- SMDI #
- 2737
- Current Showing Name
- Drill Holes VR-3 to VR-10 or C Conductor Zone or Wide Lake Uranium Zone or Centennial Uranium Deposit
- Historical Showing Names
- Drill Holes VR-3 to VR-10 or C Conductor Zone or Wide Lake Uranium Zone or Centennial Uranium Deposit
- Company Name
- Project Name
- UTM Easting (NAD83 Z13)
- 348035.7000
- UTM Northing (NAD83 Z13)
- 6391143.2100
- NTS Sheet
- 074G12
- TRM (Township-Range-Meridian)
- 99-10-3
- Primary Commodities
- Uranium
- Associated Commodities
- Iron
- Discovery Type
- Drillhole
- Status
- Prospect: Primary Exploration
- Geological Details
- Drill hole VR-3, the discovery hole, was spudded 2.2 miles (3.54 km) east southeast of the southeast bay on MacFarlane Lake and 9.2 miles (14.8 km) east northeast of SMDI 2540 or drill hole DF-3. The hole, which is located at Wide Lake grid coordinates 48+00N and 196+00E, was completed to test the C conductor.
The showing area is underlain by Virgin River Domain rocks that have been unconformably covered by Athabasca Group sandstones. The Virgin River Domain, in the showing area, has been metamorphosed to upper amphibolite facies then retrograde metamprohosed to upper greenschist facies.
In the showing area,these rocks occupy a broad magnetic low. The strike extrension of the Virgin River Shear Zone cross-cuts this sequence of rocks. Three main deformational events effected these rocks. The F1 event resulted in small isoclinal folds. The F2 event produced regional northeast-trending folding, The F3 event produced regional east-west trending folding that was followed by migmatization and mylonitization. Locally, a F4 event gave small-scale folding and local banding to the mylonites.
At Drill Hole VR-3, the Athabasca Group is unconformably overlain by 6.3 m (20.7 ft) of glacial drift overburden.
The upper Athabasca Group consists of 612.7 m (2010.2 ft) of Manitou Falls D member (MFd) or fine- to coarse-grained sandstone with clay interclasts. The sandstone is weakly to moderately limonitized, hematized (red and maroon), silicified, and clay altered. The sheared and brecciated sandstone is locally intruded by narrow diabase dykes. From 328.5 to 455.3 m, the sandstone contains numerous pebbles and only rare clasts and resembles the Manitou Falls Member A. This sheared interval is mineralized. From 619.0 to 694.1 m (2030.8 to 2277.2 ft), one finds Manitou Falls C Member (Mfc) or medium- to coarse-grained sandstone with disseminated pebbles and pebble bands. Unit Mfc exhibits strong maroon hematization and weak red hematization as well as silicification and local concentrations of sooty pitchblende along fracture planes. Unit Mfc is underlain by 192.1 m (694.1 m to 886.2 m) of Manitou Falls Member A (Mfa) or medium- to coarse-grained sandstone with local pebbles and rare pebble bands. The sandstone is red-altered, silicified, pyritized, clay-altered, and strongly fractured and brecciated.
Unit Mfa is unconformably underlain by Virgin River Domain Precambrian basement rocks. The first 14.6 m of basement rocks consists of red-altered (886.3 to 890.0) and red-green-altered (890.0 to 900.3) fine- to coarse-grained intrusive rock. This, in turn, is underlain by a series of banded to foliated, fine- to medium-grained metasedimentary schists that have been intruded by diorite.
The mineralization in drill hole VR-3 is found within a sheared and brecciated interval of Mfa sandstone. Sooty pyrite and sooty pitchblende occurs as fracture plane infillings and as coatings on bedding planes.
