| 11. | The two types of seismic body waves are compressional waves ( P-waves ) and shear waves ( S-waves ).
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| 12. | Recent models of global body waves used over 10 7 traveltimes to model 10 5 to 10 6 unknowns.
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| 13. | The accuracy of QMC depends strongly on the initial guess of many-body wave-functions and the form of the many-body wave-function.
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| 14. | Quantum Monte Carlo is a way to directly study the many-body problem and the many-body wave function beyond these approximations.
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| 15. | Two scales were developed, one based on surface waves, M _ s, and one on body waves, M _ b.
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| 16. | The accuracy of QMC depends strongly on the initial guess of many-body wave-functions and the form of the many-body wave-function.
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| 17. | Therefore, the body waves undergo less attenuation and reverberation than seismic waves from shallow earthquakes, resulting in sharp body wave peaks.
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| 18. | They usually travel slightly faster than Rayleigh waves, about 90 % of the body wave velocity, and have the largest amplitude.
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| 19. | Therefore, the body waves undergo less attenuation and reverberation than seismic waves from shallow earthquakes, resulting in sharp body wave peaks.
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| 20. | The shock had a body wave magnitude of 3.5 and a maximum Mercalli intensity of V ( " Moderate " ).
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