.
Enter the email you signed up with and we'll email it to you.
Location: 31 km NW from Carlin, Nevada, United States
1655 Mountain City HighwayElkoNevada, United States89801
Stay on top of the latest gold discoveries. Examine the latest updates on drilling outcomes spanning various commodities.
Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
Shaft depth, mining scale, backfill type and mill throughput data.Full profiles of select mines and projects.
Equipment type, model, size and quantity.Full profiles of select mines and projects.
Camp size, mine location and contacts.Full profiles of select mines and projects.
The Carlin complex is operated as a joint venture (JV) through Nevada Gold Mines which was formed in 2019. Barrick is the JV operator and owns 61.5%, with Newmont owning the remaining 38.5% JV interest.
- subscription is required.
The mineral deposits along the Carlin Trend form a suite of deposits known as Carlin type deposits. Carlin mineral systems are a unique class of epigenetic ore deposits with enigmatic origins. They are unique due to the size and scale of deposits that formed exclusively within NE Nevada during the middle-Eocene period (42-35 Ma), establishing this area as a world-class gold complex. Carlin mineral systems are enigmatic due to their unknown, distal source of gold, as well as deposit characteristics and hydrothermal conditions that culminate to being atypical of most documented mineral systems.Greater Leeville areaDeposits of the Greater Leeville area include Leeville (West Leeville, Turf, Four Corners orebodys), Fallon, Pete Bajo and Rita K. Leeville, Pete Bajo and Rita K contain both Mineral Resources and Mineral Reserves and are currently in operation. Fallon is a Mineral Resource and in development for future mining.Gold mineralization is hosted within Popovich, Rodeo Creek, and Roberts Mountains formations, and associated with a series of variably orientated, discordant undifferentiated dikes that are intensely argillized. Local Phase II thrust-propagated folding structurally controls the highest-grade zones of mineralization within the anticline axial planes, disseminating outwards as stratabound mineralization in favorable sub-units. Subsequent high-angle normal faulting offsets the fold-thrust package and provide feeder-style transport for the hydrothermal fluid event often hosting mineralization associated with dikes.The dimensions and orientations of the modelled mineralized domains for Greater Leeville deposit:Length - 40 – 4,000 mWidth - 30 – 1,900 mTrue Thickness - 5 – 570 mApproximate Strike Direction - NNE.
Success!