Guidelines for finding concretionary Mn-Fe oxides in streams
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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 |