Structure and heterogeneity of the Earth's mantle from broadband earthquake seismology
Attenuation of seismic energy is often seen as an unavoidable 'problem' in earthquake seismology. Observation of earthquakes at teleseismic distances is severely limited by the signal-to-noise ratio of the recording seismograph. However, the underlying mechanisms behind seismic attenuation...
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University of Edinburgh
1995
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.661812 |