Abstract
Deep-water deposits may be defined in terms of ‘architectural elements’ (cf. fluvial models of Miall 1985). In fluvial sedimentology, Miall’s (1985) ‘architectural elements’ are characterized by facies associations and three-dimensional geometry (including orientation). The identification of depositional geometry requires the classification of a hierarchy of bounding surfaces, an approach now widely accepted for fluvial and eolian deposits. Using a hierarchy of bounding surfaces, together with facies analysis and geometry, it is shown how ‘architectural element analysis’ may be used as an aid in the interpretation of deep-water systems and their depositional history.
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Pickering, K.T., Clark, J.D., Smith, R.D.A., Hiscott, R.N., Ricci Lucchi, F., Kenyon, N.H. (1995). Architectural element analysis of turbidite systems, and selected topical problems for sand-prone deep-water systems. In: Pickering, K.T., Hiscott, R.N., Kenyon, N.H., Ricci Lucchi, F., Smith, R.D.A. (eds) Atlas of Deep Water Environments. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1234-5_1
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