(Q59053206)

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

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title

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

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main subject

banded iron formation

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M. E. Barley

1

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A. L. Pickard

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2

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P. J. Sylvester

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3

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language of work or name

English

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publication date

January 1997

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published in

Nature

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volume

385

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issue

6611

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page(s)

55-58

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exact match

https://scigraph.springernature.com/pub.10.1038/385055a0

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cites work

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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https://api.crossref.org/works/10.1038%2F385055A0

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7 January 2021

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Paleoecological Significance of the Banded Iron-Formation

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https://api.crossref.org/works/10.1038%2F385055A0

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7 January 2021

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Theoretical constraints on oxygen and carbon dioxide concentrations in the Precambrian atmosphere

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https://api.crossref.org/works/10.1038%2F385055A0

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7 January 2021

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Tectonic control of the crustal organic carbon reservoir during the Precambrian

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Tectonic evolution of the Late Archaean to Early Proterozoic Mount Bruce Megasequence Set, western Australia

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The role of mantle plumes in continental breakup: case histories from Gondwanaland

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https://api.crossref.org/works/10.1038%2F385055A0

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7 January 2021

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U-Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass-resolution ion microprobe

1 reference

stated in

Crossref

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https://api.crossref.org/works/10.1038%2F385055A0

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7 January 2021

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Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides

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reference URL

https://api.crossref.org/works/10.1038%2F385055A0

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7 January 2021

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Himalayan ironstones, "superplumes," and the breakup of Gondwana

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https://api.crossref.org/works/10.1038%2F385055A0

retrieved

7 January 2021

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1053127917

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(Q59053206)

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

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