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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Published in | IEEE journal of oceanic engineering Vol. 14; no. 4; pp. 338 - 347 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
New York, NY
IEEE
01.10.1989
Institute of Electrical and Electronics Engineers |
Subjects | |
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Abstract | 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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AbstractList | At scales of tens to hundreds of kilometers, the most prevalent patterns on the seafloor are those formed by the succession of elongate abyssal hills. This seafloor fabric, generated at the ridge axis and modified by sedimentation, mass wasting, and volcanism as it moves away from the ridge, is a record of geologic interest. In this paper the authors describe a method for obtaining parameters from Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity that they use in their analysis is the distribution of topographic slopes in a region. They apply the slope-analysis method to three regions in the Northeast Pacific Ocean and two regions in the Southwest Indian Ocean. 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 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.< > |
Author | Smith, D.K. Shaw, P.R. |
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References | ref13 ref12 ref15 ref31 ref30 ref11 ref2 menard (ref20) 1964 ref1 ref17 ref16 davis (ref26) 1973 ref19 pittman (ref32) 1974 ref18 yesyunin (ref10) 1975; 15 ref24 ref23 ref25 ref22 ref21 ref28 ref27 ref29 renard (ref14) 1979; 56 ref8 ref7 ref4 ref3 ref6 ref5 krause (ref9) 1973 |
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Snippet | The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic... At scales of tens to hundreds of kilometers, the most prevalent patterns on the seafloor are those formed by the succession of elongate abyssal hills. This... |
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SubjectTerms | abyssal hills Azimuth bathymetry Coastal oceanography, estuaries. Regional oceanography Density functional theory Earth, ocean, space Exact sciences and technology External geophysics Fabrics Geology INE Marine mid-ocean ridges Oceanographic techniques oceanography Oceans Physics of the oceans Robustness Sea floor Shape signal processing statistical analysis Surfaces swaths topography |
Title | Using topographic slope distributions to infer seafloor patterns |
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