In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia

In sedimentary basins, the determination of the absolute timing of deposition and diagenetic events is a challenging yet critical parameter necessary in the reconstruction of paleo-fluid evolution and burial histories. Here we demonstrate the practical application of in situ calcite U–Pb geochronolo...

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Main Authors: Li, Zhen, Rankenburg, Kai, Normore, L.S., Evans, Noreen, McInnes, Brent, Dent, L.M., Fielding, I.O.H.
Format: Journal Article
Language:English
Published: TAYLOR & FRANCIS LTD 2023
Subjects:
Online Access:http://purl.org/au-research/grants/arc/LE140100150
http://hdl.handle.net/20.500.11937/95550
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author Li, Zhen
Rankenburg, Kai
Normore, L.S.
Evans, Noreen
McInnes, Brent
Dent, L.M.
Fielding, I.O.H.
author_facet Li, Zhen
Rankenburg, Kai
Normore, L.S.
Evans, Noreen
McInnes, Brent
Dent, L.M.
Fielding, I.O.H.
author_sort Li, Zhen
building Curtin Institutional Repository
collection Online Access
description In sedimentary basins, the determination of the absolute timing of deposition and diagenetic events is a challenging yet critical parameter necessary in the reconstruction of paleo-fluid evolution and burial histories. Here we demonstrate the practical application of in situ calcite U–Pb geochronology on core samples from the Olympic 1 well in the Canning Basin of Western Australia. Using quantitative mineralogy and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) analytical techniques, we obtained an authigenic calcite U–Pb age of 469.7 ± 4.3 Ma for limestone in the Samphire Marsh Member of the Lower Ordovician Nambeet Formation. This precise depositional age can be independently verified using zircon thermal ionisation mass spectrometry U–Pb ages of 479.4 to 470.2 Ma determined on adjacent volcanic ash beds. Further geochronology studies on calcite cements from the Lower Ordovician Fly Flat Member sandstone from the Nambeet Formation returned a U–Pb age of 365.3 ± 5.8 Ma. This is the first study to place absolute age constraints on the diagenetic event that occluded the intergranular space in a sandstone reservoir. The calcite cementation age suggests that impairment of reservoir quality in the Fly Flat Member sandstone occurred in the Late Devonian, much earlier than major petroleum charge events in the Canning Basin. The calcite U–Pb geochronometer, when combined with complementary quantitative mineralogical analysis, can build direct temporal constraints on the depositional and diagenetic processes in both carbonate and clastic sedimentary rocks in basins worldwide.
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spelling curtin-20.500.11937-955502024-10-10T01:43:24Z In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia Li, Zhen Rankenburg, Kai Normore, L.S. Evans, Noreen McInnes, Brent Dent, L.M. Fielding, I.O.H. Science & Technology Physical Sciences Geosciences, Multidisciplinary Geology deposition of sediments diagenesis in situ calcite U-Pb dating automated quantitative mineralogy carbonate sandstone Canning Basin AGE EVOLUTION In sedimentary basins, the determination of the absolute timing of deposition and diagenetic events is a challenging yet critical parameter necessary in the reconstruction of paleo-fluid evolution and burial histories. Here we demonstrate the practical application of in situ calcite U–Pb geochronology on core samples from the Olympic 1 well in the Canning Basin of Western Australia. Using quantitative mineralogy and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) analytical techniques, we obtained an authigenic calcite U–Pb age of 469.7 ± 4.3 Ma for limestone in the Samphire Marsh Member of the Lower Ordovician Nambeet Formation. This precise depositional age can be independently verified using zircon thermal ionisation mass spectrometry U–Pb ages of 479.4 to 470.2 Ma determined on adjacent volcanic ash beds. Further geochronology studies on calcite cements from the Lower Ordovician Fly Flat Member sandstone from the Nambeet Formation returned a U–Pb age of 365.3 ± 5.8 Ma. This is the first study to place absolute age constraints on the diagenetic event that occluded the intergranular space in a sandstone reservoir. The calcite cementation age suggests that impairment of reservoir quality in the Fly Flat Member sandstone occurred in the Late Devonian, much earlier than major petroleum charge events in the Canning Basin. The calcite U–Pb geochronometer, when combined with complementary quantitative mineralogical analysis, can build direct temporal constraints on the depositional and diagenetic processes in both carbonate and clastic sedimentary rocks in basins worldwide. 2023 Journal Article http://hdl.handle.net/20.500.11937/95550 10.1080/08120099.2023.2161635 English http://purl.org/au-research/grants/arc/LE140100150 TAYLOR & FRANCIS LTD restricted
spellingShingle Science & Technology
Physical Sciences
Geosciences, Multidisciplinary
Geology
deposition of sediments
diagenesis
in situ calcite U-Pb dating
automated quantitative mineralogy
carbonate
sandstone
Canning Basin
AGE
EVOLUTION
Li, Zhen
Rankenburg, Kai
Normore, L.S.
Evans, Noreen
McInnes, Brent
Dent, L.M.
Fielding, I.O.H.
In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia
title In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia
title_full In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia
title_fullStr In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia
title_full_unstemmed In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia
title_short In situ calcite U–Pb geochronology of carbonate and clastic sedimentary rocks from the Canning Basin, Western Australia
title_sort in situ calcite u–pb geochronology of carbonate and clastic sedimentary rocks from the canning basin, western australia
topic Science & Technology
Physical Sciences
Geosciences, Multidisciplinary
Geology
deposition of sediments
diagenesis
in situ calcite U-Pb dating
automated quantitative mineralogy
carbonate
sandstone
Canning Basin
AGE
EVOLUTION
url http://purl.org/au-research/grants/arc/LE140100150
http://hdl.handle.net/20.500.11937/95550