6.98 g/t Au over 7.1 metres in Zone 27. The first interval contains trace pyrite, disseminated and clustered, within a moderate sericite altered felsic dike. The second interval contains up to 15% stringer and disseminated pyrite within a strong silica altered and moderate sericite altered rhyolite. The last interval contains up to 10% pyrite stringers, 1% disseminated pyrite within a moderate silica and sericite altered felsic porphyritic dike.

 

 

OSK-W-18-1559 intersected 3.43 g/t Au over 2.0 metres in Zone 27. Mineralization consists of 1% pyrite stringers within a moderate sericite altered contact between an andesite and a felsic intrusion.

 

 

OSK-W-18-1563 intersected four intervals: 4.72 g/t Au over 2.8 metres and 4.52 g/t Au over 2.0 metres in Caribou and, 5.20 g/t Au over 2.9 metres and 4.67 g/t Au over 2.0 metres in Zone 27. The first interval contains 30% semi-massive pyrite hosted in a moderate sericite altered rhyolite. The second interval contains trace disseminated pyrite within a moderate chlorite altered rhyolite. The third interval contains 2% disseminated pyrite and 1% pyrite stringers within a moderate silica and carbonate altered felsic porphyritic intrusion. The last interval contains 1% pyrite, disseminated and stringers, within a moderate chlorite altered andesite.

 

 

OSK-W-18-1567 intersected 3.34 g/t Au over 2.0 metres and 8.56 g/t Au over 3.8 metres in Zone 27. The first interval contains trace disseminated pyrite and ptygmatic tourmaline veins hosted in a moderate sericite altered rhyolite. The second interval contains 5% pyrite-tourmaline veins and 1% pyrite stringers hosted in quartz-carbonate and moderate sericite altered felsic porphyritic intrusion.

 

 

OSK-W-18-1572 intersected 3.44 g/t Au over 2.0 metres in Caribou and 6.61 g/t Au over 2.0 metres in Zone 27. The first interval contains 2% pyrite-silica flooding and 1% pyrite stringers within a moderate sericite, chlorite and carbonate altered rhyolite. The second interval contains up to 2% pyrite, disseminated and stringers, hosted in a moderate chlorite and carbonate altered felsic dike.

 

 

OSK-W-18-1577 intersected 8.83 g/t Au over 2.4 metres in Zone 27. Mineralization consists of 40% semi-massive pyrite at a strong sericite altered contact between a gabbro and felsic porphyritic intrusion.

 

 

OSK-W-18-1580 intersected 6.47 g/t Au over 2.0 metres in Zone 27. Mineralization consists of 5% quartz-tourmaline veins and 5% semi-massive pyrite hosted in a weak sericite altered rhyolite.

 

 

OSK-W-18-1586 intersected 37.9 g/t Au over 3.2 metres in Zone 27. Mineralization contains 25% pyrite-tourmaline stringers and local visible gold within a strong silica and moderate sericite altered rhyolite.

 

 

OSK-W-18-1594 intersected 3.53 g/t Au over 2.4 metres in Zone 27. Mineralization consists of up to 15% pyrite stringers hosted in a moderate sericite altered felsic porphyritic dike.

 

 

OSK-W-18-1596 intersected 5.52 g/t Au over 2.1 metres in Zone 27. Mineralization consists of up to 3% pyrite, disseminated and stringers, hosted in moderate sericite altered rhyolite.

 

 

OSK-W-18-1597 intersected two intervals: 9.08 g/t Au over 2.1 metres in Caribou and 5.08 g/t Au over 2.5 metres in Zone 27. The first interval contains up to 1% pyrite, disseminated and clusters, hosted in moderate sericite and chlorite altered rhyolite. The second interval contains up to 20% pyrite-tourmaline stringers within a moderate sericite altered rhyolite.

 

 

OSK-W-18-1601 intersected 4.38 g/t Au over 2.0 metres in Caribou. Mineralization consists of 2% pyrite stringers, 1% sphalerite clusters and quartz veins hosted in a moderate sericite, moderate chlorite and weak fuchsite altered gabbro.

 

 

OSK-W-18-1602 intersected three intervals: 18.4 g/t Au over 2.0 metres, 7.94 g/t Au over 2.4 metres and 4.13 g/t Au over 2.0 metres in Caribou. The first interval contains trace disseminated and stringer pyrite within a moderate sericite altered rhyolite. The second interval contains 10% pyrite stringers, ptygmatic tourmaline veins and trace sphalerite and chalcopyrite hosted in a strong silica and moderate sericite altered felsic porphyritic intrusion.

