Sediment-Hosted Lead-Zinc Deposits in Earth History
Abstract
Sediment-hosted Pb-Zn deposits can be divided into two major subtypes. The first subtype is clastic-dominated lead-zinc (CD Pb-Zn) ores, which are hosted in shale, sandstone, siltstone, or mixed clastic rocks, or occur as carbonate replacement, within a CD sedimentary rock sequence. This subtype includes deposits that have been traditionally referred to as sedimentary exhalative (SEDEX) deposits. The CD Pb-Zn deposits occur in passive margins,...
Paper Details
Title
Sediment-Hosted Lead-Zinc Deposits in Earth History
Published Date
May 1, 2010
Journal
Volume
105
Issue
3
Pages
593 - 625
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Notes
History