Guidelines for finding concretionary Mn-Fe oxides in streams

Journal of Geochemical Exploration
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Abstract

Concretionary Mn-Fe oxides in streams form at interfaces between oxidizing and reducing environments. A reducing environment produces waters high in dissolved Mn and Fe, and an oxidizing environment causes precipitation. Mineralogical, microprobe, and optical studies of concretionary Mn-Fe oxides may further our understanding of the role of Mn-Fe oxides in determining the trace-element geochemistry of stream sediments. 

Publication type Article
Publication Subtype Journal Article
Title Guidelines for finding concretionary Mn-Fe oxides in streams
Series title Journal of Geochemical Exploration
DOI 10.1016/0375-6742(82)90021-8
Volume 17
Issue 1
Year Published 1982
Language English
Publisher Elsevier
Description 3 p.
First page 77
Last page 79
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