ADVANCES IN GEOPHYSICS docx

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ADVANCES IN GEOPHYSICS docx

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[...]... COUPLING ALONG ALASKA-ALEUTIANS 15 recorded trace water intake L FIG.6 Sketch of a stilling-well tide gauge The stilling-well gauge consists of a well with a water intake and a float that is attached to a recording system As the water level in a bay or harbor increases or decreases, the float in the stilling well rises or falls This motion is recorded on a paper record as a continuous trace Each recording...This Page Intentionally Left Blank ADVANCES IN GEOPHYSICS VOL 39 HETEROGENEOUS COUPLING ALONG ALASKA-ALEUTIANS AS INFERRED FROM TSUNAMI, SEISMIC, AND GEODETIC INVERSIONS JEAN M JOHNSON Division of Natural Sciences Shorter College Rome, Georgia 1 INTRODUCTION The Alaskan-Aleutian arc has a history of rupturing in large and great earthquakes The most recent sequence began in 1938 and has ruptured... 1)sinC)+ Q, .

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  • Advances in Geophysics, Volume 39

  • Copyright Page

  • Contents

  • Contributors

  • Chapter 1. Heterogeneous Coupling along Alaska-Aleutians as Inferred from Tsunami, Seismic, and Geodetic Inversions

    • 1. Introduction

    • 2. Generation, Computation, and Inversion of Tsunami Waveforms

    • 3. The 1965 Rat Islands Earthquake: A Critical Comparison of Seismic and Tsunami Wave Inversions

    • 4. The 1957 Great Aleutian Earthquake

    • 5. Rupture Extent of the 1938 Alaskan Earthquake as Inferred from Tsunami Waveforms

    • 6. Estimation of Seismic Moment and Slip Distribution of the 1 April 1946 Aleutian Tsunami Earthquake

    • 7. The 1964 Prince William Sound Earthquake: Joint Inversion of Tsunami and Geodetic Data

    • 8. Conclusions

    • Appendix: Notes on the Tsunami Waveform Inversion Method

    • References

    • Chapter 2. Local Tsunamis and Earthquake Source Parameters

      • 1. Introduction

      • 2. Tsunami Theory

      • 3. Local versus Far-Field Tsunamis

      • 4. Tectonic Setting of Tsunamigenic Earthquakes

      • 5. Effect of Static Source Parameters on Tsunamis

      • 6. Effect of Spatial Variations in Earthquake Source Parameters

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