Depositional age and provenance of the Cobar Supergroup |
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| Authors: | M D Parrish R A Hegarty P J Gilmore H-Q Huang |
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| Institution: | 1. NSW Institute for Frontiers Geoscience, University of Newcastle, Newcastle, NSW 2308, Australia;2. Geological Survey of New South Wales, NSW Department of Planning and Environment, NSW 2310, Australia;3. Division of Tropical Environments and Societies, James Cook University, Townsville, QLD 4814, Australia |
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| Abstract: | AbstractThe turbidite-filled, Lower Devonian Cobar Basin is characterised through a detrital zircon study. Uranium–Pb age data for six samples were combined with published data to show the basin has a unique age spectrum characterised by a subordinate Middle Ordovician (ca 470?Ma) peak superimposed on a dominant ca 500?Ma peak. Maximum depositional ages for 3 samples were ca 425?Ma, close to the published Lower Devonian (Lochkovian 419–411?Ma) biostratigraphic ages. A minor ca 1000?Ma zircon population was also identified. The major source of the 500?Ma zircons was probably the local Ordovician metasedimentary basement, which was folded, thickened and presumably exposed during the ca 440?Ma Benambran Orogeny. The ca 470?Ma age peak reflects derivation from Middle Ordovician (Phase 2) rocks of the Macquarie Arc to the east. The I-type Florida Volcanics, located ～50?km eastward from the Cobar Basin, contains distinctive Middle and Late Ordovician zircon populations, considered to be derived from deeply underthrust Macquarie Arc crust. Protracted silicic magmatism occurred before, during and after Cobar Basin deposition, indicating that the basin formed by subduction-related processes in a back-arc setting, rather than as a continental rift. |
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| Keywords: | Cobar Basin U-Pb detrital zircon ages Thomson Orogen Tasmanides tectonics Cobar Supergroup |
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