Palaeoproterozoic magnesite-stromatolite-dolomite-"red beds"assocation, Russian Karelia: palaeoenvironmental constraints on the 2.0 Ga positive carbon isotope shift.

dc.contributor.author	Melezhik, V. A.
dc.contributor.author	Makarikhin, V.V.
dc.contributor.author	Medvedev, P. V.
dc.contributor.author	Fallick, A. E.
dc.date.accessioned	2020-07-15T08:10:08Z
dc.date.available	2020-07-15T08:10:08Z
dc.date.issued	1999
dc.identifier.issn	0800-3416
dc.identifier.uri	https://hdl.handle.net/11250/2665528
dc.description.abstract	Forkortet The ca. 2000 MA Tulomozerskaya Formation, Russian Karelia, representests the most 13C-rich carbonates (up to +18%)which have ever been reported. The implication of this excursion for our understanding of the coeval global geodynamic carbon cycle is not clear, but the interpretation of the maximum....
dc.language.iso	eng
dc.relation.ispartofseries	NGU-Rapport (99.052)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	KARBONATITT
dc.subject	PALEOZOIKUM
dc.subject	DOLOMITT
dc.subject	MAGNESITT
dc.subject	BERGART
dc.title	Palaeoproterozoic magnesite-stromatolite-dolomite-"red beds"assocation, Russian Karelia: palaeoenvironmental constraints on the 2.0 Ga positive carbon isotope shift.
dc.type	Report
dc.description.localcode	46239
dc.source.pagenumber	39

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