Journal of Geophysical Research: Earth Surface

Kinematic controls on the geometry of the preserved cross sets

Authors

  • Vamsi Ganti,

    Corresponding author
    1. Department of Civil Engineering, National Center for Earth-surface Dynamics, St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, Minnesota, USA
    2. Now at Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA
    • Corresponding author: V. Ganti, Division of Geological and Planetary Sciences, California Institute of Technology, MC 170-25, 1200 E. California Blvd., Pasadena, CA 91125, USA. (vganti@caltech.edu)

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  • Chris Paola,

    1. Department of Earth Sciences, National Center for Earth-surface Dynamics, St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, Minnesota, USA
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  • Efi Foufoula-Georgiou

    1. Department of Civil Engineering, National Center for Earth-surface Dynamics, St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, Minnesota, USA
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  • This article was published online on 24 July 2013. Some text has been changed to reflect the wording in Martin and Jerolmack [2013]. This notice is included in the online and print versions to indicate that both have been corrected on 6 September 2013.

Abstract

[1] The geometry of sedimentary strata records the dynamics of the surfaces that produced them. Cross strata are one of the most common features preserved in the stratigraphic record and are typically formed by migrating ripples, dunes, and bars. Cross-stratal geometry depends on the movement and shape of the bed forms. In this study, we provide theoretical relationships that map the statistics of surface kinematics and geometry of migrating bed forms into the 2-D geometrical structure of the preserved stratigraphy. The surface kinematics is characterized by the migration (translation of the waveforms) and deformation (change in shape of the waveforms) of the bed forms. We show that, for transverse, unidirectional bed forms, the local slope and curvature of the preserved stratigraphic boundaries depend on the competition between migration and deformation of the bed forms. Further, we show that deformation is the sole cause of curved cross-set boundaries and define a quantitative relationship between the curvature of the bounding surfaces of the preserved cross sets and the deformation rate of the bed forms. The theoretical results compare well with experimental data of subaqueous, transverse bed form evolution under equilibrium, steady state conditions with no net deposition.

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