"The alignment of olivine crystals is considered as the dominant source of seismic anisotropy in the subcrustal lithosphere and asthenosphere. Different components of large-scale anisotropy can be traced in depth distributions of the radial and azimuthal anisotropy of surface waves." . . . "Mapping the lithosphere-asthenosphere boundary through changes in surface-wave anisotropy."@en . "0040-1951" . "3"^^ . . "3"^^ . "Mapping the lithosphere-asthenosphere boundary through changes in surface-wave anisotropy." . "Babu\u0161ka, Vladislav" . . . "0"^^ . . "175;185" . "0"^^ . "358" . "RIV/67985530:_____/02:03020025!RIV/2003/AV0/A03003/N" . "NL - Nizozemsko" . "P(IAA3012908), Z(AV0Z3012916)" . . . . "RIV/67985530:_____/02:03020025" . . "The alignment of olivine crystals is considered as the dominant source of seismic anisotropy in the subcrustal lithosphere and asthenosphere. Different components of large-scale anisotropy can be traced in depth distributions of the radial and azimuthal anisotropy of surface waves."@en . "1/4" . "11"^^ . . . . "Tectonophysics" . . "Kouba, Daniel" . . "Plomerov\u00E1, Jaroslava" . "Mapping the lithosphere-asthenosphere boundary through changes in surface-wave anisotropy." . "652457" . "lithosphere-asthenosphere boundary; surface waves; radial polarisation; azimuthal anisotropy"@en . . . . "Mapping the lithosphere-asthenosphere boundary through changes in surface-wave anisotropy."@en . . "[C1E9162DDDA0]" . .