Construction of the Yilgarn Craton over 1.5 billion years
<div>The Yilgarn Craton of Western Australia represents one of the largest pieces of Precambrian crust on Earth, and a key repository of information on the Meso-Neoarchean period. Understanding the crustal, tectonic, thermal, and chemical evolution of the craton is critical in placing these events into an accurate geological context, as well as developing holistic tectonic models for the Archean Earth. In this study, we collected a large U-Pb (420 collated samples) and Hf isotopic (2163 analyses) dataset on zircon to investigate the evolution of the craton. These data provide strong evidence for a Hadean-Eoarchean origin for the Yilgarn Craton from mafic crust at ca. 4000 Ma. This ancient cratonic nucleus was subsequently rifted, expanded and reworked by successive crustal growth events at ca. 3700 Ma, ca. 3300 Ma, 3000-2900 Ma, 2825-2800 Ma, and ca. 2730-2620 Ma. The <3050 Ma crustal growth events correlate broadly with known komatiite events, and patterns of craton evolution, revealed by Hf isotope time-slice mapping, image the periodic break-up of the Yilgarn proto-continent and the formation of rift-zones between the older crustal blocks. Crustal growth and new magmatic pulses were focused into these zones and at craton margins, resulting in continent growth via internal (rift-enabled) expansion, and peripheral (crustal extraction at craton margins) magmatism. Consequently, we interpret these major geodynamic processes to be analogous to plume-lid tectonics, where the majority of tonalite-trondhjemite-granodiorite (TTG) felsic crust, and later granitic crust, was formed by reworking of hydrated mafic rocks and TTGs, respectively, via a combination of infracrustal and/or drip-tectonic settings. While this process of crust formation and evolution is not necessarily restricted to a specific geodynamic system, we find limited direct evidence that subduction-like processes formed a major tectonic component, aside from re-docking the Narryer Terrane to the craton at ca. 2740 Ma. Overall, these 'rift-expansion' and 'craton margin' crustal growth process led to an intra-cratonic architecture of younger, juvenile terranes located internal and external to older, long-lived, reworked crustal blocks. This framework provided pathways that localized later magmas and fluids, driving the exceptional mineral endowment of the Yilgarn Craton.</div>
This Abstract/Poster was submitted to & presented at the 2023 6th International Archean Symposium (6IAS) 25 - 27 July ( https://6ias.org/)
Simple
Identification info
- Date (Creation)
- 2023-02-16T07:00:00
- Date (Publication)
- 2023-09-14T23:00:40
- Citation identifier
- Geoscience Australia Persistent Identifier/https://pid.geoscience.gov.au/dataset/ga/147724
- Cited responsible party
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Role Organisation / Individual Name Details Publisher Commonwealth of Australia (Geoscience Australia)
Voice Author Mole, D.
Internal Contact Author Kirkland, C.L.
External Contact Author Fiorentini, M.L.
External Contact Author Barnes, S.J.
External Contact Author Cassidy, K.F.
External Contact Author Belousova, E.A.
External Contact Author Hartnady, M.
External Contact Author Thebaud, N.
External Contact
- Name
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6th International Archean Symposium 25-27 July 2023 Fremantle Perth WA
- Purpose
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Conference abstract for the 6th International Archean Symposium in Perth, WA 25-27th July 2023.
- Status
- Completed
- Point of contact
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Role Organisation / Individual Name Details Resource provider Minerals, Energy and Groundwater Division
External Contact Point of contact Commonwealth of Australia (Geoscience Australia)
Voice Point of contact Mole, D.
Internal Contact
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- Geoscientific information
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))
- Maintenance and update frequency
- Not planned
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- Title
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Product data repository: Various Formats
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Data Store directory containing the digital product files
Data Store directory containing one or more files, possibly in a variety of formats, accessible to Geoscience Australia staff only for internal purposes
- Keywords
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Yilgarn Craton
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Archean
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zircon
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continental crust
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Western Australia
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Lu-Hf isotopes
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Isotopic mapping
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- theme.ANZRC Fields of Research.rdf
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Isotope geochemistry
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Published_External
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Resource constraints
- Title
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Creative Commons Attribution 4.0 International Licence
- Alternate title
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CC-BY
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4.0
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Role Organisation / Individual Name Details User Any
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© Commonwealth of Australia (Geoscience Australia) 2023
Resource constraints
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Australian Government Security Classification System
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- 2018-11-01T00:00:00
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Australian Government Security Classification System
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- English
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- UTF8
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Role Organisation / Individual Name Details Distributor Commonwealth of Australia (Geoscience Australia)
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Link to Conference Page
Link to Conference Page
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- OnLine resource
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Link to Abstract Volume
Link to Abstract Volume
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Download Poster (pdf) [8.4 MB]
Download Poster (pdf) [8.4 MB]
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pdf
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nil
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Resource lineage
- Statement
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<div>Data were created during the primary authors PhD in 2012, and subsequently published in Earth Science Reviews in 2019. This abstract is a summary of that work.</div>
Metadata constraints
- Title
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Australian Government Security Classification System
- Edition date
- 2018-11-01T00:00:00
- Classification
- Unclassified
Metadata
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urn:uuid/bbef5c62-2781-450a-9a6f-76708db6426e
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GeoNetwork UUID
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Role Organisation / Individual Name Details Point of contact Commonwealth of Australia (Geoscience Australia)
Voice Point of contact Mole, D.
Internal Contact
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Conference Abstract
Alternative metadata reference
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Geoscience Australia - short identifier for metadata record with
uuid
- Citation identifier
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- Date info (Creation)
- 2023-09-14T22:43:27
- Date info (Revision)
- 2023-09-14T22:43:27
Metadata standard
- Title
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AU/NZS ISO 19115-1:2014
Metadata standard
- Title
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ISO 19115-1:2014
Metadata standard
- Title
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ISO 19115-3
- Title
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Geoscience Australia Community Metadata Profile of ISO 19115-1:2014
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Version 2.0, September 2018
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- http://pid.geoscience.gov.au/dataset/ga/122551