Banded iron formations and palaeoenvironment: a problem in petrogenesis

The mineralogy, chemistry and stratigraphy of Precambrian banded iron formations have been extensively documented, yet the way such formations are produced remains a subject for debate. Differentiation by varving, microbial precipitation and secondary alteration are all seen as possible mechanisms,...

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Bibliographic Details
Published inGeology today Vol. 17; no. 4; pp. 140 - 143
Main Author Page, David
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Science Ltd 01.07.2001
Online AccessGet full text
ISSN0266-6979
1365-2451
DOI10.1046/j.0266-6979.2001.00298.x

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Summary:The mineralogy, chemistry and stratigraphy of Precambrian banded iron formations have been extensively documented, yet the way such formations are produced remains a subject for debate. Differentiation by varving, microbial precipitation and secondary alteration are all seen as possible mechanisms, but discussion returns to the lack of any modern analogue. Nothing like banded iron forms anywhere in the world today or has done during the entire Phanerozoic. Where do we begin with such enigmatic rocks?
Bibliography:ArticleID:GTO298
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ark:/67375/WNG-82GTKG6V-H
ISSN:0266-6979
1365-2451
DOI:10.1046/j.0266-6979.2001.00298.x