Details


SMDI #
2529
Current Showing Name
McClean Lake Uranium Deposit [Caribou, McClean North, Sue D, Sue E, Ore Stockpile]
Historical Showing Names
McClean Lake Uranium Deposit, McClean Lake Uranium Deposit [Caribou, McClean North, Sue D, Sue E, Ore Stockpile], Sue A Deposit; Sue B Deposit; Sue C Deposit; Sue C-1 Open Pit; Sue CQ Zone; Sue CQQ Zone; Sue D Zone; Sue E Zone; McLean Pod
Company Name
Orano Canada Inc., Denison Mines Corp.
Project Name
McClean Lake
UTM Easting (NAD83 Z13)
570230.0000
UTM Northing (NAD83 Z13)
6458465.0000
NTS Sheet
064L05
TRM (Township-Range-Meridian)
107-11-2
Primary Commodities
Uranium
Associated Commodities
Arsenic, Cobalt, Copper, Lead, Nickel
Discovery Type
Status
Deposit: Development
Geological Details
The mineralization which constitutes the Sue Deposit occurs in three small pods which have been designated the SUE A, B, and C zones. The Sue A Zone is located 2.9 km (1.8 miles) east-northeast of the McClean North Deposit or SMDI 1718. The Sue B Zone is located 350 m (1148.3 ft) north northeast of the Sue A Zone and the Sue C Zone is located 60 m (196.9 ft) south of the Sue A Zone. The Sue Deposits lie on the western flank of the Collins Bay high along a north-trending graphitic (1 to 70%) quartz-feldspar-biotite-cordierite gneiss horizon. This horizon, approximately 1 km north of the Sue B Deposit, is folded sharply to the west and eventually the horizon links up with the structure controlling the McClean Deposits. In the immediate deposit area, the graphitic gneiss is in fault contact to the east with feldspathic gneisses and granitoids to pegmatoids. To the west, the horizon is in gradational contact with a series of intermediate gneisses. Combined normal and reverse faults, which parallel the east-dipping graphitic gneiss, have offset the regolith between the Athabasca Formation sandstones and the underlying graphitic gneiss by up to 20 m (65.6 ft). Reverse faulting has resulted in a stepping-down of the regolith in a westward direction. The Sue A and B deposits occur along the western flank of a 8 to 10 m (26.2 to 32.8 ft) high basement horst. In is felt that a series of northeasterly- and northwesterly-trending faults offset the major north-south-trending structures and limit the extent of mineralization along the north-south structures. The Sue A Deposit (58°15'42",103°48'11"), which lies between 60 and 75 m (196.9 to 246.1 ft) below the surface, strikes N12°E. The deposit has been traced along strike for 176 m (577.4 ft) and across width which varies from 8 to 30 m (averaging 15 to 20 m). The Deposit lies on and immediately above the unconformity in an envelope of massive earthy-red clay within the Athabasca Formation sandstones (only minor amounts of uranium mineralization extend into the basement graphitic gneisses along fault planes). The mineralization, which is extensively fault-controlled, terminates against the northeast-trending VAS Fault to the south and against the northeast-trending AJ Fault to the north. This results in a flattened, west-dipping deposit which follows the down-stepping of the unconformity to the west. The mineralization present at the Sue A Deposit is dominantly coffinite along with minor nodular pitchblende and crystalline uraninite. Niccolite (in a 4:1 ratio with U3O8), nickel and silver arsenides, cobalt minerals, molybdenum, vanadium, galena, and copper minerals are also present in anomalous amounts. The Sue B Deposit (58°15'54",103°48'06"), which is located 350 m (1148.9 ft) north of the Sue A Deposit, consists of a 90 m (295.3 ft) long by average 40 m (131.2 ft) wide zone of mineralization within the sandstone which consists of two distinct mineralized horizons. The upper zone, which contains 75% of the deposit ore, lies at a depth of 20 m (65.6 ft), is about 20 m (65.6 ft) above the unconformity, and is 50 m (164.0 ft) long by 26 m (85.3 ft) wide by 17 m (55.8 ft) thick. The upper zone tapers to 0 m thickness within 10 to 25 m (32.8 to 82.0 ft) along strike. The upper zone ore is hosted by earthy-red clay within weakly silicified sandstone. Ore is controlled by a series of intersecting conjugate faults. The lower zone, which lies on and immediately below the unconformity at a depth of 60 to 75 m, occurs on the western flank of a 20 m (65.6 ft) high basement high. Lower zone ore, which is fault-offset to the west of the upper zone mineralization, is hosted within a earthy-red clay within non-silicified, faulted sandstone. The two zones are connected by vertical, fault-controlled, chimney-like zones of mineralization. Like the A Deposit, The Sue B Deposit ore is limited along strike to the north and south by two northwest-trending faults. The Sue B Deposit is a medium-grade deposit with a mineralogy that is identical to that found at the Sue A Deposit. The structurally controlled Sue C Deposit (58°15'36",103°48'11"), which is located 60 m (196.9 ft) south of the south end of the Sue A Deposit, trends N12°E for 325 m (1066.3 