Replacement origin for hematite in 2.5 Ga banded iron formation: Evidence for postdepositional oxidation of iron-bearing minerals

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Replacement origin for hematite in 2.5 Ga banded iron formation: Evidence for postdepositional oxidation of iron-bearing minerals

Banded iron formations (BIFs) are central to interpretations about the composition of the Precambrian ocean, atmosphere, and biosphere. Hematite is an important component of many BIFs, and its presence has been used as evidence for the former presence of hydrous ferric oxyhydroxides that formed from...

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Bibliographic Details
Main Authors:	Rasmussen, Birger, Krapež, Bryan, Meier, D.
Format:	Journal Article
Published:	Geological Society of America 2014
Online Access:	http://hdl.handle.net/20.500.11937/7795

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