Anorogenic intra-plate magmatism was widespread in Europe from early Tertiary to Recent
times, extending west to east from Spain to Bulgaria, and south to north from Sicily to central …

Recent progress in numerical methods and computer science allows us today to simulate
the propagation of seismic waves through realistically heterogeneous Earth models with …

We present a new global model for the Earth's crust based on seismic refraction data
published in the period 1948–1995 and a detailed compilation of ice and sediment …

In global-scale seismic tomography, teleseismic P and PP waves mainly constrain structures
in the upper two thirds of the mantle, whereas core-diffracted waves (Pdiff) constrain the …

We study the upper mantle P wave velocity structure below the Euro‐Mediterranean area,
down to 1000 km depth, by seismic travel time tomography. We invert summary residuals …

We present a full seismic waveform tomography for upper-mantle structure in the
Australasian region. Our method is based on spectral-element simulations of seismic wave …

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 …

This paper presents the results of a study of the dispersion characteristics of broadband
fundamental surface waves propagating across Eurasia. The study is broader band …

Images of the European crust and upper mantle, created using seismic tomography, identify
the Cenozoic Rift System and related volcanism in central and western Europe. They also …

Seismic velocity heterogeneity in the Earth's mantle is strongly concentrated near its top. The
shallow heterogeneity of the mantle correlates strongly with surface tectonics. We use these …