Details


SMDI #
1425a
Current Showing Name
Cinch/Cenex Mine; Cinch Lake Mine; New Joburke Mine; Cenex Mine [20 Ore Zone, Breccia Zone, Shear Zone, River or Enex or Main Zone]; B Uranium Showing
Historical Showing Names
Cinch/Cenex Mine; Cinch Lake Mine; New Joburke Mine; Cenex Mine [20 Ore Zone, Breccia Zone, Shear Zone, River or Enex or Main Zone]; B Uranium Showing
Company Name
Project Name
UTM Easting (NAD83 Z13)
292658.0100
UTM Northing (NAD83 Z13)
6606248.3500
NTS Sheet
074N10
TRM (Township-Range-Meridian)
121-16-3
Primary Commodities
Uranium
Associated Commodities
Copper, Iron, Titanium
Discovery Type
Status
Deposit: Post-Production
Geological Details
The Cinch Lake Mine is located 700 m (0.44 mile) west of and south of Cinch Lake and 2.5 km (1.6 miles) south of Uranium City. The area underlying the mine site contains mylonitized and brecciated quartz-rich gneiss which contains minor amounts of granite, graphite, amphibolite, and hornblende-feldspar gneiss and schist. The mine area is a "wedge" of rock located between the Crackingstone River Fault and the Main Fault which is locally known as the Tazin Formation "Cayzor Unit". K. Ashton et al re-mapped the surface rocks at the deposit as unit Gl or pink to red, fine- to medium-grained, cataclastic leucogranite. In the Cinch Mine, the highest grade ore is associated with a 2 to 10 ft (0.6 to 3.1 m) wide band of mylonite which has been named the Main Ore Fault. This northeast-trending fault, which parallels the Black Bay Fault, is located approximately 900 ft (274.3 m) southeast of Guts Lake. On the second level of the mine (-500 feet) the ore is limited to a shoot extending along the Main Ore Fault from 45 to 365 feet (13.7 to 111.3 m) northeast of the junction with the northeast-trending Crackingstone River Fault. From this level it extends upwards for 135 feet (41.1 m) and downwards for an undetermined distance. As the Crackingstone and Main Ore Faults converge at the 5th mine level (-875 ft), there is little ore found below this level. Pitchblende, usually accompanied by calcite and chlorite, is disseminated through the highly chloritized and hematized red mylonite host (Main Ore Fault) in fine feathery grains and rims to breccia fragments. Hematite is finely disseminated throughout the 2 to 10 ft (0.6 to 3.1 m) thick ore zone and is densely concentrated near pitchblende. Pyrite, chalcopyrite, specular and earthy hematite, and rutile occur locally. Ore also occurs in steeply dipping northwest-striking tension faults connecting the Main Ore Fault and Crackingstone River Fault. Breccia and fracture zones along the subsidiary faults are cemented or veined with calcite, hematite, and pitchblende. Individual shoots of ore range from 1 to 7 feet (0.3 to 2.1 m) in width and from 50 to 250 feet (15.2 to 76.2 m) in length. The River Zone is on the hanging-wall side of the Crackingstone Fault, about 1,200 feet (365.8 m) west of the shaft. The major portion of this deposit is not connected to the mine workings. Pitchblende-bearing veins occur in both northeast- and northwest-trending fractures and one small ore shoot (made up of two main veins) was outlined. The area underlying the River Zone is the same geologically as that underlying the Cinch Lake Mine. The 'B' Showing, located between the mine and the River Zone, consists of short narrow chlorite fractures trending northeast and northwest which contain hematite and pitchblende. The fracture zone is intermittently radioactive for 600 feet (965.6 m). The area is underlain by a northeast-striking contact zone between chloritic gneiss and mylonitized quartz-feldspar gneiss. The best assay is a trench sample that gave 1.36% U3O8 across 4.8 feet. The Lake Cinch Extension Drilling zone area (see SMDI 0425b) is underlain by a northeast-trending sequence of mylonitized and brecciated paragneiss enclosing a strike fault, believed to be the offset extension of the Main Ore Fault the Cinch Lake Mine. The Cinch extension Zone, which is located approximately 600 feet west of the River Zone, gave a best assay of 0.3% U3O8 across 5 feet. Mineralization is spotty and has poor continuity. The ore-bearing structures of the Cenex Mine consist of a series of sub-zones which were named the Breccia Zone, the Shear Zone, and the above-described River Zone (also called the main orebody). The Breccia Zone consists of a 70°S-plunging curved tabular unit which is 1 to 5 m (3.3 to 16.4 ft) thick. The ore is hosted within a series