(Q70523479)

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The formation of Palæoproterozoic banded iron formations and their associated Fe and Mn deposits, with reference to the Griqualand West deposits, South Africa

scientific article published in January 2000

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The formation of Palæoproterozoic banded iron formations and their associated Fe and Mn deposits, with reference to the Griqualand West deposits, South Africa (English)

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banded iron formation

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Dietrich D. Klemm

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publication date

January 2000

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Journal of African Earth Sciences

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30

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1

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1-24

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Microfossils from the Neoarchean Campbell Group, Griqualand West Sequence of the Transvaal Supergroup, and their paleoenvironmental and evolutionary implications

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Emplacement of a large igneous province as a possible cause of banded iron formation 2.45 billion years ago

1 reference

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U-Pb zircon age for a tuff in the Campbell Group, Griqualand West Sequence, South Africa: Implications for Early Proterozoic rock accumulation rates

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Rare earth element systematics of the chemically precipitated component in early precambrian iron formations and the evolution of the terrestrial atmosphere-hydrosphere-lithosphere system

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The chemical evolution of Precambrian seawater: Evidence from REEs in banded iron formations

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Megascopic eukaryotic algae from the 2.1-billion-year-old negaunee iron-formation, Michigan

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Natural Occurrence of Amino-Acids in Dolomitic Limestones Containing Algal Growths

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Earth's early atmosphere

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Chronological correlations between the Pilbara and Kaapvaal cratons

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Were kinetics of Archean calcium carbonate precipitation related to oxygen concentration?

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Geochemistry and sedimentology of a facies transition — from microbanded to granular iron-formation — in the early Proterozoic Transvaal Supergroup, South Africa

1 reference

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Geochemistry and sedimentology of a facies transition from limestone to iron-formation deposition in the early Proterozoic Transvaal Supergroup, South Africa

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Identifiers

10.1016/S0899-5362(00)00005-1

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2000JAfES..30....1K

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