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The AAPG/Datapages Combined Publications Database
Rocky Mountain Section (SEPM)
Abstract
Origin of the Ore Deposits at Gilman and Leadville, Colorado
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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