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- W55659103 abstract "Lithofacies maps of the northern Great Barrier Reef Province based merely on the proportions of carbonate and siliciclastic components in surface sediments present an over-simplified picture of an across-the-shelf carbonate source. The decrease in the proportion of siliciclastic components across the shelf is not gradual because of the dominance of along-the-shelf sediment transport in the near-shore and inner-shelf. Reefs, in situ post-mortem contributions, and Halimeda meadows are the main sources of carbonate end-members. Siliciclastic end-members are derived from the mainland and high-islands. Mixing of end-members is an important process in determining the nature of most inter-reef sediments, while others may represent lag deposits, dependent for their grain size characteristics upon in situ post-mortem contributions and currents of removal. Cores from the outer shelf banks that are veneered by present Halimeda meadows indicate that Halimeda has been an important source of carbonate in the area during the Holocene." @default.
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- W55659103 date "1988-01-01" @default.
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- W55659103 title "Chapter 6 Mixed Siliciclastic/Carbonate Sediments of the Northern Great Barrier Reef Province, Australia" @default.
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- W55659103 doi "https://doi.org/10.1016/s0070-4571(08)70168-7" @default.
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