ft) within a 4 m (13.1 ft) wide, 70° to 80°SE-dipping structure. The deposit occurs on the west limb of the Collins Bay granitic dome at an average depth of 76 m (249.3 ft). The deposit is overlain by ~68 m (223.1 ft) of Athabasca Group sandstone and 8 m (26.3 ft) of glacial till. The mineralization continues south of the main C Deposit as a broad area of disseminated mineralization which is referred to as the CQ Deposit. The unconformity at the C Deposit steps down to the west (a local basement relief of 10 to 30 m) and local northeast- and northwest-trending faults offset the structure by 2 to 5 m (6.6 to 16.4 ft). The Sue C Deposit consists of high-grade uranium mineralization within a steeply dipping, gently south-plunging vein. The orebody is restricted to to the basement (mine sequence: graphitic gneiss, garnet-cordierite-sillimanite gneiss, hematite-rich gneiss and foliated quartzite) and does not appear in the overlying sandstones. The 250 m (820.2 ft) long by 10 m (32.8 ft) wide (average) zone of mineralization (a series of south-plunging ore shoots) subcrops at the unconformity in the north and central portions. The central portion of the deposit, which is 80 to 100 m (262.5 to 328.1 ft) wide, contains 65% of the known reserves in a single high-grade lens. To the north, the deposit thins to 1 m and extends to 1 m below the unconformity. To the south, the top of the deposit drops away from the unconformity through a transitional zone, which contains lenses of high-grade ore in vein-like structures, into the CQ Zone. The mineralization consists of massive uraninite with pitchblende and minor coffinite which is hosted in a clay matrix and argillized gneisses, as well as lenses of massive pitchblende. There are only minor amounts of other associated metallic minerals present (0.1% Ni and As, 0.35% Pb, 0.25% Va, and minor Mo, Cu, and Co). Three different types of ore were recognized by G. Tourigny: (1) foliation-parallel veinlets and disseminations: spacing between veinlets is irregular and vertical continuity of mineralized veins is interrupted by croscutting band-like fractures and foliation-parallel boudinage. (2) Mineralization within shear veins and extensional veins: pitchblende- hematite-clay-rich stringers occur within subvertical to steeply east- dipping shears which are <2 m thick and 2 to 10 cm thick en echelon entensional veins of pitchblende (representing mineralized hybrid extensional shear fractures). (3)Massive ore: black pods and nodules of pitchblende which range from a few decimeters up to 1.5 m in diameter. A brecciated massive ore (fragments of quartz-cordierite-garnet gneiss supported by a pitchblende-yellow uranium oxides-hematite-clay matrix) formedduring brittle slip events. The Sue C Deposit is located within an 10 to 30 m (32.8 to 98.4 ft) wide, north-northeast-trending, 70 to 75° east-dipping anastamosing fault zone which has a vertical displacement of 10 to 20 m (16.4 to 32.8 ft). Within this fault, one finds a series of shallow, flat-dipping faults which create a series of flat steps that offset the main ore zone and which control the distribution of high grade ore lenses. The CQ Zone, which is separated from the Sue C Zone by a major NNW-trending fault, is a 125 m (410.0 ft) long by 20 to 30 m 64.8 to 98.4 ft) wide by 40 to 120 m deep (45 m below the unconformity) block of disseminated uranium mineralization which is hosted by foliated graphitic metasediments. The CQ orebody, which extends from 7+12.5S to 8+37.5S, consists of a series of vertically discontinous, moderately dipping lenses of coffinite- and pitchblende-rich altered gneisses which occur within a NNW-SSE-trending fault set. The mineralization is bounded to the west by the contact between the host gneisses and a silicified zone. The CQQ Zone, which is located 150 m (492.1 ft) south of the CQ Zone, was first encountered by drill hole S285. The basement-hosted mineralization is overlain by 75 to 80 m (246.1 to 262.5 ft) of basal Athabasca Group medium- to coarse-grained sandstone with conglomerate interbeds. The zone consists of a moderately to steeply east-dipping zone of multiple stacked veins of CQ-style ore which extends almost up to the unconformity. The mineralization is hosted within a series of graphitic gneisses, "quartzite" units, and, to a lesser extent, within intermediate gneisses which dip 20°-30°E immediately below the unconformity. The dip steepens to 70°E with depth. The hanging wall rocks consist of a 20 m (65.6 ft) thick sequence of graphitic intermediate gneisses which are bounded above and below by a fine- to medium-grained, graphite-depleted intermediate gneiss. The footwall, like the footwall of the C and CQ zones, is characterized by a 1 to 2 m thick quartzite which is bounded above and below by a strongly silicified intermediate gneiss. This sequence of strongly argillized, chloritized, clay-altered, and hematized rocks are cross-cut by a series of foliation-parallel, shallow-dipping