$GEMSF Infinity Stone Hits Massive Graphite on Roc
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Posted On: 11/22/2022 9:41:01 AM
$GEMSF Infinity Stone Hits Massive Graphite on Rockstone Step-Out Hole
https://www.newsfilecorp.com/release/145256
Highlights
Infinity Stone has completed drilling of the RS-22-03 step out drillhole, intersecting four separate intervals comprising a total of 45.5 metres of semi-massive to massive graphite.
The Company has expanded the drill program with an additional drill hole. RS-22-04 is a northern step-out of RS-22-03.
Vancouver, British Columbia--(Newsfile Corp. - November 22, 2022) - Infinity Stone Ventures Corp. (CSE: GEMS) (OTCQB: GEMSF) (FSE: B2I) (the "Company" or "Infinity Stone"
, is pleased to provide an update on its Fall drill program (the "Fall Drill Program" on the Rockstone Graphite project located near Thunder Bay, Ontario ("Rockstone" or the "Rockstone Graphite Project" .
The Company has completed the drilling of RS-22-03, a step-out of the historic GC-12-01 and RS-22-01 hole. Within RS-22-03, four graphitic zones, consisting of semi-massive to massive graphite, were encountered in the following intervals (Table 1).
https://www.newsfilecorp.com/release/145256
Highlights
Infinity Stone has completed drilling of the RS-22-03 step out drillhole, intersecting four separate intervals comprising a total of 45.5 metres of semi-massive to massive graphite.
The Company has expanded the drill program with an additional drill hole. RS-22-04 is a northern step-out of RS-22-03.
Vancouver, British Columbia--(Newsfile Corp. - November 22, 2022) - Infinity Stone Ventures Corp. (CSE: GEMS) (OTCQB: GEMSF) (FSE: B2I) (the "Company" or "Infinity Stone"
, is pleased to provide an update on its Fall drill program (the "Fall Drill Program" on the Rockstone Graphite project located near Thunder Bay, Ontario ("Rockstone" or the "Rockstone Graphite Project" . The Company has completed the drilling of RS-22-03, a step-out of the historic GC-12-01 and RS-22-01 hole. Within RS-22-03, four graphitic zones, consisting of semi-massive to massive graphite, were encountered in the following intervals (Table 1).
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