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 in | Geological magazine Vol. 160; no. 8; pp. 1535 - 1555 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Cambridge, UK
Cambridge University Press
01.08.2023
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Subjects | |
Online Access | Get full text |
ISSN | 0016-7568 1469-5081 |
DOI | 10.1017/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. |
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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 |
Author_xml | – sequence: 1 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 – sequence: 2 givenname: Robin surname: Offler fullname: Offler, Robin organization: 2School of Environmental and Life Sciences, University of Newcastle, Callaghan NSW, Australia – sequence: 3 givenname: Chrysanthos surname: Botziolis fullname: Botziolis, Chrysanthos organization: 3Laboratory of Sedimentology, Department of Geology, University of Patras, Rion, Greece – sequence: 4 givenname: George surname: Pantopoulos fullname: Pantopoulos, George organization: 4Department of Earth Sciences “Ardito Desio”, University of Milan, Milan, Italy – sequence: 5 givenname: Alexandra surname: Scott fullname: Scott, Alexandra organization: 2School of Environmental and Life Sciences, University of Newcastle, Callaghan NSW, Australia – sequence: 6 givenname: Bill surname: Landenberger fullname: Landenberger, Bill organization: 2School of Environmental and Life Sciences, University of Newcastle, Callaghan NSW, Australia – sequence: 7 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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Keywords | tectonic setting provenance Permian retroarc foreland basin Northern Sydney Basin |
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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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