normal and reverse faults which displace the unconformity by up to 5 m. The CQQ Zone mineralization consists of millimetric nodules of pitchblende, very rare uraninite crystals, and powdery coffinite which infills both foliation-parallel and cross-cutting fractures. The zone has an extensive halo of V, Ni, and As mineralization. As at the CQ Zone, the low grade mineralization which is extensive over several tens of meters contains local scattered areas of higher grade "nugget" mineralization. The mineralization, which has a width of <1.0 m to 21.5 m, occurs in a series of stacked irregular lenses or veins. Individual veins vary in length from 5 to 40 m and are from <1.0 to 10 m thick. Unlike the CQ Zone, the mineralization at the CQQ Zone extends upwards to within 2 or 3 m of the unconformity. Discovery drill hole S285 encountered 2 m which returned 0.29% U3O8. Follow-up holes S291 and S292 returned 0.32% U3O8 over 21.5 m and 0.27% U3O8 over 9.5 m respectively. The Sue D Zone, which is located on the edge of a gravity and resistivity low 125 m (410.0 ft) south of the Sue CQ Zone, is contained within the same north-south-trending reverse fault zone which hosts the Sue C and CQ zones. The 150 m (492.1 ft) long by 20 to 50 m (65.6 to 164.0 ft) wide by up to 100 m (328.1 ft) thick zone has a hangingwall sequence of 60° to 90° east-dipping graphitic intermediate gneiss and intermediate gneisses which contain numerous conformable coarse-grained injection pegmatoids. The footwall sequence, which hosts the D Zone, consists of a series of graphitic intermediate gneisses and intermediate gneisses which contain local strongly resilicified intervals. The structurally controlled D Zone mineralization is limited by the foliation and by a set of conjugate fault sets (a set of foliation-parallel faults which dip 60°-90°E and a set of 10° to 30°W-dipping faults which cross-cut the foliation) A dense and complex network of intersecting faults, which represent several generations of tectonic activity, control the mineralization. Basement alteration is variable. Green to grey green chloritization has been bleached or strongly altered to hematite-stained clay. Argillization and secondary silicification are present. The overlying sandstones are extensively fractured and exhibit bleaching, argillization, and clay alteration. The D Zone consists of a 10 m (32.8 ft) thick, irregular shaped, heterogenous lense which subcrops at the unconformity and which extends 80 m down dip. The geological setting of the Sue D Zone is similar to the Sue C and E deposits. The mineralized lense contains minor nickeline (NiAs), chalcopyrite, pyrite, and coffinite and massive pitchblende. The massive pitchblende occurs as nodules, massive veins, and as a breccia matrix within highly clay-altered, bleached, silicified, hematized, argillized, tourmalinized graphitic paragneiss and within mineralized clay. The Sue D Deposit has been subdivided into two broad zones. The upper zone consists of north-south-trending, east dipping, mineralized structures between line 9+62S and 10+62S. The mineralized zone, which is 20 m (65.0 ft) thick at the north end, pinches out at line 10+62S. The lower zone, which extends from line 9+87S to line 10+87S, occurs from 10 to 110 m below the unconformity, and is 10 to 30 m thick due to the stacking of the mineralized gneiss units. The Sue E Zone mineralization was first encountered in drill hole S-395 (14+00S and 19+15E). The 250 m (820.2 ft) long zone is 15 to 20 m (49.2 to 65.6 ft) wide at the south end and 5 m (15.2 ft) wide at the north end. The geological setting of the Sue E Zone is identical to that found at the Sue C Zone. The near vertical to steeply east-dipping, reverse fault-controlled mineralization consists of a matrix of pitchblende-rich hematized clay with local abundant visible niccolite within a sheared, chloritized, argillized, hematized, and strongly sheared. Sequence of interlayered, fine- to medium-grained graphitic gneisses and medium-grained pegmatoids. The high-grade ore, which pinches out at a depth of 130 m (426.5 ft) occurs as a massive replacement in graphitic gneisses in the zone of maximum shearing. Below 130 m (426.5 ft), lower grade ore occurs within a quartzitic unit of variable thickness. Locally, he quartzite is highly faulted and it forms a series of imbricated slabs. This quartzite and underlying pelites locally hosts discontinous zones of lower grade uranium mineralization that are often found along major subvertical faults. The south end of the zone consists of a >120 m long area of high grade mineralization. The northern lower grade portion of the zone has a strike length of 150 m (492.1 ft). Sue E Zone mineralization is controlled by subvertical reverse faults and related steeply east-dipping conjugate faults - a compressional stress system. The main reverse faults, which have a 10 to 12 m vertical displacement, subparallel the foliation.that subparallel the foliation.