DRILLHOLE INTERSECTION WIDTH PPM PPM PPM PPM PPM INTERVAL
NUMBER (M) (M) U MO ZN CO CU DESCRIPTION
___________________________________________________________________________
VR-03 825.0 - 825.5 0.5 5750 136 283 1062 307 sheared Mfa
826.5 - 827.0 0.5 1620 3 3 0 0 sheared Mfa
827.5 - 828.0 0.5 3600 7 3 0 86 sheared Mfa
829.0 - 829.5 0.5 1620 28 8 1 29 sheared Mfa
829.5 - 830.0 0.5 1650 3 22 2 24 sheared Mfa
830.0 - 830.5 0.5 1520 3 11 6 41 sheared Mfa
830.5 - 831.0 0.5 1770 8 5 3 17 sheared Mfa
831.0 - 831.5 0.5 1240 3 4 3 8 sheared Mfa
831.5 - 832.0 0.5 1432 3 7 3 7 sheared Mfa
832.0 - 832.5 0.5 5440 2 6 3 22 sheared Mfa
832.5 - 833.0 0.5 2600 1 5 3 5 sheared Mfa
833.0 - 833.5 0.5 4710 1 8 3 8 sheared Mfa
833.5 - 834.0 0.5 19800 12 34 21 20 sheared Mfa
834.0 - 834.5 0.5 8810 1 8 6 5 sheared Mfa
834.0 - 834.5 0.5 2100 3 4 2 2 sheared Mfa
834.5 - 835.0 0.5 4440 1 4 4 5 sheared Mfa
835.0 - 835.5 0.5 2290 1 4 8 4 sheared Mfa
839.0 - 839.5 0.5 2430 1 24 2 6 sheared Mfa
VR-04 810.5 - 811.0 0.5 1750 61 15 3 4 sheared Mfa
818.0 - 818.5 0.5 1417 7 130 237 75 faulted Mfa
VR-08 815.6 - 815.7 0.1 4800 9 123 94 37 breccia Mfa
VR-16 845.5 - 846.0 0.5 1500 - --- 9 189 unconformity
846.6 - 847.0 0.4 2680 - --- 9 124 qte-clay bx
887.0 - 887.5 0.5 838 - --- 1 1 alter pelite
888.0 - 888.5 0.5 817 - --- 0 0.5 alter pelite
888.5 - 889.0 0.5 625 - --- 1 0.4 alter pelite
889.0 - 889.5 0.5 536 - --- 1 0.3 alter pelite
889.5 - 890.0 0.5 590 - --- 1 1.1 alter pelite
- Geological Domain
- Mudjatik
- Host Rocks
- Host Minerals
- Pyrite
- Indicators
- Exploration History
- 11/1/2002 On 4 August 1977, Eric Partridge staked the showing area as CBS 5072 for Denison Mines Ltd. In the following year, Denison flew an airborne radiometric and magnetic survey and completed follow-up prospecting, geological mapping, soil and lake sediment sampling, and ground EM and magnetic surveys on the property (AF 74G12-0007 and -0008). In 1979, further prospecting, mapping, lake sediment and radon surveys (AF 74G12-0009). In 1980, further prospecting, lake sediment sampling, EM surveys and radon gas surveys were completed (AF 74G12-0018). In 1981, drill holes ML81-1 to 81-3 were completed (AF 74G12-0020). No significant mineralization was encountered. The claim block lapsed on 1 March 1981.
On 21 April 1987, Uranerz Exploration and Mining Limited staked the showing area as S-98157. No work was reported on the claim and it lapsed on
3 July 1989.
On 1 December 1994, Uranerz Exploration and Mining applied for MPP 1176 over the showing area. In 1995, Uranerz completed a reconnaissance boulder sample and outcrop sample survey, surficial air photo geology, and ground TDEM surveys on the property (AF 74G14-0012). In the following year, Uranerz continued the boulder sample survey, verified sample results by pitting and sampling, and completed a ground UTEM/TDEM survey on the claim (AF 74G-0015). On 11 December 1996, the area was staked as CBS 7794 within MPP 1176 by Rod Spooner for Uranerz Exploration and Mining Limited. The remainder of the MPP was allowed to lapse.
In 1997, Uranerz Exploration and Mining completed a ground TDEM survey and follow-up drill holes VR-1 and VR-2 to the immediate north of the showing area (AF 74G12-0034). In 1998, a partnership involving Uranerz (98%) and Coronation Mines (2%) completed an airborne GEOTEM EM and magnetic survey over the claim block and followed this up by drilling holes VR-3 to VR-10 (AF 74G-0016). Hole VR-3 encountered the mineralization that constitutes the showing. Holes 4 to 10 were completed to further test and delineate the mineralization. In 1999, a partnership involving Uranerz, Cameco, and Cogema Resources completed ground TDEM, gravity, and level surveys on grid VR-99 and drill holes VR-11 and VR-12 to further test the mineralization encountered by drill hole VR-3 (AF 74G12-0036). The drill holes failed tointersect significant mineralization. Hole VR-11 returned a maximum probe value of 312 cps on Mfa sandstone and hole VR-12 had a maximum reading of 2,341 cps in Mfa sandstone.
In the spring of 2000,the partnership completed ground TDEM, magnetic, gravity, and levelling surveys and follow-up drill holes VR-13, VR-14, and VR-14W1 on the VR-2000 grid (AF 74G12-0037). The maximum scintillometer reading for these holes is 100 cps.
On 21 August 2001, the claim block was transferred 100% to UEM Inc. In the following year, a partnership involving UEM Inc., Cameco, and 2% Formation Capital completed drill hole VR0-16 on the showing and dr-sampled and completed core petrographic studies on holes VR-06, VR-07, VR-11 to -13, and VR-14W (AF 74G12-SE-0039). Better intersections are reported above.
In 2003, a partnership involving Cameco and Cogema completed ground TDEM and pole-dipole resistivity surveys that covered the showing and they re-examined historic hole MC-02 located to the southwest of the zone (AF 74G12-SE-0040). In the same year, a UEM Inc.-Cameco-Cogema Resources-Formation Capital joint venture completed a core study of drill holes VR-5, VR-11, VR-13, VR-15, and VR-16, a drill hole review for drill holes VR-3 to -8 and -11 to -16 as well as ground TDEM and IP/Resistivity surveys (AF 74G12-SE-0041).
- Production History
- Reserves and/or Resources