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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Published in | Geology today Vol. 17; no. 4; pp. 140 - 143 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Oxford, UK
Blackwell Science Ltd
01.07.2001
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Online Access | Get full text |
ISSN | 0266-6979 1365-2451 |
DOI | 10.1046/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? |
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Bibliography: | ArticleID:GTO298 istex:BE6E4BACF359424B688BD2031B031CDCB6998B20 ark:/67375/WNG-82GTKG6V-H |
ISSN: | 0266-6979 1365-2451 |
DOI: | 10.1046/j.0266-6979.2001.00298.x |