Shear wave attenuation structure and anisotropy in the Hikurangi subduction zone, central North Island, New Zealand
The seismic attenuation structure of a subduction zone can constrain variations in temperature, composition and fluids. Amplitude spectra of 2206 local earthquakes, recorded by a dense network of 116 seismic stations in central North Island (NI), New Zealand, are modelled to image the three-dimensio...
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University of Leeds
2009
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Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.507045 |