One of the highest grade silver project in the world; low cost, high return that is currently in the construction phase with silver commissioning currently underway
The Mangazeisky Silver Project is located in the north-central potion Yakutia Russia, approximately 400 kms north of the capital city of Yakutsk (population 300,000). The economic development of the region around the Mangazeisky Project is low with little or no infrastructure with limited access to the site, including seasonal winter road from December to April and for the remainder of the year the project is accessible primarily by helicopter or fixed wing aircraft from either Yakutsk or Batagai.
The closest village to the Mangazeisky Project is Sebyan-Kuel which is located approximately 50 km south. The village of Sangar, located 240 km southwest of the Project, is the administrative centre for the district of Kobyask Ulas within which lies the Mangazeisky Project.
The Mangazeisky Exploration Licence area is located within the Verkhoyansk mobile belt of northeastern Yakutia. The fold-and-thrust belt forms part of a major orogenic system separating the Siberian North Asian Craton to the west from the immense expanse of accreted terrains, which form most of the Russian Far East.
The belt extends for 2,000 km from the Laptev Sea to the Sea of Okhotsk. The belt is made up of a rock package that is greater than seven km in thickness and is comprised of Late Precambrian to Triassic rocks deposited along the paleo‑Pacific margin of the Siberian Craton. This margin developed as a consequence of rifting events which occurred in the Late Precambrian and again during the Late Devonian to Early Mississippian periods. Deformation events during the Late Jurassic to Early Cretaceous periods were accompanied by low-grade metamorphism in the internal parts of the belt and the emplacement of high-level granitic bodies. During the Tertiary period, strike-slip faulting occurred within the fold-and-thrust belt. The central part of the belt is dominated by a thick monotonous succession of Carboniferous and Permian turbidites which are metamorphosed to lower greenschist grade. Granodiorite and granite plutons intrude the core of the range and are associated with extensive gold-bearing quartz vein systems.
The silver mineralization is epigenetic. To date, Mangazeisky host four types of mineralisation:
For more detailed information regarding the Mangazeisky Silver Project, please refer to Section NI 43-101 for full technical reports.