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The shape of deep-water siliciclastic systems: A discussion

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Abstract

Deep-water siliciclastic systems are classified primarily on their shape as: submarine fans with well developed or poorly developed morphology, slope drapes, for example, over relatively stable basin margins, fault-scarp aprons, canyons and large channels, under-supplied sheet systems such as abyssal plains, non-fan ponded systems such as over-supplied perched basins, and fan deltas. Collectively, or separately, these systems may form sedimentary basin fills that can be over or under-supplied with respect to the sediment input although most systems will tend toward over-supply/overflow with time. Finally, the sum total of the siliciclastic systems and basins can be used to define the tectonic milieux such as passive, strike-slip and convergent margins.

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  1. Department of Geology, University of London, Goldsmiths' College, Rachel McMillan Building, Creek Rd., SE8 3BU, London, U.K.

    K. T. Pickering

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Pickering, K.T. The shape of deep-water siliciclastic systems: A discussion. Geo-Marine Letters 2, 41–46 (1982). https://doi.org/10.1007/BF02462798

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