Geological Domain
Wollaston
Host Rocks
Host Minerals
Arsenopyrite
Indicators
Exploration History
12/1/2023 A total of 19.23M lb (8723 t) tri-uranium octoxide (U3O8) was produced, the majority coming from the Cigar Lake (Cameco Corp.)–McClean Lake (Orano Canada Inc.) operation (Table 1), which accounted for 18.0M lb (8164.7 t) U3O8 (100 per cent basis) in 2022. Cameco forecasted a total production of 16.8M lb (7620.4 t) U3O8 in 2023, adjusting the 2022 number due to initiation of mining a new zone in the orebody and equipment reliability issues. (Saskatchewan Exploration and Development Highlights 2023, p.7) (See also Production and Reserves/Resources, from Saskatchewan Exploration and Development Highlights 2023, Table 1 & 2, p.7-8) 12/1/2024 In January 2024, Orano Canada Inc. (Orano) and Denison Mines Corp. (Denison) announced plans to restart uranium mining operations at the McClean Lake mine in 2025 with production of about 800 000 lbs triuranium octoxide (U3O8) expected that year. Orano and Denison plan to use the patented Surface Access Borehole Resource Extraction (SABRE) technology with recovered ore processed at the McClean Lake mill. (Saskatchewan Exploration and Development Highlights 2024, p.7) (See also Reserves/Resources, from Saskatchewan Exploration and Development Highlights 2024, Tables 2 & 3, p.7-9) 5/4/1993 In 1964, Compagnie de Mokta Ltee commenced uranium exploration in the Athabasca Basin. This work led to the discovery of the Cluff Lake Deposit in 1969. During the same period of time, Dynamic Group formed a joint venture with British American Oil Company to explore for uranium. Gulf Mineral Resources took over this partnership and discovered the Rabbit Lake Deposit in 1968. The discovery or the Rabbit Lake Deposit resulted in a rush of uranium staking and prospecting. By 1971, most of these uranium permits had lapsed. In 1974, a partnership involving Uranerz Exploration and Mining Company, Inexco Mining Company, and SMDC commenced an exploration program which culminated in the discovery of the Gaertner Deposit in 1975 and the Deilmann Deposit in 1976. On 12 August 1974, Vern Studer staked the showing area as CBS 3501 and transferred the property to Canadian Occidental Petroleum. Canadian Occidental commenced exploring the land between the Rabbit Lake Deposit and Midwest Lake for uranium. In 1975, a track etch survey was completed on the property. In 1976, the exploration program included percussion drilling, ground geochemical and geophysical surveys, and a follow-up track etch survey (AF 64L05-0024). In 1977, Canadian Occidental and Inco Limited formed a joint venture partnership to continue exploration of the property. Between 1977 and 1978, the partnership completed airborne geophysical surveys, ground EM surveys, and follow-up diamond drilling (AF 64L05-0023 and -0043). Continued drilling in 1979 resulted in the discovery of the McClean North Deposit (AF 64L05-0047 and -0048). From 1979 to 1980, twelve methods of ground geophysics (including magnetic and VLEM surveys) were completed over the McClean North Deposit area (AF 64L05-0075). On 14 January, 1980, drill hole number 1004 discovered the McClean South Zone. In 1980, airborne INPUT surveys were completed over the property (AF 74I-0005 to -0007). On 12 August 1980, CBS 3501 converted to ML 5290. Between 1980 and 1981, ground EM and magnetic surveys were completed over numerous grids (AF 64L05-0074). In 1981, Clark, Brummer, and Fogwill regionally geologically mapped the property. In the same year, a pre-feasibility study was completed. In 1983, a Canico-Canadian Occidental Petroleum joint venture completed muskeg sampling and a clay content of boulders study for the McClean Deposits (AF 64L05-0084). Lake water/sediment sampling (AF 74I01-0001) and ground EM and magnetic surveys (AF 64L05-0025, -0075, and -0077) were completed. In 1982, Asamera Corporation re-interpreted the 1980 GSC Cotran Survey (AF 64L05-0103). In the winter of 1984, a Canico-Canadian Occidental Petroleum joint venture completed ground VLF-EM surveys over the Black, Snake, and Misty grids on CBS 3501 to CBS 3505 (AF 64L05-0085) in addition to further diamond drilling (AF 64L05-0076). In January of 1985, the partners entered into a joint venture agreement with Total Minatco Company Ltd./Ltee. To further explore ML 5290. In 1986, further