 

 

OSK-W-18-1605 intersected 3.05 g/t Au over 2.0 metres in Zone 27. Mineralization contains up to 8% pyrite stringers and 1% disseminated pyrite at the contact between a sericite felsic porphyritic intrusion and a bleached andesite.

 

 

OSK-W-18-1607 intersected 3.89 g/t Au over 2.0 metres in Zone 27. Mineralization consists of 1% pyrite stringers within a moderate chlorite altered rhyolite.

 

 

OSK-W-18-1609 intersected two intervals: 5.54 g/t Au over 2.5 metres in Caribou and 4.69 g/t Au over 2.7 metres in Zone 27. The first interval contains up to 15% pyrite stockwork and 1% disseminated pyrite hosted in moderate sericite and weak silica altered rhyolite.

 

 

OSK-W-18-1611 intersected two intervals: 5.19 g/t Au over 2.1 metres in Caribou and 5.41 g/t Au over 2.1 metres in Zone 27. The first interval contains 80% massive pyrite and pyrite stockwork hosted in a strong sericite and silica altered felsic porphyritic intrusion. The second interval contains 2% pyrite clusters, 1% pyrite stringers and fine disseminated pyrite hosted in a moderate chlorite altered andesite.

 

 

OSK-W-18-1614 intersected two intervals: 6.47 g/t Au 2.1 metres and 34.8 g/t Au over 4.3 metres in Zone 27. The first interval contains pyrite stringers within a strong sericite and fuchsite altered contact between a gabbro and a fragmental andesite. The second interval contains 20% pyrite stringers and 2% disseminated pyrite within a strong sericite altered fragmental andesite.

 

 

OSK-W-18-1617 intersected 3.49 g/t Au over 2.6 metres in Caribou. Mineralization consists of 20% pyrite stringers, 10% sphalerite, pyrite-silica flooding and 1% pyrite-tourmaline veins hosted in moderate sericite and silica altered rhyolite.

 

 

OSK-W-18-1631 intersected 17.1 g/t Au over 2.0 metres in Zone 27. Mineralization consists of trace pyrite stringers and clusters within a strong sericite altered felsic dike.

 

 

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 currently unknown but is estimated at 65-80% 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 an Aqua Regia-ICP-AES 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 Lake Gold Deposit

 

The Windfall Lake gold deposit is located between Val-d’Or and Chibougamau in the Abitibi region of Québec, Canada. The mineral resource defined by Osisko, as disclosed in the Windfall Lake Technical Report (as defined below), comprises 2,382,000 tonnes at 7.85 g/t Au (601,000 ounces) in the indicated mineral resource category and 10,605,000 tonnes at 6.70 g/t Au (2,284,000 ounces) in the inferred mineral resource category. For details regarding the key assumptions, parameters and methods used to estimate the mineral resources presented in respect of the Windfall Lake gold project, please see the technical report entitled “Technical Report and Mineral Resource Estimate for the Windfall Lake Project, Windfall Lake and Urban-Barry Properties” and dated June 12, 2018 (effective date of May 14, 2018), which has been prepared by InnovExplo Inc. from Val-d’Or, Québec (the “Windfall Lake Technical Report”). The Windfall Lake Technical Report is available on Osisko’s website at www.osiskomining.com and on SEDAR under Osisko’s issuer profile at www.sedar.com). The Windfall Lake gold deposit is currently one of the highest grade resource-stage gold projects in Canada. Mineralization occurs in four principal zones: Lynx, Zone 27, Caribou and Underdog. All zones comprise sub-vertical lenses following intrusive porphyry contacts plunging to the northeast. The deposit is well defined from surface to a depth of 900 metres and remains open along strike and at depth. Mineralization has been identified only 30 metres from surface in some areas and as deep as 1,200 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% in the high-grade Windfall Lake 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 Quevillon area (over 3,300 square kilometres), a 100% interest in the Marban project located in the heart of Québec’s prolific Abitibi gold mining district, and properties in the Larder Lake Mining Division in northeast Ontario, including the Jonpol and Garrcon deposits on the Garrison property, the Buffonta past producing mine and the Gold Pike mine property. The Corporation also holds interests and options in a number of additional properties in northern Québec and Ontario.

 

Posted August 8, 2018

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