Using topographic slope distributions to infer seafloor patterns

The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity used in the analysis is the distribution of topographic slopes in a region. A convenient means for parameterizing these slopes is thro...

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Bibliographic Details
Published inIEEE journal of oceanic engineering Vol. 14; no. 4; pp. 338 - 347
Main Authors Smith, D.K., Shaw, P.R.
Format Journal Article
LanguageEnglish
Published New York, NY IEEE 01.10.1989
Institute of Electrical and Electronics Engineers
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Summary:The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity used in the analysis is the distribution of topographic slopes in a region. A convenient means for parameterizing these slopes is through unit vectors that are normal to small patches of the seafloor; the normal vectors are decomposed into azimuthal and dip components. It is found that the azimuthal distribution of the vectors provides a first-order indication of the dominant elongation directions in the topography, including multiple lineations when they are present. It is shown that the slope statistics are relatively independent of long-wavelength depth variations and are robust even if large anomalous features such as seamounts and fracture zones are included in the section of bathymetry analyzed.< >
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ISSN:0364-9059
1558-1691
DOI:10.1109/48.35984