Palaeoenvironmental analysis of Archaean siliciclastic sedimentary rocks in the west-central Jack Hills Belt, Western Australia with new constraints on ages and correlations

Zircons with ages between 3.05 and 4.4 Ga and hosted in conglomerates and associated sandstones in the Jack Hills belt of Western Australia have been the subject of numerous studies but none, to date, has been concerned with understanding the depositional environments of the sedimentary rocks. Intac...

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Published inJournal of the Geological Society Vol. 167; no. 4; pp. 827 - 840
Main Authors Eriksson, Kenneth A, Wilde, Simon A
Format Journal Article
LanguageEnglish
Published London, UK Geological Society of London 01.07.2010
The Geological Society of London
Geological Society
Geological Society Publishing House
Subjects
absolute age
Alluvial fans
Archean
arenite
Australasia
Australia
clastic rocks
conglomerate
Conglomerates
Continental crust
correlation
cross-bedding
Crystalline rocks
dates
deltas
depositional environment
Earth sciences
Earth, ocean, space
Exact sciences and technology
facies
fan deltas
Flow velocity
Geology
High flow
Hills
Igneous and metamorphic rocks petrology, volcanic processes, magmas
ion probe data
Jack Hills Belt
lacustrine environment
mass spectra
metamorphic rocks
metasedimentary rocks
nesosilicates
orthosilicates
paleocurrents
paleoenvironment
planar bedding structures
Precambrian
progradation
provenance
Quartz
quartz arenite
Rocks
sandstone
sea-level changes
sed rocks, sediments
Sedimentary petrology
Sedimentary rocks
sedimentary structures
SHRIMP data
silicates
siliciclastics
spectra
Stratigraphy
Studies
succession
transgression
U/Pb
Western Australia
zircon
zircon group
Australia
Western Australia
ISW, Australia, Western Australia
depositional environment
Australasia
arenite
fan deltas
alluvial fans
continental crust
sandstone
zircon
silicates
lakes
flow
clastic rocks
nesosilicates
geologic sections
siliciclastics
reworking
conglomerate
U/Pb
velocity
continents
sedimentary rocks
correlation
discoveries
hills
quartz arenite
Online AccessGet full text
ISSN0016-7649
2041-479X
DOI10.1144/0016-76492008-127

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Abstract Zircons with ages between 3.05 and 4.4 Ga and hosted in conglomerates and associated sandstones in the Jack Hills belt of Western Australia have been the subject of numerous studies but none, to date, has been concerned with understanding the depositional environments of the sedimentary rocks. Intact, 250 and 320 m thick stratigraphical sections include conglomerates and sandstones that are equivalent to those at the W74 discovery site that host the ancient zircons. Facies associations are compatible with a prograding fan delta depositional setting in which alluvial fans were sourced by proximal highlands, were built directly into a lake or sea and were characterized by high gradients and high flow velocities. Locally, the succession is capped by a 20-25 m thick interval of cross-bedded quartz arenite-gritstone with a similar U-Pb detrital zircon age spectrum to the W74 discovery site, suggesting that this facies association is of comparable age and genetically related to the underlying facies associations. The quartz arenite-gritstone facies association is interpreted to record transgressive tidal reworking of the fan delta. Similar sedimentary units, including areally extensive quartz arenite successions, are widely developed elsewhere in Western Australia and on other continents, indicating that stable continental crust was widespread by 3.0 Ga.
AbstractList Zircons with ages between 3.05 and 4.4 Ga and hosted in conglomerates and associated sandstones in the Jack Hills belt of Western Australia have been the subject of numerous studies but none, to date, has been concerned with understanding the depositional environments of the sedimentary rocks. Intact, 250 and 320 m thick stratigraphical sections include conglomerates and sandstones that are equivalent to those at the W74 discovery site that host the ancient zircons. Facies associations are compatible with a prograding fan delta depositional setting in which alluvial fans were sourced by proximal highlands, were built directly into a lake or sea and were characterized by high gradients and high flow velocities. Locally, the succession is capped by a 20–25 m thick interval of cross-bedded quartz arenite–gritstone with a similar U–Pb detrital zircon age spectrum to the W74 discovery site, suggesting that this facies association is of comparable age and genetically related to the underlying facies associations. The quartz arenite–gritstone facies association is interpreted to record transgressive tidal reworking of the fan delta. Similar sedimentary units, including areally extensive quartz arenite successions, are widely developed elsewhere in Western Australia and on other continents, indicating that stable continental crust was widespread by 3.0 Ga.
Zircons with ages between 3.05 and 4.4 Ga and hosted in conglomerates and associated sandstones in the Jack Hills belt of Western Australia have been the subject of numerous studies but none, to date, has been concerned with understanding the depositional environments of the sedimentary rocks. Intact, 250 and 320 m thick stratigraphical sections include conglomerates and sandstones that are equivalent to those at the W74 discovery site that host the ancient zircons. Facies associations are compatible with a prograding fan delta depositional setting in which alluvial fans were sourced by proximal highlands, were built directly into a lake or sea and were characterized by high gradients and high flow velocities. Locally, the succession is capped by a 20-25 m thick interval of cross-bedded quartz arenite-gritstone with a similar U-Pb detrital zircon age spectrum to the W74 discovery site, suggesting that this facies association is of comparable age and genetically related to the underlying facies associations. The quartz arenite-gritstone facies association is interpreted to record transgressive tidal reworking of the fan delta. Similar sedimentary units, including areally extensive quartz arenite successions, are widely developed elsewhere in Western Australia and on other continents, indicating that stable continental crust was widespread by 3.0 Ga. [PUBLICATION ABSTRACT]
Author Eriksson, Kenneth A
Wilde, Simon A
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Issue 4
Keywords depositional environment
Australasia
arenite
fan deltas
alluvial fans
continental crust
sandstone
zircon
silicates
lakes
flow
clastic rocks
nesosilicates
geologic sections
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Snippet Zircons with ages between 3.05 and 4.4 Ga and hosted in conglomerates and associated sandstones in the Jack Hills belt of Western Australia have been the...
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SubjectTerms absolute age
Alluvial fans
Archean
arenite
Australasia
Australia
clastic rocks
conglomerate
Conglomerates
Continental crust
correlation
cross-bedding
Crystalline rocks
dates
deltas
depositional environment
Earth sciences
Earth, ocean, space
Exact sciences and technology
facies
fan deltas
Flow velocity
Geology
High flow
Hills
Igneous and metamorphic rocks petrology, volcanic processes, magmas
ion probe data
Jack Hills Belt
lacustrine environment
mass spectra
metamorphic rocks
metasedimentary rocks
nesosilicates
orthosilicates
paleocurrents
paleoenvironment
planar bedding structures
Precambrian
progradation
provenance
Quartz
quartz arenite
Rocks
sandstone
sea-level changes
sed rocks, sediments
Sedimentary petrology
Sedimentary rocks
sedimentary structures
SHRIMP data
silicates
siliciclastics
spectra
Stratigraphy
Studies
succession
transgression
U/Pb
Western Australia
zircon
zircon group
Title Palaeoenvironmental analysis of Archaean siliciclastic sedimentary rocks in the west-central Jack Hills Belt, Western Australia with new constraints on ages and correlations
URI https://pubs.geoscienceworld.org/jgs/article/167/4/827/372886
https://www.lyellcollection.org/doi/10.1144/0016-76492008-127
https://www.proquest.com/docview/577609294
https://www.proquest.com/docview/754534034
Volume 167
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