EM surveys and follow-up drilling was completed in the McClean to Lasby lakes area (AF 64L05-0118). In 1987, ground VLF-EM, HLEM, and magnetic surveys and drill holes SL-1 to -9 were completed on the Sue Lake grid (AF 64L05-0132). In 1988, further ground geophysics and percussion drilling was completed on the Sue Lake grid (AF 64L05-0133). This work resulted in the discovery of the Sue A and B zones. In 1989, further ground geophysics and diamond drilling was completed on the Sue Lake grid (AF 64L05-0134). This work resulted in the discovery of the Sue C Zone (discovery drill holes CS60 and CS34). In this year, Minatco retained SENES Consultants Limited to prepare an environmental Impact Study on the McClean, JEB, and Sue Deposits. Drilling on the Sue C Zone in 1990 outlined sufficent reserves to warrant possible mining of the C Zone when the A and B zones are mined. On 22 June 1990, the showing area was staked as CBS 7657 within ML 5290 and on 1 August 1990, the remainder of ML 5290 was allowed to lapse. In November of 1990, Minatco acquired the shares of Canadian Occidental and Inco in the project and became sole owner of the deposits. Minatco completed ground IP-resistivity and gravity surveys and drill holes S242 to S304 on the Sue Deposit C and CQ zones (AF 63L05-0135). Drill hole S285 discovered the mineralization which was named the Sue CQQ and Sue D zones. At this time, the deposit reserves were given. In 1991, hydrology test holes PV-6 to -13 were completed on the Sue A to C pit sites, drill holes S-305 to S-408 were completed on the Sue C, CQ, D and E Zones and extensions (AF 64L05-0136). The C and CQ zones were drilled at 12.5 m centres, the Sue D Zone was delineation drilled (14 holes), and drill hole S-395 discovered the Sue E Zone mineralization. In 1992, Minatco completed 87 drill holes (S-409 to 495) and VLF-EM, HLEM, and VLEM surveys were completed on the Sue grid (AF 64L05-0137). Twenty six holes tested the Sue D Zone, fourty two holes tested the Sue E Zone, and nineteen exploration holes were completed. In 1993, the Federal Environmental Assessment Review Office panel was convened to examine the McLean Deposit development proposal. The panel recommended that the project be placed on hold. Late in 1993, the Federal and Provincial Governments gave approval to start development of the ore bodies which constitute this deposit. It is proposed that both open pit and underground methods will be used to mine the zones which comprise the McClean Lake Uranium Deposit. The ore will be processed at the McClean Project mill. In the same year, the partners completed a ground IP/resistivity survey on the Sue grid and further delineation drilling (S-525 to S-555) and condemnation drilling (S-556 to S-571) on the A, B, and C Zones and drill holes S-496 to S-524 were completed to test the Sue North area north of the Sue B Zone (AF 64L05-0138). In 1994, Cogema Canada Inc completed ground gradient array resistivity, VLF-R, and HLEM surveys on the Sue grid (AF 64L05-0142). In 1997, the Sue C Deposit open pit mine commenced stripping operations. In the same year, a Cogema-Minatco partnership completed drill holes S-572 to -594 on the Sue D Zone and a boulder sample survey over the Sue zones (AF 64L05-0143). In the 24 August 1998, Northern Miner (page 3) it was announced that the Atomic Energy Control Board had approved the tailings storage at McClean Lake. The hearing to obtain a mining licence is is scheduled for November of 1998. At this time mineable reserves for McClean Lake were given as 720,000 tonnes grading 3.15% U3O8. In later 1998, the Sue C Deposit open pit was commenced. Ore will likely be encountered by Christmas of 1998 and production is expected to begin early in 1999 (once regulatory approval is granted). The ore was stockpiled and then run through the McLean Mill which useed the JEB Open Pit as a tailings pond. As of 31 December 1997, Denison Mines Limited gave the estimated proved mineable reserves for the Sue Deposits. In 1999, the Sue C open pit was developed to a depth of 80 m (immediately above the ore). This pit will be used to mine both of the Sue A and Sue C deposits. The Sue B deposit will mined as a separate pit. It is planned that the deposits be mined out by 2003 (1999 Exploration and Development Highlights). At the end of 2000, the Sue Pit had 27,340,000 