Definition and description
Ball-and-pillow structure is a soft-sediment deformation structure comprising rounded masses of clastic sediment (pseudonodules, q.v.) set in similar or finer grained matrix, that are vertically stacked within one horizon (Figure B2(A), (B)). Much of the discussion in the entry for pseudonodules, relating to their description and their origin through loading processes related to variations in gravitational potential energy, is relevant to ball-and-pillow structure. Distinctive features of ball-and-pillow structure include: the pseudonodules are commonly contorted into spiral or zig zag shapes; there may be very little matrix between the pseudonodules; and some ball-and-pillow horizons are consistently underlain by convolute stratification and overlain by dish structure.
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Bibliography
Allen, J.R.L., 1982. Sedimentary Structures: their Character and Physical Basis. Amsterdam: Elsevier.
Kuenen, Ph.H., 1958. Experiments in geology. Transactions of the Geological Society of Glasgow, 23: 1–28.
Potter, P.E., and Pettijohn, F.J., 1963. Paleocurrents and Basin Analysis. Berlin: Springer-Verlag.
Smith, B., 1916. Ball or pillow-form structures in sandstones. Geological Magazine, 53: 146–156.
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© 1978 Dowden, Hutchinson & Ross, Inc.
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Owen, G. (1978). Ball-and-pillow (pillow) structure. In: Sedimentology. Encyclopedia of Earth Science. Springer, Berlin, Heidelberg . https://doi.org/10.1007/3-540-31079-7_18
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