Titlebook: Geodynamics of Lithosphere & Earth’s Mantle; Seismic Anisotropy a Jaroslava Plomerová,Robert C. Liebermann,Vladislav Conference proceedings

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Passive Seismology and Deep Structure in Central Italyf the depth and geometry of the Moho through the receiver function technique is in progress. Tomographic results from the northernmost 1994 and the central 1995 teleseismic experiments confirm that a high-velocity anomaly (HVA) does exist in the upper 200–250 km and is confined to the northern Apenn

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New Perspectives on Mantle Dynamics from High-resolution Seismic Tomographic Model P1200r degrees exceeding around 10, the spectra at various depths decay with a power-law like dependence on the degree, with the logarithmic slopes in the asymptotic portion of the spectra containing values between 2 and 2.6. These spectral results may suggest the time-dependent nature of mantle convecti

hypnogram

Regional Correlation Analysis between Seismic Heterogeneity in the Lower Mantle and Subduction in thion and in the mid-mantle for subduction younger than 120 Myr. An increase in the correlation close to the core-mantle boundary nevertheless indicates that, under certain circumstances, the slabs can reach the bottom of the mantle in the West Pacific and in the Alpine-Himalayan regions as well. The

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https://doi.org/10.1007/978-3-662-28967-9rface and those extending deep into the interior of the Earth. Seismic anisotropy provides some of the most diagnostic evidence for mapping past and present deformation of the entire crust-mantle system.

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