Radial and azimuthal anisotropy in seismicwave speeds have long been observed using surface waves and are believed to be controlled by deformation within the Earth’s crust and uppermost mantle. Although radial and azimuthal anisotropy reflect important aspects of anisotropic media, few studies have tried to interpret them jointly. We describe a method of inversion that interprets simultaneous…

Tahun Terbit

1990

No. Panggil

330.01 PAR p