The boulders were processed for heavy-mineral concentrates from which grains of Mg-ilmenite, chromite, garnet, clinopyroxene and olivine were picked, counted and analyzed by electron microprobe. Based on relative abundances and composition of these mineral phases, the boulders could be assigned to six mineralogically different groups, five for the Kirkland Lake area and one for the Lake Timiskaming area. Their indicator mineral composition and abundances are compared to existing data for known kimberlites in both the Kirkland Lake and Lake Timiskaming areas. Six boulders from the Munro Esker form a compositionally homogeneous group I in which the Mg-ilmenite population is very similar to that of the A1 kimberlite, located 7—12 km N up-ice , directly adjacent to the Munro esker in the Kirkland Lake kimberlite field. U—Pb perovskite ages of three of the group I boulders overlap with that of the A1 kimberlite. Three other boulders recovered from the same localities in the Munro Esker also show some broad similarities in Mg-ilmenite composition and age to the A1 kimberlite. However, they are sufficiently different in mineral abundances and composition from each other and from the A1 kimberlite to assign them to different groups II—IV. Their sources could be different phases of the same kimberlite or—more likely—three different, hitherto unknown kimberlites up-ice of the sample localities along the Munro Esker in the Kirkland Lake kimberlite field. A single boulder from the Misema River esker, Kirkland Lake, has mineral compositions that do not match any of the known kimberlites from the Kirkland Lake field. This suggests another unknown kimberlite exists in the area up-ice of the Larder Lake pit along the Misema River esker.
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Heaman Abstract Sixteen kimberlite boulders were collected from three sites on the Munro and Misema River Eskers in the Kirkland Lake kimberlite field and one site on the Sharp Lake esker in the Lake Timiskaming kimberlite field. The boulders were processed for heavy-mineral concentrates from which grains of Mg-ilmenite, chromite, garnet, clinopyroxene and olivine were picked, counted and analyzed by electron microprobe.
Based on relative abundances and composition of these mineral phases, the boulders could be assigned to six mineralogically different groups, five for the Kirkland Lake area and one for the Lake Timiskaming area. Their indicator mineral composition and abundances are compared to existing data for known kimberlites in both the Kirkland Lake and Lake Timiskaming areas. Six boulders from the Munro Esker form a compositionally homogeneous group I in which the Mg-ilmenite population is very similar to that of the A1 kimberlite, located km N up-ice , directly adjacent to the Munro esker in the Kirkland Lake kimberlite field.
U-Pb perovskite ages of three of the group I boulders overlap with that of the A1 kimberlite. Three other boulders recovered from the same localities in the Munro Esker also show some broad similarities in Mg-ilmenite composition and age to the A1 kimberlite. However, they are sufficiently different in mineral abundances and composition from each other and from the A1 kimberlite to assign them to different groups II-IV.
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The Sr isotope data record geographic variations which, from east to west on the KC fault is 0. Metasomatised fault zones are systematically more radiogenic than contiguous host lithologies, and imply a source reservoir 0. Carbon isotope compositions of ferroan dolomites in faults are tightly clustered along local fault sectors, but also display a marked provinciality: This is a preview of subscription content, log in to check access Preview Unable to display preview. Can J Earth Sci Am J Sci
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During Q1 , the mill processed 91, tonnes at an average grade of Mine production during Q1 totaled 89, tonnes at an average run of mine grade of The main decline development is ongoing, although the focus in Q1 was development of the ‘ Level east and west from the main ramp. The Decline towards the Lower D North LDN zone is now below the ‘ Level and infrastructure is currently being developed in order to commence production in Holt During Q1 , the Holt Mine delivered , tonnes of ore at an average grade of 4.
After mill recoveries of
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Hamden, a spry year-old, remembers his first big break in at the Lake Shore mine, then one of the deepest gold mines in the world, producing 8. We had 17 different hotels in the Kirkland Lake area alone. Mining jobs vanished, shops and hotels closed and housing prices crumbled, prompting fears that Kirkland Lake – an eight-hour drive north of Toronto – could turn into a ghost town. Companies are reopening mines that were mothballed for decades, offering many new jobs and sparking an economic recovery in the area.
And there are definitely improvements in technology. The best part is All kinds of things can be hiding right under your nose. The town grew haphazardly around the mines and its streets are a maze that appear to be ripped out of a jig-saw puzzle. The north end of the town is dominated by a large dry hollow, which was once the lake that gave the town its name. Filled in with mine tailings years ago, the lake has since been dredged, but it is kept mostly dry now to avoid flooding the mine workings that extend deep below the surface.
Although many houses in the area date back to the s and s, housing prices have soared as the area booms. The housing market is so tight that St Andrew Goldfields took a drastic step and bought two motels in the nearby town of Matheson to use as worker accommodation. While the boom helps eateries and hotels, not all ventures are enjoying similar success. Many miners are transient, with families in nearby hubs like Rouyn-Noranda, Timmins, North Bay and Sudbury, so much of the money earned in and around Kirkland Lake, ends up outside the area.
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Engineer charged with negligence in Elliot Lake mall roof collapse In a scathing indictment of those who allowed the Algo Centre Mall to rust to the point of collapse, Commissioner Paul Belanger pulls few punches in holding those responsible to account. Nineteen others were injured. Putting parking on the roof was a bad idea. The defective roof design — using an untested combination of materials — made matters much worse. Ironically, the mall seldom lacked for professional oversight from architects and engineers, with some 30 visits, inspections and reports over its year life.
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He was also predeceased by his in-laws Charles Budd and Sally Budd Barry was a gentle, caring man that was one of a kind, irreplaceable in many ways. He will be sadly missed by all that who knew him. He was an avid curler in his younger years, a place were he met the love of his life Donna. He enjoyed many gatherings and time spent creating memories with his family at Keefer Lake.
Barry was a true sports fan, hockey, football you name it, he followed it. Prior to Donna’s illness they loved to travel, leaving the kids to wonder where they were off to next. Some highlights of his travels were a family trip to Disney World and attending the th Anniversary Grey Cup. His love for his family was second to none, unconditionally. He was the foundation of our family unit always keeping us together. He was a true gentleman. Barry was known by many as the Manager of Purchasing for the school board in Schumacher for many years, creating a lot of friendships along the way.