Banded iron formation to iron ore: a record of the evolution of Earth environments?

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Banded iron formation to iron ore: a record of the evolution of Earth environments?

Banded iron formations (BIF) are the protolith to most of the world’s largest iron ore deposits. Previous hypogene genetic models for Paleoproterozoic “Lake Superior” BIF-hosted deposits invoke upwards, down-temperature flow of basinal brines via complex silica and carbonate precipitation/dissolutio...

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Bibliographic Details
Main Authors:	Evans, Katy, McCuaig, T., Leach, D., Angerer, T., Hagemann, S.
Format:	Journal Article
Published:	Geological Society of America 2013
Subjects:	BIF oxygen atmosphere sulfur evolution
Online Access:	http://hdl.handle.net/20.500.11937/20126

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