Genetic modelling for banded iron-formation of the Hamersley Group, Pilbara Craton, Western Australia

Morris, R.C.

doi:10.1016/0301-9268(93)90051-3

Cited by 306Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisGeological and Geochemical Analysis

Genetic modelling for banded iron-formation of the Hamersley Group, Pilbara Craton, Western Australia

Morris, R.C.·1993·Precambrian Research

DOI 10.1016/0301-9268(93)90051-3

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Traditionally, iron oxides in iron formations are interpreted to have formed from an initial Fe(III)-oxyhydroxide phase, such as ferrihydrite, which precipitated in the photic zone from seawater via oxidation of dissolved Fe(II) at concentrations that may have ranged from 0.03 to 0.5 mM.
“Traditionally, iron oxides in IF are interpreted to have formed from an initial Fe(III)-oxyhydroxide phase, e.g., ferrihydrite, Fe(OH)3, which precipitated in the photic zone from seawater via the oxidation of dissolved ferrous iron, Fe(II), at concentrations that may have ranged from 0.03 to 0.5 mM; Holland, 1973; Morris, 1993).”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Morris, 1993
Morris (1993) proposed that the depositional environment for the Hamersley BIFs included a steady source of silica and iron, and a water depth shallow enough to form the large carbonate platforms.
“Morris (1993) also proposed that the depositional environment for the Hamersley BIFs included a steady source of silica and iron, and a water depth shallow enough to form the large carbonate platforms”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Morris (1993)

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Authors: Morris, R. C.
Affiliations: Commonwealth Scientific and Industrial Research Organisation (AU)
Corresponding author: Morris, R.C.
Venue: Precambrian Research
Publisher: Elsevier BV
Published: 1993-01
Volume: 60
Issue: 1-4
Pages: 243-286
ISSN: 0301-9268 (ISSN-L)
DOI: 10.1016/0301-9268(93)90051-3
OpenAlex: W2034914622
Cited by: 306
References: 91
Citations by year: 2026: 7 · 2025: 6 · 2024: 16 · 2023: 7 · 2022: 11 · 2021: 19 · 2020: 7 · 2019: 16 · 2018: 9 · 2017: 15 · 2016: 15 · 2015: 15 · 2014: 20 · 2013: 20 · 2012: 14
FWCI: 8.05
Type: journal article
Language: en
Open access: closed
Licence: www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Locations: Precambrian Research (publishedVersion)
Topics: Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
Keywords: banded iron formations, Hamersley Group, Pilbara Craton, genetic modeling, chert, varves, ocean upwelling, hotspot volcanism

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Genetic modelling for banded iron-formation of the Hamersley Group, Pilbara Craton, Western Australia

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