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Abstract
Sedimentology, Dolomitization, Karstification, and Mineralization of the Leadville Limestone (Mississippian), Central Colorado; Field Trip No. 6, 1985
Pages 137-142
Origin of the Ore Deposits at Gilman and Leadville, Colorado
Tommy B. Thompson,
David W. Beaty,
C. W. Naeser,
C. G. Cunningham
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.
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