Provenance of a Late Permian retroarc foreland basin along the eastern Gondwanan margin: northern Sydney Basin, eastern Australia

The Upper Permian sedimentary successions in the northern Sydney Basin have been the subject of several stratigraphic, sedimentological and coal petrographic studies, and recently, extensive U-Pb zircon dating has been carried out on tuffs in the Newcastle Coal Measures. However, detailed petrograph...

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Published inGeological magazine Vol. 160; no. 8; pp. 1535 - 1555
Main Authors Maravelis, Angelos G., Offler, Robin, Botziolis, Chrysanthos, Pantopoulos, George, Scott, Alexandra, Landenberger, Bill, Collins, William J.
Format Journal Article
LanguageEnglish
Published Cambridge, UK Cambridge University Press 01.08.2023
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ISSN0016-7568
1469-5081
DOI10.1017/S0016756823000535

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Abstract The Upper Permian sedimentary successions in the northern Sydney Basin have been the subject of several stratigraphic, sedimentological and coal petrographic studies, and recently, extensive U-Pb zircon dating has been carried out on tuffs in the Newcastle Coal Measures. However, detailed petrographic and geochemical studies of these successions are lacking. These are important because a major change in tectonic setting occurred prior to the Late Permian because of the Hunter-Bowen Orogeny that caused the uplift of the Carboniferous and Devonian successions in the Tamworth Group and Tablelands Complex adjacent to the Sydney Basin. This should be reflected in the detrital makeup of the Upper Permian rocks. This study provides data that confirms major changes did take place at this time. Petrographic analysis indicates that the source area is composed of sedimentary, felsic volcanic and plutonic and low-grade metamorphic rocks. Conglomerate clast composition analysis confirms these results, revealing a source region that is composed of felsic volcanics, cherts, mudstones and sandstones. Geochemical analysis suggests that the sediments are geochemically mature and have undergone a moderate degree of weathering. The provenance data presented in this paper indicate that the southern New England Orogen is the principal source of detritus in the basin. Discrimination diagrams confirm that the source rocks derive from an arc-related, contractional setting and agree with the provenance analyses that indicate sediment deposition in a retroarc foreland basin. This study offers new insights on the provenance and tectonic setting of the Northern Sydney Basin, eastern Australia.
AbstractList The Upper Permian sedimentary successions in the northern Sydney Basin have been the subject of several stratigraphic, sedimentological and coal petrographic studies, and recently, extensive U-Pb zircon dating has been carried out on tuffs in the Newcastle Coal Measures. However, detailed petrographic and geochemical studies of these successions are lacking. These are important because a major change in tectonic setting occurred prior to the Late Permian because of the Hunter-Bowen Orogeny that caused the uplift of the Carboniferous and Devonian successions in the Tamworth Group and Tablelands Complex adjacent to the Sydney Basin. This should be reflected in the detrital makeup of the Upper Permian rocks. This study provides data that confirms major changes did take place at this time. Petrographic analysis indicates that the source area is composed of sedimentary, felsic volcanic and plutonic and low-grade metamorphic rocks. Conglomerate clast composition analysis confirms these results, revealing a source region that is composed of felsic volcanics, cherts, mudstones and sandstones. Geochemical analysis suggests that the sediments are geochemically mature and have undergone a moderate degree of weathering. The provenance data presented in this paper indicate that the southern New England Orogen is the principal source of detritus in the basin. Discrimination diagrams confirm that the source rocks derive from an arc-related, contractional setting and agree with the provenance analyses that indicate sediment deposition in a retroarc foreland basin. This study offers new insights on the provenance and tectonic setting of the Northern Sydney Basin, eastern Australia.
Author Offler, Robin
Maravelis, Angelos G.
Collins, William J.
Pantopoulos, George
Scott, Alexandra
Landenberger, Bill
Botziolis, Chrysanthos
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  givenname: Angelos G.
  orcidid: 0000-0002-9694-7500
  surname: Maravelis
  fullname: Maravelis, Angelos G.
  email: angmar@geo.auth.gr
  organization: 1Department of Geology, Aristotle University of Thessaloniki, Thessaloniki, Greece
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  givenname: Robin
  surname: Offler
  fullname: Offler, Robin
  organization: 2School of Environmental and Life Sciences, University of Newcastle, Callaghan NSW, Australia
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  givenname: Chrysanthos
  surname: Botziolis
  fullname: Botziolis, Chrysanthos
  organization: 3Laboratory of Sedimentology, Department of Geology, University of Patras, Rion, Greece
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  givenname: George
  surname: Pantopoulos
  fullname: Pantopoulos, George
  organization: 4Department of Earth Sciences “Ardito Desio”, University of Milan, Milan, Italy
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  givenname: Alexandra
  surname: Scott
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  organization: 2School of Environmental and Life Sciences, University of Newcastle, Callaghan NSW, Australia
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  givenname: Bill
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  organization: 2School of Environmental and Life Sciences, University of Newcastle, Callaghan NSW, Australia
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  givenname: William J.
  surname: Collins
  fullname: Collins, William J.
  organization: 5The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, Perth WA, Australia
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CitedBy_id crossref_primary_10_1016_j_coal_2024_104628
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Issue 8
Keywords tectonic setting
provenance
Permian
retroarc foreland basin
Northern Sydney Basin
Language English
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Snippet The Upper Permian sedimentary successions in the northern Sydney Basin have been the subject of several stratigraphic, sedimentological and coal petrographic...
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SubjectTerms Analysis
Basins
Carboniferous
Coal
Conglomerates
Dating
Detritus
Devonian
Geochemistry
Geochronometry
Gondwana
Metamorphic rocks
Original Article
Orogeny
Permian
Radiometric dating
Sandstone
Sediment
Sediments
Stratigraphy
Tectonics
Uplift
Zircon
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Title Provenance of a Late Permian retroarc foreland basin along the eastern Gondwanan margin: northern Sydney Basin, eastern Australia
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