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Deformational Structures (1963–1976)

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Paleocurrents and Basin Analysis

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Abstract

Structures due to deformation contemporaneous with sedimentation continue to attract attention. Interest has focused on structures produced by those vertical or convective movements due to inverse density stratification and on those structures related to dewatering of sediments and momentary “liquification” and, also, on the largest deformational features — olistostromes — structures difficult to distinguish from true tectonic melanges. The relations between olistostromes, turbidites, and tectonics are explored by Abbate (1970b). The deformational structures generally have limited paleocurrent value except perhaps those produced by slump or other lateral movements which are presumed to define the paleoslope.

Much better understanding of the largest of all deformational structures — olistostromes — plus recognition of dewatering during compaction as an agent for much internal deformation of silts and sands.

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Annotated References of Experimental and Theoretical Studies

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Authors and Affiliations

  1. Department of Geology, University of Cincinnati, Old Tech Building, Cincinnati, OH, 45221, USA

    Prof. Paul Edwin Potter

  2. Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, MD, 21218, USA

    Prof. Francis J Pettijohn

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  1. Prof. Paul Edwin Potter
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  2. Prof. Francis J Pettijohn
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© 1977 Springer-Verlag Berlin Heidelberg

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Potter, P.E., Pettijohn, F.J. (1977). Deformational Structures (1963–1976). In: Paleocurrents and Basin Analysis. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-61887-1_11

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  • DOI: https://doi.org/10.1007/978-3-642-61887-1_11

  • Publisher Name: Springer, Berlin, Heidelberg

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