
Nevada, USA
Dollar Antimony Project
Favourable geological setting
The prospect is located in the Jett Mining District on the eastern slope of the Toiyabe Range in Nye County, Nevada. The regional geology map indicates the prospect lies at the contact between Tertiary volcanic rocks and unconsolidated Quaternary sediments. The Toiyabe Range is a horst block composed primarily of uplifted Paleozoic sedimentary rocks, including limestone, shale, and siltstone, which are bordered and locally overlain by Tertiary volcanic rocks.
Mineralisation in the district, particularly for antimony, is structurally controlled and hosted in shear zones and faults. A notable occurrence, the Dollar antimony-silver mine, is located at the mouth of Boyd Canyon and features stibnite mineralization along a shear zone at the contact between silicified limestone and shale. This geological setting, involving Paleozoic sediments intruded or overlain by Tertiary volcanics with significant.
High-Grade Historical Assays
The project demonstrates exceptional high-grade potential. Historical assays returned values up to 40.63% Antimony (Sb). Recent USGS sampling has confirmed this potential, with values up to 1.0% Sb from surface sampling. This primary antimony mineralisation is accompanied by valuable silver, lead, and copper credits, enhancing the project’s potential economics.
