Temperature is one of the key parameters controlling lithospheric and mantle dynamics and
rheology. Using recent experimental data on elastic parameters and anelasticity, we obtain …

The upper mantle low velocity zone (LVZ) is a depth interval with slightly reduced seismic
velocity compared to the surrounding depth intervals. The zone is present below a relatively …

Since 1969, seismology has been extended beyond the Earth, and seismic sensors have
been placed on the surface of other bodies of the solar system. A Lunar seismic network …

A geometrical attenuation model is proposed as an alternative to the conventional frequency-
dependent attenuation law Q (f)= Q 0 (f/f 0) η. The new model provides a straightforward …

Seismic scattering in the deep Earth below the mantle transition zone is observed from
precursors and codas to a number of body‐wave arrivals, including P, P diff, PKP, PKiKP …

We present new data sets of P and S arrival times which have been handpicked from long‐
period vertical and transverse component recordings of the various global seismic networks …

Displacement and velocity records of P and SH body waves with broadband frequency
content from 0.01 to 5.0 Hz are obtained either directly or through multichannel …

We have generalized the methodology of our regional amplitude tomography from the Lg
phase to the four primary regional phases (Pn, Pg, Sn, Lg). Differences in the geometrical …

We present a new velocity model for the continental upper mantle beneath central Siberia
based on observations of the 1982 'RIFT'Deep Seismic Sounding (DSS) profile. Three …

We present the results of an analysis of global lateral variations in anelasticity of the upper
mantle, as measured from very long period Rayleigh waves observed on the GEOSCOPE …