early stage exploration project 90 km south of voisey's bay nickel-copper-cobalt mine
early stage exploration project 90 km south of voisey's bay nickel-copper-cobalt mine
Targeting Voisey's Bay
Eastern Deeps
Style Deposit
90 km SOUTH OF VOISEY'S BAY Ni-Cu-Co MINE
PROXIMAL TO CHURCHILL-NAIN TECTONIC CONTACT
highlights |
Along Churchill-Nain Suture Zone, Host to Massive World-Class Deposits
Untested EM Conductors in Gabbro Dykes Cut by Disseminated Ni-Cu-Co Mineralization
Historical Stream Sediment Samples Up to 31 and 34 ppm Ni (Wares, 1997); Yet to be Explored
Geochemical Anomalies Proximal to Untested EM Conductors
Anomalous Nickel Values Coincident With Increased Copper Values
Conductors in Anorthosite May Result From Deep Mineralization As Seen In the Eastern
Deeps Deposit
deposit model |
overview |
The Hopedale Nickel (±Copper-Cobalt) Project is located approximately 90 kilometres west of the town of Hopedale in Labrador, Canada and 90 kilometres south of Voisey’s Bay Nickel-Copper-Cobalt Mine. The Project consists of 106 claims totaling 26.5 square kilometres and is 100% owned by Anteros Metals Inc. The geological setting bears similarities to the rocks and structures that host the Voisey’s Bay Eastern Deeps Deposit, expected to produce 500,000 tonnes of Nickel by 2034.
Magmatic Nickel Sulphide Deposit
geology
and target
Regional Geology
Churchill-Nain Suture Zone
The Project lies within the Nain Province near the suture of the Churchill and Nain Provinces formed during the Torngat Orogen. Archean gneisses of the Nain Province were intruded by a series of igneous rocks during periods of intracontinental rifting resulting in the Nain Plutonic Suite and the Harp Lake Intrusive Complex, anorthositic to gabbroic rocks highly-prospective for nickel mineralization. Middle Proterozoic diabase dikes trend northeast and cross-cut all units.
The Nain Plutonic Suite is host to the world-class Voisey’s Bay Nickel-Copper-Cobalt sulphide deposit.
Property Geology
Harp Lake Intrusive Complex
Southwestern portions of the property are underlain by gabbroic and anorthositic rocks of the Harp Lake Intrusive Complex, highly prospective for sulphide related mineralization. Northwestern portions of the property overlie granitic to monzonitic rocks. All units are cut by harp dikes, a series of northeast-trending gabbro dikes also associated with nickel-copper-cobalt sulphide mineralization.
Target Model
Magmatic Nickel Sulphide
Untested electromagnetic conductors within anorthositic rocks on the Property may be resultant from deeper, disseminated mineralization, as known to occur at the Eastern Deeps Deposit of the Voisey’s Bay Ni-Cu-Co Mine. Sediment surveying on the Property has resulted in anomalous nickel values, coincident with elevated copper.