Titlebook: Scattering and Attenuations of Seismic Waves, Part I; Keiiti Aki,Ru-Shan Wu Book 1988 Springer Basel AG 1988 Manuscript.modeling.numerical

表状态

https://doi.org/10.1007/978-3-0348-7722-0Manuscript; modeling; numerical method

JOG

我悲伤

Scattering and Attenuations of Seismic Waves, Part I978-3-0348-7722-0Series ISSN 2504-3625 Series E-ISSN 2504-3633

文艺

酷热

Introduction: Seismic Wave Scattering in Three-dimensionally Heterogeneous Earth,eneous everywhere from the crust, mantle to the core with scale from the grain size of rocks to the lowest orders of global spherical harmonics. Figure 1 shows the strength and scale length of heterogeneities in the crust and mantle of the earth, in terms of v, the perturbation index of seismic (. o

habitat

Synthesis of Coda Waves in Layered Medium,atterers in a layered medium. The scattered waveform itself is generated and examined instead of its energy envelope. The theory used allows 1) mode conversion, 2) wave type conversion, 3) finite scatterer distribution, and 4) the effect of attenuation from scattering as well as intrinsic absorption

tic-douloureux

Is the Single Scattering Model Invalid for the Coda Excitation at Long Lapse Time?, made the dimensional analysis for the temporal decay of the multiple scattering energy density at the hypocenter. The number of scatterers in a sphere of radius . is assumed to be proportional to ... Then, the energy density of the . th order scattering decays according to the [(. — 2). — 3]th powe

Conflagration

俗艳

endure