of brecciated mylonitic and ultramylonitic, leucocratic quartzofeldspathic gneisses (Unit 3) and a mylonite chlorite-sericite-quartz-graphite schist (Unit 4). The Breccia Zone pinches out above mine level 2. The Shear Zone, which is hosted within the same rock types as the Breccia Zone, strikes northeast and dips 70°SE. The Shear Zone consists of an undulating series of graphite-covered shears which are spaced 3 to 7 cm (1.2 to 2.8 inches) apart. The 20 Ore Zone consists of mineralized areas around the 20 Zone Fault - a splay off the River Zone fault. The wedge-shaped zone, which is connected to thee River Zone at its southeast end, consists of numerous mineralized carbonate veins and mineralized adjacent wallrock in the foot wall of the 20 Zone Fault. The ore grade of this zone varies from 0.1% to 0.5% U3O8. The ore which comprises this zone is of three types: (1) The Shear Zone style of ore, which is regarded as the oldest ore, is restricted to the Shear Zone and small portions of the River Zone and the 20 Zone. The ore consists of fine disseminations of uraniferous titanite±fine pitchblende grains± yellow secondary uranium minerals along foliation planes. (2) The second generation ore, called breccia style ore, is found in the River Zone and locally in the 20 Zone. This style of mineralization, which accounts for 75% of the production, consists of pitchblende grains, uraniferous titanite veinlets±secondary uranium minerals which are present throughout the brick-red mylonite and ultramylonite fragments in the breccia and as a finely disseminated pitchbelnde-calcite-hematite in the breccia groundmass. (3) The youngest generation of ore, or vein style ore is found in the 20 Zone, the uppermost level of the River Zone, and in portions of the 16 Vein. It consists of disseminations of uranium minerals plus local colloform pitchblende which is hosted in carbonate veins which infill shears in the wallrock.
Geological Domain
Zemlak
Host Rocks
Host Minerals
Hematite, Rutile
Indicators
Exploration History
7/29/1988 The Cinch Lake Mine began as a series of 4 showings occurring along a straight line between Cinch Lake and Guts Lake. The showings are spaced over equal intervals along a distance of 1,800 feet (548.6 m). The Cinch Lake Mine and 'River Zone' will be described first. The property covering the mine was first staked in 1948 for C. Swenson, who sold it in 1950 to Cinch Lake Uranium Mines Ltd. From 1951 to 1953, the property was examined in detail by the Mining Corporation of Canada Ltd., and 65 diamond drill holes for a total footage of 13,752 feet were drilled over a few small highgrade showings outlined just south of the Crackingstone River. In 1955, Cinch Lake Mines Ltd. discovered a minor pitchblende occurrence, named the B Zone, between the Cinch Mine and the River Zone. The showing was trenched and drilled between 1955 and 1956. In October 1954, Cinch Lake Uranium Mines Ltd., was re-organized to Lake Cinch Mines Ltd. and controlled by Violamac Mines Ltd., and by late 1955 an additional 22,500 feet of diamond drilling in 65 holes were done by Lake Cinch on the main radioactive zones. Results warranted the sinking of a vertical production shaft. The shaft was started in late 1955 and sunk to a depth of 548 feet (167 m). Two levels were established. Shipments to the Lorado Mill commenced in May 1957. In 1958 the shaft was deepened to 867 feet (264.3 m) and again in 1959 to 1,096 feet (334.1 m). By then four new levels had been established and lateral development on all six levels had been completed. On 26 March 1960, the production stopped and in May 1960 the mine was closed. Proven and probable reserves for the deposit were released at the time of closure. The ground covering the River Zone was restaked in 1965 and acquired by Enex Mines in 1966 when additional diamond drilling was done. This resulted in outlining two main veins in this zone, which is situated 1,200 feet (365.8 m) due west of the Cinch Lake Mine site. The major portion of this deposit is not connected to the mine workings. In 1969, the Enex group merged with Lake Cinch Mines under the name Gardex Mines for the purpose of developing the two properties jointly and using the Lake Cinch shaft. In July 1974, Eldorado purchased the property from Gardex and carried out an exploratory drill program over the next 15 months. Eldorado optioned these properties to New Joburke, who took the option in 1976, and through its wholly owned subsidiary, Mining