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ARTICLE IN PRESS Quaternary Science Reviews xxx (2008) 1–15 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Episodic intraplate deformation of stable continental margins: evidence from Late Neogene and Quaternary marine terraces, Cape Liptrap, Southeastern Australia Thomas Gardner a,*, John Webb b, Claudia Pezzia a, Terri Amborn a, Robert Tunnell a, Sarah Flanagan a, Dorothy Merritts a, Jeffrey Marshall a, Derek Fabel c, Matthew L. Cupper d a Keck Geology Consortium, Department of Earth and Environment, Franklin & Marshall College, P.O. Box 3003, Lancaster, PA 17604-3003, USA b School of Environmental Science, La Trobe University, Victoria 3086, Australia c Department of Geographical and Earth Sciences, East Quadrangle, University of Glasgow, Glasgow G12 8QQ, UK d School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia article info abstract Article history: The Waratah Fault is a northeast trending, high angle, reverse fault in the Late Paleozoic Lachlan Fold Belt Received 4 February 2008 at Cape Liptrap on the Southeastern Australian Coast. It is susceptible to reactivation in the modern Received in revised form intraplate stress field in Southeast Australia and exhibits Late Pliocene to Late Pleistocene reactivation. 7 October 2008 Radiocarbon, optically stimulated luminescence (OSL), and cosmogenic radionuclide (CRN) dating of Accepted 9 October 2008 marine terraces on Cape Liptrap are used to constrain rates of displacement across the reactivated Available online xxx Waratah Fault. Six marine terraces, numbered Qt6–Tt1 (youngest to oldest), are well developed at Cape Liptrap with altitudes ranging from w1.5 m to w170 m amsl, respectively.
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