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- W2036708963 abstract "The Early Devonian Walhalla Group is a turbidite sequence deposited on the eastern margin of the Melbourne Trough. Five lithofacies were identified: (1) massive sandstones; (2) turbidites with a basal Ta division; (3) turbidites with a basal laminated division (Tb or Td); (4) fine grained, rippled sandstones interbedded with shales; and (5) shales and siltstones. Episodic reworking by water currents has produced reworking features such as wave‐current and unidirectional current ripples, sharp topped turbidites and interrupted Bouma sequences. The reworking was attributed to storm currents indicating that the sequence was deposited above storm‐weather wave‐base. Palaeobathymetric calculations, based on wave ripple geometry, are consistent with geological observations, and suggest that deposition took place in 65–90 m of water. The relatively shallow water depths implied, combined with the general areal continuity of lithofacies, suggested that the turbidites are sheet‐like deposits originating from a distr..." @default.
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- W2036708963 date "1988-12-01" @default.
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- W2036708963 title "Sedimentology of the Early Devonian Walhalla Group at Walhalla, Victoria" @default.
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- W2036708963 doi "https://doi.org/10.1080/08120098808729459" @default.
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