Passive- and active-source seismological studies of northern Scotland and the South Caspian Basin indicate: (1) pervasive and laterally heterogeneous velocity discontinuities within the upper mantle influenced by the localized tectonic and thermal history of northwest Scotland, …
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Seismological waveform data recorded by networks in Spain and Morocco are used to study seismicity and to image the velocity and attenuation structure of the lithosphere and upper mantle beneath the Africa-Iberia plate boundary zone using tomographic methods. An Mw = 6.0 earthqu…