lbs U3O8 in situ. The first yellowcake was produced on 8 July 1999. In January 2000, mining removed ore from the Sue C1 open pit and mining of waste rock from the Sue C2 underground mine commenced. Commercial production commenced on 1 February 2000. In 2001, a partnership involving Cogema Resources, Denison Mines, and OURD completed 31 drill holes (S-646 to S-676) and HLEM and TDEM surveys on the Sue B, D, and E deposits and a ground HLEM survey on the Moffat Nose grid (AF 64L05-SW-0154). Drill holes S-655 and S-659 encountered minor mineralization on the Sue D area and drill hole S-672 encountered minor mineralization where the Sue C trend intersects the Telephone Lake Fault. In the 5 February 2001, Northern Miner, it was announced that McClean mine was the first Canadian mine to be awarded an environmental management certificate. In 2001, the Sue C1 pit was mined out to a depth of 100 m (ore was stockpiled in the pit) and the Sue C2 extension pit had reached a depth of 30 m and was still in sandstone. It was planned that the Sue deposits would be mined out by 2003. On 11 November 2001, Sue C mining set a production record. Over 1,200,000 lbs of ore grading just over 10% U3O8 was mined from the C pit within a 24 hour period. In the winter of 2001, Cogema Resources Inc.and Cameco Corporation completed 28 delineation drill holes (S-624 to S-645 and S-677 to S-682) on the Sue E deposit (AF 64L04-NW-0112). In the December 2001 Cogema Communique, Cogema announced that by the end of December 2001, the Sue C2 extension pit will be mined out. At this point, Cogema stated that they would have enough ore stockpiled to feed the mill for four to five years. Therefore, Cogema announced that it would suspend mining operations. After Christmas, employees would relocate JEB and Sue special waste stockpiles to the mined-out Sue C pit and they would haul stockpiled ore from the mine to the mill storage pad. Once this was completed, the Sue site will shut down. On 29 April 2002, CBS 6802 was re-staked as S-106953 and S-106954. In a news release dated 02 May 2002, Denison Mines Ltd. Announced that the mining of the Sue C deposit was completed on 3 February 2002. At the time of closure, the Sue C1 extension pit was mined out at a depth of 100 m (328.1 ft) and the C2 extension pit was mined out at a depth of 143 m (469.2 ft). The pit produced 650,000 tonnes of ore grading 2.6% U3O8 (14,031 t U or 36.4 M lb U3O8). On 22 June 2006, CBS 7657 was re-staked as ML 5514. In 2002, Cameco completed ground TDEM and HLEM surveys that covered the Sue E orebody (AF 64L04-NW-0113).In the same year, an airborne AeroTem survey was flown which covered the deposits and ground TDEM and Resistivity surveys were completed to the northwest of the deposits on the Caribou Grid (AF 64L05-SW-0156). Denison Mines announced, with the closure of the Sue C Pit, that about 33% more uranium than had been anticipated had been added to surface stockpiles. All mining would cease for the next few years and mineral exploration at McClean would cease until ground conditions improve and until drill results have been assessed. Mining of Sue C Pit ore was completed in February of 2002. The Sue C orebody provided 650,000 t of ore grading just over 2.6% U3O8 and the deposit produced 36.4 M lbs U3O8. At this time, it was suggested that future development of the Sue A deposit would occur from an extension of the Sue C pit and the Sue B deposit would require a separate pit. In 2003, milling of stockpiled ore continued at the McClean Lake mill. At this point, Cogema estimated that the Sue E deposit would be mined in 2005 (depending on the regulatory review results). In 2005, stockpiled Sue C Deposit ore was milled. Mining of the Sue A deposit commenced in July of 2005. In the first year, 3,513,452 tonnes of waste (overburden) was mined. The first ore was mined in December 2005. The deposit should be mined out in February of 2006. Pre-mining overburden stripping at the Sue E deposit commenced in September of 2005. Ore will not be reached until the summer of 2006. In 2006, test mining of the McLean Pod commenced. Initially, it was felt that the pod would be mined using underground methods. The Mine Equipment Development Project (MED) was tasked with testing the feasibility of mining this pod remotely using jet boring ore extraction techniques.
