Theory of Seismic Head Waves /
Head waves - also called refraction arrivals, lateral waves, or conical waves - have been used extensively in near-earthquake studies, geophysical prospecting, and deep-crustal seismological investigations. In the past, research was confined largely to the kinematic characteristics of the waves, but...
Autores principales: | , |
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Formato: | Electrónico eBook |
Idioma: | Inglés |
Publicado: |
Toronto :
University of Toronto Press,
[2017]
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Colección: | Heritage
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Temas: | |
Acceso en línea: | Texto completo Texto completo |
Tabla de Contenidos:
- Frontmatter
- CONTENTS
- PREFACE
- LIST OF IMPORTANT SYMBOLS
- 1. INTRODUCTION
- 2. THE RAY METHOD
- 3. HEAD WAVES FROM A SINGLE INTERFACE
- 4. HEAD WAVES IN MULTILAYERED MEDIA
- 5. CURVED AND DIPPING INTERFACES IN THE OVERBURDEN
- 6. INTERFERENCE HEAD WAVES
- 7. HEAD WAVES BY WAVE METHODS
- APPENDIX : Some useful vector identities
- REFERENCE
- INDEX