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Showing 1 to 4 of 4 for “"GOLD VEINS"”.

  1. History of the fluids associated with the lode-gold deposits, and complex U-PGE-Au vein-type deposits, Goldfields Peninsula, Northern Saskatchewan, Canada

    … granites "intrusive" into the Group (lode-­gold deposits, e.g. Box, Athona, Frontier). The complex Au-PGE-U vein-type deposits, and other minor mineralizations, are genetically associated with later, overlying sedimentary sequences such as the Late Aphebian to Helikian-aged Martin and …

    sask Repository record for History of the fluids associated with the lode-gold deposits, and complex U-PGE-Au vein-type deposits, Goldfields Peninsula, Northern Saskatchewan, Canada (opens in a new tab)

  2. Paragenetic Evolution of the Robertson Deposit: Eocene Intrusion Related Gold Deposit in the Northern Shoshone Range, Nevada

    … known as Tenabo, is an Eocene intrusion-related gold deposit 5 km north of Pipeline, which is a 20 Moz+ Carlin-type gold deposit in the northern Shoshone Range, Nevada. Carlin-type gold deposits have been the focus of many studies as they represent the second largest accumulation of gold in the …

    unr Repository record for Paragenetic Evolution of the Robertson Deposit: Eocene Intrusion Related Gold Deposit in the Northern Shoshone Range, Nevada (opens in a new tab)

  3. A STRUCTURAL HISTORY OF THE GARNET STOCK AND ITS RELATIONSHIP TO DEFORMATION ALONG THE LEWIS AND CLARK LINE, WESTERN MONTANA

    The Lewis and Clark line experienced sinistral transpressive shear during the Late Cretaceous-late Paleocene Laramide orogeny along the boundary between the massive Lewis-Eldorado-Hoadley thrust slab to the NE and the Sapphire and Lombard thrust slabs to the SW. The transpression extruded SE …

    montana-tech Repository record for A STRUCTURAL HISTORY OF THE GARNET STOCK AND ITS RELATIONSHIP TO DEFORMATION ALONG THE LEWIS AND CLARK LINE, WESTERN MONTANA (opens in a new tab)

  4. A STRUCTURAL HISTORY OF THE GARNET STOCK AND ITS RELATIONSHIP TO DEFORMATION ALONG THE LEWIS AND CLARK LINE, WESTERN MONTANA

    The Lewis and Clark line experienced sinistral transpressive shear during the Late Cretaceous-late Paleocene Laramide orogeny along the boundary between the massive Lewis-Eldorado-Hoadley thrust slab to the NE and the Sapphire and Lombard thrust slabs to the SW. The transpression extruded SE …

    montana Repository record for A STRUCTURAL HISTORY OF THE GARNET STOCK AND ITS RELATIONSHIP TO DEFORMATION ALONG THE LEWIS AND CLARK LINE, WESTERN MONTANA (opens in a new tab)