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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

  1. Dobrin, M. B., 1976, Introduction to geophysical prospecting: 3rd ed., New York, McGraw-Hill.

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  2. Grant, F. S. and G. F. West, 1965, Interpretation theory in applied geophysics: New York, McGraw-Hill.

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  3. Urick, R. J., 1967, Principles of underwater sound: 3rd ed., New York, McGraw-Hill, 342 p.

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  4. Bachman, R. T., 1983, Elastic anisotropy in marine sedimentary rocks: J. Geophys. Res., v. 88, no. B1, p. 539–545.

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  5. 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

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-009-6495-2

  • Online ISBN: 978-94-009-6493-8

  • eBook Packages: Springer Book Archive

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