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- W2061493693 abstract "Abstract Re‐examination of the Silurian to Early Devonian lithofacies, biofacies and sediment movement patterns for the Melbourne Trough suggests a palaeogeography orientated N‐S. The Melbourne Trough became progressively shallower from the late Wenlock to the early Ludlow, culminating in fringing of the trough margins by limestone and/or shallow water elastics in the Pragian. The central portion of the Trough in the Yea‐Eildon area continued to receive sediments into a deep water environment throughout the preserved depositional history of the trough, until the final depositional phase of the non‐marine red bed facies of the Middle Devonian." @default.
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- W2061493693 date "1983-07-01" @default.
- W2061493693 modified "2023-10-16" @default.
- W2061493693 title "Silurian to early devonian facies and biofacies patterns for the Melbourne Trough, central Victoria" @default.
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- W2061493693 doi "https://doi.org/10.1080/00167618308729241" @default.
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