Abstract
The Lewis and Clark line is a major lineament trending WNW from central Montana to the Coeur d’Alene mining district of northern Idaho. The Lewis and Clark line consists mainly of Cretaceous to Tertiary thrusts and steep strike-slip and dip-slip faults that are partly superimposed on Middle Proterozoic growth faults related to extension of the western continental margin.
Lode Au-Ag deposits are clustered along the Lewis and Clark line in the Big Belt uplift and comprise the Confederate Gulch, York, and Beaver Creek mining districts. These lodes are mostly epigenetic quartz veins with minor sulfides and are hosted by the Greyson Shale and Newland Limestone (of the Middle Proterozoic Belt Supergroup) and dioritic intrusions. Some mineralization, along bedding planes in the Greyson and Newland formations, may be synsedimentary or syndiagenetic, however. At least 2,581 kg (83,000 oz) Au were produced from lodes and 28,612 kg (920,000 oz) Au from placers locally derived from similar lodes. The average Au:Ag ratio for lodes is ≈ 1.5:1. Most lode Au occurrences along the Lewis and Clark line in the Big Belt uplift are interpreted to be remobilized from Archean basement rocks and deposited in Belt strata, in some cases syngenetically, near basement growth faults active during deposition of the Greyson and Newland formations. Metals were probably transported by aqueous solutions along faults. Au was probably remobilized during widespread but volumetrically minor magmatism in the Late Proterozoic and again in the Cretaceous-Tertiary.
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Woodward, L.A. (1992). Tectonic setting of Au-Ag deposits hosted by Proterozoic strata along the Lewis and Clark line, west-central Montana. In: Bartholomew, M.J., Hyndman, D.W., Mogk, D.W., Mason, R. (eds) Basement Tectonics 8. Proceedings of the International Conferences on Basement Tectonics, vol 2. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1614-5_46
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