A two‐dimensional algorithm to determine the steady state thermal structure of the
lithosphere that integrates thermal, gravity, and local isostasy analyses is presented. Gravity …

Surface wave data were initially collected from events of magnitude Ms≥ 5.0 and shallow or
moderate focal depth occurred between 1980 and 2002: 713 of them generated Rayleigh …

We have obtained high resolution group velocity maps of Rayleigh waves at periods from 8
to 25 seconds across the Iberian Peninsula by cross‐correlating four months of ambient …

Relative SV and SH wave speeds are generally attributed to radial seismic anisotropy which
can be used as the indicator of crust/mantle deformation styles. Surface wave data were …

We conducted a tomographic inversion of Rayleigh‐wave dispersion to obtain 2D phase
and group velocity tomographic images in the 10–100 s period range and shear‐wave …

A joint inversion of regionalized phase and group velocities of fundamental mode Rayleigh
waves is performed by means of a simulated annealing scheme which makes use of some …

An MT profile which roughly coincides with the south side of the ECORS-Pyrenees deep
reflection seismic profile was made from the North Pyrenean zone through the central …

Seismic surface waves exhibit much more complicated wavefields than is commonly
assumed. We are led to this conclusion after analysing 90 teleseismic events recorded at on …

The earthquake of 24 June, 1984, with epicenter in the Granada Basin (36.86° N, 3.76° W;
H= 12 km; mb= 4.9), was the first event to produce accelerograms in Spain. It was recorded …

The lithospheric structure of the Sinai Peninsula is shown by means of nine shear velocity
profiles for depths ranging from zero to 50 km, determined from the Rayleigh wave analysis …