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- W1644291330 abstract "Models of the Earth’s long period three dimensional structure have been obtained from the study of the splitting of Earth’s free oscillation spectra. These data place important constraints on the aspherical compressional and shear wave velocity structure, and in addition have the capability to provide information on aspherical density structure. In general, splitting functions are measured from the normal mode spectra using a least squares inversion. These splitting functions are linearly dependent upon the aspherical velocity and density structure and are then used in a second least squares inversion to obtain tomographic velocity models. Many recent tomographic models, including S20RTS, have used splitting functions in addition to body wave and surface wave data. In principle, normal mode spectra can also be inverted directly to get tomographic models." @default.
- W1644291330 created "2016-06-24" @default.
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- W1644291330 date "2003-12-01" @default.
- W1644291330 modified "2023-09-24" @default.
- W1644291330 title "Long-period mantle structure from Earth's free oscillation spectra" @default.
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