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• W2133751738 startingPage "481" @default.
• W2133751738 abstract "The southeastern Lachlan Fold Belt at Batemans Bay on the New South Wales south coast is an accretionary complex with a prolonged deformation history. Early features include synsedimentary folds, mélange, disaggregated bedding and faults. Fabrics within the clast-in-matrix mélange and mudstone match those found in cores from the lower slopes of modern accretionary prisms. At the toe of the accretionary prism, the contact between the craton-derived Adaminaby Group and ocean floor deposits of the Wagonga Group is conformable. As subduction continued, the early structures were overprinted by (D1) deformation that produced meridional north – south-trending, tight to isoclinal folds (F1) and associated axial-plane cleavage (S1). This west-dipping subduction occurred in the Late Ordovician/Early Silurian but probably began much earlier. A younger regional deformation (D2) resulted in north – south-trending, open to tight folds (F2), slightly oblique to F1, and an axial-surface cleavage (S2)." @default.
• W2133751738 created "2016-06-24" @default.
• W2133751738 creator A5079710889 @default.
• W2133751738 date "2007-06-01" @default.
• W2133751738 modified "2023-09-23" @default.
• W2133751738 title "Early Palaeozoic subduction in the southeastern Lachlan Fold Belt, Batemans Bay, New South Wales" @default.
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• W2133751738 doi "https://doi.org/10.1080/08120090600981475" @default.
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