Corporation of Canada (1964) Ltd., would be the mine operator and would play a key role in financing a $6 to $7 million project. It was proposed to explore and develop the River Zone, or Enex Zone, by an adit and decline to a vertical depth of 300 feet (91.4 m) below surface by trackless mining methods and equipment. The ore was to be treated and concentrated by Eldorado in its Beaverlodge Mill. The ore reserves for the deposit and for the Lethbridge Zone (or the combined 03 and 04 Zones): located just to the west of the River Zone were released. In August of 1977, New Joburke changed its name to Cenex Ltd. At this time, the deposit proven, probable, and possible ore reserves Enex property were re-calculated using data collected from the 1975 to 1976 drill program and and the amount of ore remaining in the Cinch Lake Mine was re-calculated. The River Zone was only examined underground on the first level of the mine during the operations of the Cinch Lake Mine. Because such good tonnages were outlined between 1975 to 1976, Eldorado over this zone and the adjacent Cinch Lake property, an adit, as mentioned above, was to be collared and mining of the ore was to commence by 1 May 1977. New Joburke through its subsidiary Mining Corporation of Canada (1964) Ltd. was to be the operator of this mining exploration, development and production work. In 1978, Cenex Ltd purchased the properties. A 2,500 m (8,202.1 ft) spiral decline was driven to 375 ft (114.3 m) vertical depth on the 03 Zone (1,500 ft (457.2 m) west of the shaft). Between 1978 and 1979, an ore sorter was installed and ore was trucked to the Eldorado Mill. In February 1979, a fire destroyed the powerhouse. Working capital became short and Cenex was placed in receivership. Mining ceased in October of 1979. In 1980, A. Frame Contracting purchased the minesite and stockpiled ore.
Production History
Production Period: 1978-01-01 to 1979-10-31 Cenex Mine In 1978, Cenex Ltd. drove a 2,500 m (8282 ft) spiral decline on the 03 Zone and installed a ore sorter. This is referred to as the New Joburke or Cenex Mine. Between 1978 and 1979, approximately 2,000 tons of ore a week were shipped to the Eldorado Mill. Work ceased in 1979 as the powerhouse burned down. The mine closed in October 1979. Between 1978 and 1979, the Cenex Mine produced 712,375 lbs U3O8 and the Lethbridge Zone (combined Zones 3 and 4) produced 855,429 lbs U3O8 (482,000 lbs concentrates). In 1980, A. Frame purchased the minesite and the stockpiled ore. Summary: - Uranium: 712,375.00 lb - Uranium: 855,429.00 lb Production Period: 1957-05-01 to 1960-05-01 125,205.00 tons The mine workings consist of 3 shafts (Cinch Lake), a decline (Cenex). Shaft 2 is located 10 m (32.8 ft) west of shaft 1, shaft 3 is located 500 m (1640.4 ft) west of shaft 2, and the adit is located southwest of shaft 3. Late in 1955, a 548 ft (167 m) shaft was sunk and level development commenced. Shipments from the Cinch Lake Mine to the Lorado Mill commenced in May 1957. In 1958, the shaft was deepened to 867 ft (264.3 m) and in 1959, the shaft was deepened to 1096 ft (334.1 m). Production stopped and the mine closed in May 1960. During this period of mining, 125,205 tons of ore were shipped. This produced 661,257 lbs U3O8. Summary: - Uranium: 661,257.00 lb
Reserves and/or Resources
1979-09-06 The Lethbridge Zone contains 15,000 tons grading 8.4 lb/ton U3O8 in the 03 Zone below the 500 foot level. Summary: Lethbridge Zone: Historic reserve (unspecified) of 15,000.00 ton - Uranium: 15,000.00 ton @ 8.4 lb/ton 1977-08-01 300,000 tons of ore which contain about 1,200,000 lbs U3O8 (included ore left in the Cinch Mine), of which 600,000 lbs on the Enex property are classed "fast pay". This is calculated to 300 feet on the Enex property and 1,000 feet at Cinch. Summary: Historic reserve (unspecified) of 300,000.00 ton - Uranium: 1,200,000.00 lb 1976-01-01 300,000 tons of ore grading 0.2% U3O8 (after 39% dilution) to the 1,000 foot level in the Cinch Mine and to the 300 foot level on the River Zone. Summary: River Zone: Historic reserve (unspecified) of 300,000.00 ton - Uranium: 300,000.00 ton @ 0.2 % 1960-05-01 (at mine closure) Proven reserves: 32,473 tons with an average grade of 0.196% U3O8. Probable reserves: 150,000 tons with an average grade of 0.23% U3O8. Summary: Historic proven reserve of 32,473.00 ton - Uranium: 32,473.00 ton @ 0.196 % Historic probable reserve of 150,000.00 ton - Uranium: 150,000.00 ton @ 0.23 %