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Showing 81-100 of 118 results
  1. A Fast Simulated Annealing Algorithm for the Inversion of Marine Sediment Seismo-Acoustic Parameters

    Nonlinear seismo-acoustic inversion is performed using a fast simulated annealing algorithm A high-resolution cost function and the matched-field...
    W. A. Kuperman, M. D. Collins, H. Schmidt in Shear Waves in Marine Sediments
    Chapter 1991
  2. Very low frequency Ocean Bottom ambient seismic noise and coupling on the shallow continental shelf

    Sources of very low frequency (0.01 to 1.0 Hz) ambient seismic noise in the shallow (<100 m) water continental margin sediments are investigated...

    Mark V. Trevorrow, Tokuo Yamamoto, ... Mohsen Badiey in Marine Geophysical Researches
    Article 01 June 1989
  3. Seismic diffraction

    Durk J. Doornbos in Geophysics
    Reference work entry 1989
  4. Seismic energy partitioning and scattering in laterally heterogeneous ocean crust

    We present finite difference forward models of elastic wave propagation through laterally heterogeneous upper oceanic crust. The finite difference...

    Martin E. Dougherty, Ralph A. Stephen in pure and applied geophysics
    Article 01 March 1988
  5. Book review

    Richard H. Sibson, Emile A. Okal, ... Antonio Navarra in pure and applied geophysics
    Article 01 March 1988
  6. On the validity of the ray approximation for interpreting delay times

    This chapter deals with the influence of diffracted waves on tomographic observations. Probably most workers in tomography are aware of the existence...
    E. Wielandt in Seismic Tomography
    Chapter 1987
  7. Shear Properties of Ocean Sediments Determined from Numerical Modelling of Scholte Wave Data

    Recently it has become apparent that shear properties of ocean sediments are most easily determined from measured propagation characteristics of...
    Finn B. Jensen, Henrik Schmidt in Ocean Seismo-Acoustics
    Chapter 1986
  8. On the Role of Bottom Interface Waves in Ocean Seismo-Acoustics: A Review

    Ocean bottom interface waves of the Scholte type (sometimes also called oceanic Rayleigh or Stoneley waves) are guided by the acoustically most...
    Dieter Rauch in Ocean Seismo-Acoustics
    Chapter 1986
  9. The Use of Love Waves to Determine the Geoacoustic Properties of Marine Sediments

    The importance of the geoacoustic properties of marine sediments for low-frequency shallow water propagation is well established. Reliable...
    T. Akal, H. Schmidt, P. Curzi in Ocean Seismo-Acoustics
    Chapter 1986
  10. Observations of Interface Waves and Low-Frequency Acoustic Propagation Over a Rough Granite Seabed

    Experimental measurements of hydrophone signals from explosive sources in shallow water over a rough granite seabed have revealed several interesting...
    Philip R. Staal, David M. F. Chapman in Ocean Seismo-Acoustics
    Chapter 1986
  11. A Comparison of Seismic and Hydroacoustic Measurements at Very Low Frequencies in Different Shallow Water Areas

    Numerous sea-trials concerning the detection and propagation of very low frequency sound (2 to 24 Hz) have been conducted by SACLANTCEN, mostly in...
    B. Schmalfeldt in Ocean Seismo-Acoustics
    Chapter 1986
  12. Interface Wave Studies on the Ligurian Shelf Using an OBS Array: Experimental Results and Propagation Models

    Seismic waves travelling in the water/sediment or subbottom sediment/sediment interface have been the subject of considerable interest in recent...
    Michael Snoek, Guido Guidi, Enzo Michelozzi in Ocean Seismo-Acoustics
    Chapter 1986
  13. A Propagation Anomaly Observed in the Barents Sea

    A low frequency sound propagation experiment was conducted in the Western Barents Sea from a towed continuous sound source and air-dropped explosive...
    E. H. Hug in Ocean Seismo-Acoustics
    Chapter 1986
  14. Characterization of Average Geoacoustic Bottom Properties from Expected Propagation Behavior at Very Low Frequencies (VLF) Using a Towed Array Simulation

    The purpose of this study is to determine the feasibility of broad georeconnaissance data acquisition for average bottom properties collected via a...
    M. F. Werby, G. J. Tango in Ocean Seismo-Acoustics
    Chapter 1986
  15. Ocean Bottom Seismology: History and Current Status

    Ocean bottom seismographs (OBS) have been in use for almost 50 years. The earliest instruments were used for short range explosion refraction...
    George H. Sutton in Ocean Seismo-Acoustics
    Chapter 1986
  16. Energy Fluxes at the Earth’s Surface

    Evaporation and sensible heat flux into the atmosphere require the availability of some form of energy at the earth-atmosphere interface. This...
    Wilfried Brutsaert in Evaporation into the Atmosphere
    Chapter 1982
  17. Atmospheric and Water Waves and Companion Seismic Phenomena

    Elastic waves, traveling in the solid body of the earth, sometimes convert part of their energy to other waves that propagate in the water or in the...
    Ari Ben-Menahem, Sarva Jit Singh in Seismic Waves and Sources
    Chapter 1981
  18. Surface-Wave Amplitude Theory

    In Section 3.6, we demonstrated the existence of Rayleigh waves in a homogeneous half-space and Love waves in a two-layered half-space. We also...
    Ari Ben-Menahem, Sarva Jit Singh in Seismic Waves and Sources
    Chapter 1981
  19. Asymptotic Theory of the Earth’s Normal Modes

    We have seen that the complete seismic field induced in a radially heterogeneous sphere can be expressed as an infinite sum of standing waves, namely...
    Ari Ben-Menahem, Sarva Jit Singh in Seismic Waves and Sources
    Chapter 1981
  20. The interaction of elastic waves with a solid-liquid interface, with applications to the core-mantle boundary

    The paper discusses basic ideas and principles underlying methods, which have proved useful in the interpretation of diffraction and scattering...

    D. J. Doornbos, J. C. Mondt in pure and applied geophysics
    Article 01 September 1980
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