Cited by 254Paleontology and Stratigraphy of FossilsGeological and Geochemical AnalysisGeochemistry and Elemental Analysis

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

Barley, M. E., Pickard, A. L., Sylvester, P. J.·1997·Nature

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Crossref · 10.1038/385055a0

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  • Barley et al. (1997) suggested that deposition of the Hamersley IFs was possibly linked to major submarine magmatic plume activity in the form of a large igneous province (LIP).

    “Barley et al. (1997) suggested that deposition of the Hamersley IFs was possibly linked to major submarine magmatic plume activity in the form of a large igneous province (LIP)”

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References 25 · Cited by 254

Authors
Barley, M. E., Pickard, A. L., & Sylvester, P. J.
Affiliations
  • The University of Western Australia (AU)
  • Australian National University (AU)
Venue
Nature
Published
1997-01
Volume
385
Issue
6611
Pages
55-58
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W2026909703
Cited by
254
References
25
Citations by year
2026: 2 · 2025: 4 · 2024: 6 · 2023: 5 · 2022: 10 · 2021: 10 · 2020: 6 · 2019: 8 · 2018: 8 · 2017: 9 · 2016: 5 · 2015: 15 · 2014: 10 · 2013: 11 · 2012: 12
FWCI
12.50
Type
journal article
Language
en
Open access
closed
Locations
  • Nature (publishedVersion)
  • UWA Profiles and Research Repository (UWA) (submittedVersion)
  • RePEc: Research Papers in Economics (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Keywords
banded iron formations, large igneous provinces, Hamersley Province, Paleoproterozoic, Archean, tectono-magmatic events, diabase, basalt, rhyolite, ocean oxygenation, hydrothermal activity, continental shelf, sedimentation rate, Great Oxidation

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