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- W2034939752 abstract "U–Pb ages for volcanic zircons from the Lower Devonian Turondale and Merrions Formations initially dated by Jagodzinski and Black (1999) have been recalculated by Compston (2000, 2001). The Turondale, Waterbeach and Merrions Formations are, in ascending stratigraphic order, three of the Lower Devonian deep‐water formations of the Hill End Trough. The recent discovery of a Lochkovian conodont fauna of the delta zone in derived limestone blocks from the uppermost beds of the Turondale Formation has established a maximum age for that horizon. The principal lithological assemblages of the formations are volcanic (megaturbidite and lavas), epiclastic turbidites and essentially hemipelagic lithologies. The mean zircon ages suggest a long duration for the Merrions Formation, 615 m thick and 91% volcanic, and a very much shorter interval for the upper two‐thirds of the Turondale Formation, 360 m thick and 34% volcanic, plus the intervening non‐volcanic Waterbeach Formation, 512 m thick. A sedimentological model b..." @default.
- W2034939752 created "2016-06-24" @default.
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- W2034939752 date "2003-04-01" @default.
- W2034939752 modified "2023-09-27" @default.
- W2034939752 title "U–Pb SHRIMP ages of volcanic zircons from the Merrions and Turondale Formations, New South Wales, and the Early Devonian time‐scale: A biostratigraphic and sedimentological assessment" @default.
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- W2034939752 doi "https://doi.org/10.1046/j.1440-0952.2003.00985.x" @default.
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