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.
CITATION STYLE
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 Atlas of Deep Water Environments (pp. 1–10). Springer Netherlands. https://doi.org/10.1007/978-94-011-1234-5_1
Mendeley helps you to discover research relevant for your work.