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- W2272135162 abstract "Abstract The Gilman and Leadville districts in central Colorado contain zinc-lead-silver-gold-copper deposits that have replaced Paleozoic carbonate rocks, principally within the Dyer and Leadville Dolomites. We interprete new stable isotopic fission track data to indicate that the ore was deposited during the mid-Tertiary from acidic hydrothermal solutions at 300–400°C." @default.
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- W2272135162 date "1985-01-01" @default.
- W2272135162 modified "2023-09-23" @default.
- W2272135162 title "Origin of the Ore Deposits at Gilman and Leadville, Colorado" @default.
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