Thickness of the Crust along the Irkutsk-Uian-Bator-Undershill Profile from Spectral Ratios of Body Seismic Waves
The thickness of the crust is estimated from the frequency intervals between the maxima of spectral ratios of body waves. This method was applied to processing data obtained at 15 observation sites by using digital seismic stations located along the Irkutsk-Ulan-Bator-Undurshill profile. The results obtained are consistent with the previous estimates from correlation of deep seismic sounding (DSS) data for southeastern Siberia with effective heights of topographic relief.
V. V. Mordvinova et al., "Thickness of the Crust along the Irkutsk-Uian-Bator-Undershill Profile from Spectral Ratios of Body Seismic Waves," Izvestiya Physics of the Solid Earth, vol. 31, no. 9, pp. 727-734, Maik Nauka-Interperiodica Publishing, Apr 1996.
Geosciences and Geological and Petroleum Engineering
International Standard Serial Number (ISSN)
Article - Journal
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