BANDED IRON FORMATIONS AND PALAEOENVIRONMENT: A PROBLEM IN PETROGENESIS

dc.contributor.author	Page D.
dc.date.accessioned	2021-03-19T05:26:30Z
dc.date.available	2021-03-19T05:26:30Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=1229589
dc.identifier.citation	Geology Today, 2001, 17, 4, 140-143
dc.identifier.issn	0266-6979
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26939
dc.description.abstract	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?
dc.subject	Precambrian
dc.title	BANDED IRON FORMATIONS AND PALAEOENVIRONMENT: A PROBLEM IN PETROGENESIS
dc.type	Статья
dc.subject.age	Докембрий	ru
dc.subject.age	Precambrian	en

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