Production History
Production Period: 2022-01-01 to 2022-12-31 Orano Canada Inc.: Summary: - Uranium Production Period: 2006-09-01 to 2006-12-31 Sue E (open pit) 20,640.00 tonnes SUE E OPEN PIT MINE PRODUCTION YEAR TONNES MILL HEAD RECOVERY POUNDS U3O8 YEAR END MINING MILLED GRADE RATE % PRODUCED RESERVES COMMENTS _____________________________________________________________________________ 2005 0 1,262,492 t overburden waste removed 8,945 start Sept '05 2006 20,640 8.90 94.5 432,627 7,472 Ore mining start Sept 2006 _____________________________________________________________________________ _____________________________________________________________________________ Summary: - Uranium: 432,627.00 lb @ 8.90 Production Period: 2006-01-01 to 2006-12-31 Sue C (open pit) 81,196.00 tonnes Mill stockpile adjust -110,115 kg U SUE C OPEN PIT MINE PRODUCTION YEAR TONNES MILL HEAD RECOVERY POUNDS U3O8 YEAR END MINING MILLED GRADE RATE % PRODUCED RESERVES COMMENTS _____________________________________________________________________________ 1999 0 0.00 0.0 0 26,753 Klbs in situ 2000 25,751 53.30 97.8 3,558,113 18,132 Klbs in situ 2001 51,938 44.74 98.2 6,041,423 1,476 Klbs in situ 2002 103,645 29.30 97.9 5,599,352 0 Klbs deposit mined out, mill stockpile 2003 89,333 23.80 97.7 5,527,111 0 Klbs stockpile mill 2004 152,357 15.80 97.3 6,004,920 0 Klbs mill stockpile 2005 176,350 12.30 97.1 5,483,940 0 KLbs Mill stockpile adjust -662,543 KgU 2006 81,196 3.50 94.5 676,652 0 KLbs Mill stockpile adjust -110,115 KgU _____________________________________________________________________________ Summary: - Uranium: 676,652.00 lb @ 3.50 Production Period: 2006-01-01 to 2006-12-31 Sue A (open pit) 28,637.00 tonnes SUE A OPEN PIT MINE PRODUCTION YEAR TONNES MILL HEAD RECOVERY POUNDS U3O8 YEAR END MINING MILLED GRADE RATE % PRODUCED RESERVES COMMENTS _____________________________________________________________________________ 2005 188 11.90 97.1 5,676 1,233 Klbs in situ 2006 28,637 10.00 94.5 678,729 0 Klbs Mining ceased end March 2006 - Ore stockpiled _____________________________________________________________________________ Summary: - Uranium: 678,729.00 lb @ 10.00 Production Period: 2006-01-01 to 2006-12-31 McClean (underground) 41.00 tonnes McCLEAN UNDERGROUND MINE EQUIPMENT DEVELOPMENT PROJECT (MED) YEAR MINED ORE MILLED MILL RECOVERY PRODUCED YEAR END MINING AND WASTE TONNES HEAD RATE % LBS U3O8 RESERVES COMMENTS TONNES GRADE _____________________________________________________________________________ 2006 41 41 66.8 94.5 6,406 10,711 Test Project Summary: - Uranium: 10,711.00 lb @ 66.80 Production Period: 2005-07-01 to 2005-12-31 Sue A (open pit) 188.00 tonnes It was planned that the Sue A Open Pit started mining in July of 2005 and the Sue E Open Pit began overburden stripping in September of 2005 and commenced mining in September of 2006. The B, D, and F deposits are being left for the future. Summary: - Uranium: 5,676.00 lb @ 11.90 Production Period: 2005-01-01 to 2005-12-31 Sue C (open pit) 176,350.00 tonnes Mill stockpile adjust -662,543 kg U Summary: - Uranium: 5,483,940.00 lb @ 12.30 Production Period: 2004-01-01 to 2004-12-31 Sue C (open pit) 152,357.00 tonnes Mill stockpile Summary: - Uranium: 6,004,920.00 lb @ 15.80 Production Period: 2003-01-01 to 2003-12-31 Sue C (open pit) 89,333.00 tonnes mill stockpile Summary: - Uranium: 5,527,111.00 lb @ 23.80 Production Period: 2002-01-01 to 2002-12-31 Sue C (open pit) 103,645.00 tonnes Mining of the Sue C Pit ceased on 3 February 2002. Mining ceased due to the depletion of reserves at the Sue C deposit. Summary: - Uranium: 5,599,352.00 lb @ 29.30 Production Period: 2001-01-01 to 2001-12-31 Sue C (open pit) 51,938.00 tonnes in situ Summary: - Uranium: 6,041,423.00 lb @ 44.74 Production Period: 2000-01-01 to 2000-12-31 Sue C (open pit) 25,751.00 tonnes In 1999, production commenced at the Sue C open pit. Summary: - Uranium: 3,558,113.00 lb @ 53.30
Reserves and/or Resources
