Cited by 57Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisPaleontology and Stratigraphy of Fossils

Geochemical and mineralogic effects of contact metamorphism on banded iron-formation: an example from the Transvaal Basin, South Africa

Kaufman, Alan J.·1996·Precambrian Research

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Crossref · 10.1016/0301-9268(95)00093-3

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29 of 29 references verified0 citation errors · 0 not checkable

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  • Using C isotope data, CO2 content, and Fe(II) and Fe(III) data from Beukes et al. (1990), Beukes and Klein (1990), and Kaufman (1996), the average initial Corg based on C isotope composition is 1.28 wt.% for oxide-facies IF and 3.24 wt.% for siderite-facies IF.

    “Using C isotope data, CO2 content, and Fe(II) and Fe(III) data from Beukes et al. (1990), Beukes and Klein (1990), and Kaufman (1996), the average initial Corg based on C isotope composition is 1.28 wt.% for oxidefacies IF and 3.24 wt. % for siderite-facies IF.”

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Authors
Kaufman, A. J.
Affiliations
Harvard University (US)
Corresponding author
Kaufman, Alan J.
Venue
Precambrian Research
Publisher
Elsevier BV
Published
1996-07
Volume
79
Issue
1-2
Pages
171-194
ISSN
0301-9268 (ISSN-L)
OpenAlex
W2150753243
Cited by
57
References
35
Citations by year
2026: 1 · 2025: 3 · 2024: 2 · 2023: 4 · 2022: 4 · 2021: 3 · 2020: 1 · 2019: 1 · 2018: 2 · 2017: 4 · 2016: 1 · 2015: 3 · 2014: 1 · 2013: 1 · 2012: 3
FWCI
0.74
Type
journal article
Language
en
Open access
closed
Locations
Precambrian Research (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
banded iron formations, contact metamorphism, diabase sills, Paleoproterozoic, metamorphic aureole, oxygen isotopes, carbon isotopes, total organic carbon, siderite, chert, greenalite, stilpnomelane, early diagenesis, fluid infiltration, oxidation state, mineral alteration, regional metamorphism

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