Abstract
The geophysicist uses mathematics to formulate the physical precepts involved in the transmission of sound as applied to high-resolution geophysical (HRG) surveys. The purpose of the following paragraphs is to expose the nongeophysicist to a few of those principles. Standard textbooks on the subjects of geophysics (1, 2), acoustics (3), or optics should be consulted for greater detail and the mathematical derivations.
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References
Dobrin, M. B., 1976, Introduction to geophysical prospecting: 3rd ed., New York, McGraw-Hill.
Grant, F. S. and G. F. West, 1965, Interpretation theory in applied geophysics: New York, McGraw-Hill.
Urick, R. J., 1967, Principles of underwater sound: 3rd ed., New York, McGraw-Hill, 342 p.
Bachman, R. T., 1983, Elastic anisotropy in marine sedimentary rocks: J. Geophys. Res., v. 88, no. B1, p. 539–545.
Del Grosso, V. A., 1974, New equation for the speed of sound in natural waters: J. Acoust. Soc, v. 56, p. 1084.
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© 1984 Springer Science+Business Media Dordrecht
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Trabant, P.K. (1984). Marine Geophysics: An Overview. In: Applied High-Resolution Geophysical Methods. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-6493-8_2
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DOI: https://doi.org/10.1007/978-94-009-6493-8_2
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