That ground, now known as the Mitchi project, belongs to Kintavar Exploration (TSXV: KTR), a junior explorer whose work over the last year has served some pleasant surprises.
Kintavar says it has found a near-surface and folded sedimentary system in the eastern portion of the property that can be traced for kilometre after kilometre, and displays characteristics that suggest the presence of a sediment-hosted stratiform copper type deposit.
“Instead of following the skarn model, we said we’ll trench the whole thing and open it up and see what’s there,” says Kintavar’s president and CEO, Kiril Mugerman. “Once we trenched it, we realized we weren’t dealing with a skarn but with a sedimentary system like those in the DRC.”
But unlike the deep sediment-hosted stratiform copper deposits in the DRC, Mugerman says, copper mineralization at Mitchi is near-surface and shallow dipping, which means, in theory at least, that it could be mined as an open-pit one day.
“Stratiform copper deposits are usually deep underground — none of them are exposed in an open-pit,” he says. “But ours is flat and shallow, it’s almost like a coal seam, long and continuous.”
In Mitchi’s case, it was high-grade metamorphism and folding of the Grenville rocks that brought the mineralization to surface. (The property is in the north-western portion of the Central Metasedimentary Belt of the Grenville geological province.)
“Where we are, the unit is fairly thick by itself and folded, and because of the folding you have structural enrichment,” Mugerman explains. “Think of it as a piece of paper that is folded several times and when you cut it you intercept the paper several times.”
Initial surface work found copper and silver mineralization for over 20 km along three corridors — Watson, Sherlock, and Nasigon — with grades ranging from 0.5% copper to 1% copper. Each corridor is roughly 10-plus kilometres of favourable sedimentary units that are roughly 5-7 km apart.
“The volume potential is huge,” Mugerman says in a telephone interview from Montreal.
Last year, channel samples from Watson yielded 13.6 metres grading 0.54% copper, 5.29 grams silver per tonne and 0.57% manganese, and 3 metres of 0.61% copper, 6.02 grams silver and 0.53% manganese. At Sherlock, a channel sample returned 21.4 metres of 0.49% copper and 5.5 grams silver, and at Nasigon, 10 metres of 1.1% copper and 3.4 grams silver.
This year, Kintavar is undertaking a 10,000-metre drill program, and early results seem encouraging. Drilling in the Sherlock corridor has intersected over 100 metres of copper mineralization in four of twelve drill holes.
Highlights include a 120-metre intercept grading 0.34% copper and 2.90 grams silver per tonne from 9 metres downhole (including 30 metres of 0.61% copper and 3.76 grams silver from 99 metres downhole) in hole MS-17-03; and 0.31% copper and 2.85 grams silver over 131 metres from 44 metres downhole in hole MS-17-04. Another hole, MS-17-08, cut 206.3 metres of 0.18% copper and 1.65 grams silver from 3.9 metres downhole, including 21.9 metres of 0.52% copper and 5.62 gram silver from 42.6 metres downhole.
After those results, Mugerman says, the company was approached by a number of majors, and Kintavar met many of them at the Prospectors and Developers Association of Canada convention in March.
The company recently raised $10 million — half of it from Quebec institutions. Caisse de Depot took the largest position and became an insider with a 16% stake for $3.8 million.
The junior explorer is tightly held with less than 100 million common shares or around 90 million shares fully diluted.
Geomega Resources (TSXV: GMA), which spun off Kintavar a year and a half ago, and is also run by Mugerman, owns 25%. Quebec funds own another 25%, and local investors — many of them people in the region’s forestry industry who live close to the project — own another 25%.
The 28,000-hectare project, the southern portion of which is about 300 km north of Montreal, is accessible by a network of logging and gravel roads with a hydro-electric power substation 14 km to the east. Mitchi is also just 50 km south of Parent, which has a railroad link to Rouyn-Noranda. The project has so much infrastructure, Mugerman likes to joke, that it even has a postal code.
Mugerman notes that there are under ten known sediment-hosted stratiform copper deposits in North America, among them White Pine and Copperwood in Michigan, Spar Lake in Montana, Creta in Oklahoma and Redstone in the Northwest Territories.
Traditionally, the Grenville province — which stretches from Labrador to Mexico — has not been considered a good place to look for them, he says.
“You need a sedimentary basin, but not every one of them will have the right conditions,” he explains. “Underneath the sedimentary basin you need the right rocks that have just enough copper to be leached out, then you need the perfect conditions to precipitate it.”
“They are not that rare — you find them — but the problem is they’re always too deep,” he says. As a consequence, they are not always economically significant deposits.
“The monsters in the DRC are unique because they are 5-metre-plus thicknesses at depths of between 400 and 600 metres and grades of 3-10% copper, just unbelievable. Everywhere else they are not as thick or as high-grade.”
It’s still early days, but Mugerman wonders whether Mitchi could turn out to be a monster, too.
In the meantime, the company is beginning to get a better sense of how to spot them in a Grenville setting and is investigating additional targets.
“We think there could be more.”