A model for attenuation of backscatter due to sediment accumulations and its application to determine sediment thicknesses with GLORIA sidescan sonar
- 10 December 1993
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 98 (B12), 22477-22493
- https://doi.org/10.1029/93jb02217
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Speculations on the geological causes of backscatter variation on GLORIA sonographs from the Mississippi and De Soto fans, Gulf of MexicoGeo-Marine Letters, 1992
- Climatic change and CaCO3 preservation: An 800,000 year bathymetric Reconstruction from the central equatorial Pacific OceanPaleoceanography and Paleoclimatology, 1989
- Attenuation of sound in marine sediments: A review with emphasis on new low-frequency dataThe Journal of the Acoustical Society of America, 1989
- Quantitative backscatter measurements with a long-range side-scan sonarIEEE Journal of Oceanic Engineering, 1989
- Measurement of sound absorption and sound speed in terrigeneous sedimentsThe Journal of the Acoustical Society of America, 1987
- Application of the composite roughness model to high-frequency bottom backscatteringThe Journal of the Acoustical Society of America, 1986
- Geoacoustic modeling of the sea floorThe Journal of the Acoustical Society of America, 1980
- Near-bottom seismic profiling: High lateral variability, anomalous amplitudes, and estimates of attenuationThe Journal of the Acoustical Society of America, 1980
- A near-bottom geophysical traverse of the Reykjanes RidgeEarth and Planetary Science Letters, 1978
- Sound Speed and Attenuation, from 15 to 1500 kHz, Measured in Natural Sea-Floor SedimentsThe Journal of the Acoustical Society of America, 1968