2024-12-01 Summary: McClean North: Measured and Indicated Mineral Resource - Uranium: 12,200,000.00 lb @ 2.8 % Sue E: Inferred Mineral Resource - Uranium: 7,300,000.00 lb @ 0.69 % McClean Lake ore stockpile: Proven and Probable Mineral Reserve - Uranium: 700,000.00 lb @ 0.37 % McClean North: Inferred Mineral Resource - Uranium: 10,000.00 lb @ 0.79 % Sue D: Inferred Mineral Resource - Uranium: 20,000.00 lb @ 0.39 % Caribou: Measured and Indicated Mineral Resource - Uranium: 2,800,000.00 lb @ 2.6 % Sue D: Measured and Indicated Mineral Resource - Uranium: 2,800,000.00 lb @ 1.1 % 2023-12-01 Summary: McClean North: Measured and Indicated Mineral Resource of 12,400,000.00 lb - Uranium @ 2.8 % McClean Lake ore stockpile: Proven and Probable Mineral Reserve of 730,000.00 lb - Uranium @ 0.37 % Caribou: Measured and Indicated Mineral Resource of 2,800,000.00 lb - Uranium @ 2.6 % Sue E: Inferred Mineral Resource of 7,300,000.00 lb - Uranium @ 0.69 % Sue D: Measured and Indicated Mineral Resource of 2,800,000.00 lb - Uranium @ 1.1 % Sue D: Inferred Mineral Resource of 200,000.00 lb - Uranium @ 0.39 % McClean North: Inferred Mineral Resource of 100,000.00 lb - Uranium @ 0.79 % 2021-12-31 Summary: McClean North: Indicated Mineral Resource of 204,300.00 tonne - Uranium: 12,200,000.00 lb @ 2.8 % Sue D: Inferred Mineral Resource of 24,200.00 tonne - Uranium: 200,000.00 lb @ 0.39 % McClean North: Inferred Mineral Resource of 3,300.00 tonne - Uranium: 100,000.00 lb @ 0.79 % Ore Stockpile: Proven Mineral Reserve of 90,000.00 tonne - Uranium: 726,000.00 lb @ 0.37 % Sue E: Inferred Mineral Resource of 483,400.00 tonne - Uranium: 7,300,000.00 lb @ 0.69 % Caribou: Indicated Mineral Resource of 47,800.00 tonne - Uranium: 2,800,000.00 lb @ 2.6 % Sue D: Indicated Mineral Resource of 122,800.00 tonne - Uranium: 2,800,000.00 lb @ 1.1 % 2015-01-01 NI 43-101-compliant Measured and Indicated Resource for the Sue D deposit was 121,200 tonnes grading 1.05% U3O8 for 2.8 M lb U3O8. Inferred Resource for the Sue E deposit was 480,900 tonnes grading 0.69% U3O8 for 7.3 M lb U3O8. Summary: Sue E: Inferred Mineral Resource of 480,900.00 tonne - Uranium: 7,300,000.00 lb @ 0.69 % Sue D: Measured and Indicated Mineral Resource of 121,200.00 tonne - Uranium: 2,800,000.00 lb @ 1.05 % 2005-01-01 Reserves (in situ and stockpiled) of 32.9 M lbs U3O8. Summary: Reserves (in situ and stockpiled): Historic reserve (unspecified) - Uranium: 32,900,000.00 lb 2002-12-31 Cogema – Denison – OURD Sue A, B, C, D: 14,115 t U grading 1.53%. Summary: Sue A, B, C, D: Historic resource (unspecified) - Uranium: 14,115.00 tonne @ 1.53 % 2001-01-01 A preliminary estimate of the Sue E Zone indicates about 8 million lbs U3O8 at a grade of 0.98% U3O8. Summary: Sue E: Historic resource (unspecified) - Uranium: 8,000,000.00 lb @ 0.98 % 1998-08-24 Cogema – Minatco Mineable reserves - McClean Lake deposits: 720,000 tonnes grading 3.15% U3O8. Summary: McClean Lake deposits: Historic resource (unspecified) of 720,000.00 tonne - Uranium @ 3.15 % 1997-12-31 Estimated proved reserves - Sue deposits: DEPOSIT THOUSAND GRADE MILLION TONNES ORE U3O8 LBS U3O8 ________________________________________ A 55.0 1.49 1.8 B 90.1 0.86 1.7 C 249.9 5.30 29.2 ________________________________________ Summary: Sue A: Historic proven reserve of 55,000.00 tonne - Uranium: 1,800,000.00 lb @ 1.49 % Sue C: Historic proven reserve of 249,900.00 tonne - Uranium: 29,200,000.00 lb @ 5.3 % Sue B: Historic proven reserve of 90,100.00 tonne - Uranium: 1,700,000.00 lb @ 0.86 % 1990-11-01 Deposit reserves: ZONE PROVEN PROBABLE AVERAGE RESERVES RESERVES GRADE KG U3O8 KG U3O8 % U3O8 _____________________________________ A 0.8 million 0.8 million 1.5 B 0.8 million 0.8 million 0.8 C 11.0 million 24.0 million 5.7 _____________________________________ Summary: Zone B: Historic probable reserve - Uranium: 800,000.00 kg @ 0.8 % Zone B: Historic proven reserve - Uranium: 800,000.00 kg @ 0.8 % Zone A: Historic probable reserve - Uranium: 800,000.00 kg @ 1.5 % Zone A: Historic proven reserve - Uranium: 800,000.00 kg @ 1.5 % Zone C: Historic probable reserve - Uranium: 24,000,000.00 kg @ 5.7 % Zone C: Historic proven reserve - Uranium: 11,000,000.00 kg @ 5.7 %