SHRIMP U–Pb zircon ages of tuffaceous mudrocks in the Brockman Iron Formation of the Hamersley Range, Western Australia
Abstract
Tuffaceous mudrocks are common in the banded iron‐formations (BIF) of the Brockman Iron Formation. These tuffaceous mudrocks are either stilpnomelane‐rich or siliceous. Their compositions reflect bimodal volcanic activity in the vicinity of the Hamersley BIF depositional site. They also contain complex zircon populations that record resedimentation, syndepositional volcanism and post‐depositional isotopic disturbance. The best estimates of depositional age are obtained from siliceous tuffaceous mudrocks in the Joffre Member that contain 2459 ± 3 Ma and 2454 ± 3 Ma zircon populations most likely derived from felsic volcanism coeval with BIF deposition. These dates constrain the sedimentation rates for the ∼370 m‐thick Joffre Member BIF to >15 m per million years. Siliceous tuffaceous mudrocks are not present in the underlying ∼120 m‐thick Dales Gorge Member and it is uncertain whether previously reported ages of ca 2479–2470 Ma for this unit reflect detrital/xenocrystic or syndepositional zircon populations in resedimented stilpnomelane‐rich tuffaceous mudrocks. The increased abundance of tuffaceous mudrocks in the Joffre Member suggests that a pulse of enhanced igneous and hydrothermal activity accompanied deposition of the bulk of the Brockman Iron Formation BIF after ca 2460 Ma. This preceded and culminated in the emplacement of the 2449 ± 3 Ma large igneous province represented by BIF and igneous rocks of the Weeli Wolli Formation and Woongarra Rhyolite.
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The best age estimates for the deposition of the Dales Gorge and Joffre members are 2494-2464 Ma and 2454±3 Ma, respectively.
“The best age estimates for the deposition of the Dales Gorge and Joffre members are 2494-2464 Ma (Trendall et al., 2004) and 2454±3 Ma (Pickard, 2002), respectively.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Pickard, 2002
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- Authors
- Pickard, A. L.
- Affiliations
- The University of Western Australia (AU)
- Corresponding author
- Pickard, A. L.
- Venue
- Australian Journal of Earth Sciences
- Publisher
- Informa UK Limited
- Published
- 2002-06
- Volume
- 49
- Issue
- 3
- Pages
- 491-507
- ISSN
- 0812-0099 (ISSN-L)
- 1440-0952
- OpenAlex
- W2102206761
- Cited by
- 105
- References
- 27
- Citations by year
- 2026: 1 · 2025: 7 · 2024: 6 · 2023: 3 · 2022: 5 · 2021: 2 · 2020: 4 · 2019: 6 · 2018: 8 · 2017: 6 · 2016: 6 · 2015: 1 · 2014: 5 · 2013: 6 · 2012: 4
- FWCI
- 5.40
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Australian Journal of Earth Sciences (publishedVersion)
- UWA Profiles and Research Repository (UWA) (submittedVersion)
- Funders
- Minerals and Energy Research Institute of Western Australia
- Curtin University of Technology
- Geological Survey of Western Australia
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- 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
- Keywords
- banded iron formations, Hamersley Range, zircon U-Pb geochronology, stilpnomelane, sedimentation rate, resedimentation, felsic volcanism, large igneous provinces, Precambrian stratigraphy, hydrothermal activity
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