Confirmation that two “kimberlitic” discoveries in the Otish Mountains region of north-central Quebec are diamondiferous has focused attention on the area.
Prior to the Christmas holidays,
The second kimberlitic body, dubbed Renard 2, was discovered 1 km south of Renard 1. It yielded 116 micros and 29 macros from 163.1 kg of sample, including five stones registering greater than 0.5 mm in two dimensions. The three largest diamonds measured 1.63 by 1.58 by 0.53 mm, 1.44 by 1.05 by 0.6 mm, and 1.25 by 1.05 by 0.6 mm.
Renard 2 was tested by a vertical hole, which intersected 83 metres of kimberlitic material below 18 metres of overburden. The hole was terminated in the kimberlitic unit at a depth of 101 metres. A second hole, drilled from the same site at an angle of minus 60, intersected just 11 metres of kimberlitic rock, starting at 22 metres down-hole, followed by 70 metres of mainly gneiss interspersed with lesser amounts of kimberlitic material.
Two other magnetic anomalies were tested during the first round of drilling and were explained by the presence of magnetite-rich zones in the gneissic bedrock.
When Ashton made the Otish Mountains discoveries, it was cautious in calling them kimberlite, and instead described them as having characteristics consistent with kimberlite. Subsequent petrographic analysis suggests the diamond-bearing rocks are transitional between kimberlite and melnoite. While similar in appearance to kimberlite, melnoite differs slightly in the chemical composition of the groundmass minerals.
The Renard bodies contain macrocrystic olivine in a groundmass hosting variable amounts of olivine, phlogopite, monticellite, perovskite, apatite and spinel. More importantly, the Renard bodies contain diamonds, along with indicator minerals, including pyrope garnet and chromite. A number of the pyropes have high chromium, low-calcium G10 chemical compositions.
Ashton holds more than 1,760 sq. km of mineral permits in the Otish Mountains area in a 50-50 joint venture with Quebec government-owned
Heavy mineral sampling defined several highly anomalous indicator mineral dispersion fans, with some samples containing as many as 1,000 indicator grains, including a high percentage of G10s.
Ashton flew geophysics over the original central Otish Mountains property in late 2000 and followed-up with ground geophysics over eight targets in March 2001. Last summer was spent further investigating these anomalies; 350 heavy mineral samples were taken.
Further work in 2002 will involve delineation drilling on Renard 2 and the collection of a larger test sample, along with heavy mineral sampling and geophysical surveys to define unexplained mineral trains.
Once Ashton began staking ground in the Otish Mountains area, Majescor responded by acquiring an initial 1,028 sq. km of ground covering a large part of indicator mineral anomaly, down-ice from Ashton.
BHP Diamonds, a wholly owned subsidiary of
Uranerz Explorations & Mining previously discovered a kimberlite body in the Otish Mountains region during the late 1970s while exploring for uranium. The diamondiferous Beaver Lake kimberlite lies 50 km south of Ashton’s property package.
Ditem initially tested the kimberlite with six core holes in 1998 and recovered four macros from selected samples weighing 96.1 kg. However, a follow-up, 7-tonne test sample yielded no diamonds above a 0.8-mm square mesh screen size.
In 2001, Majescor carried out widespread reconnaissance sampling and identified several anomalous indicator mineral zones in the Mistassini area, less than 5 km west of the Beaver Lake kimberlite. Majescor staked 1,216 sq. km in this area, with a further 494 sq. km still pending approval by the Quebec Ministry of Natural Resources. The land package stretches from the northern tip of Lake Mistassini to the western limit of the Otish Mountains.
Based on the till sampling results,
Majescor recently farmed out ground to
Other juniors that have recently picked up ground in the Otish Mountains area include: Dios Exploration, a soon-to-be-listed diamond vehicle of
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