Imaging the Hikurangi subduction zone, New Zealand, using teleseismic receiver functions: crustal fluids above the forearc mantle wedge
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/169/2/602/5906676/169-2-602.pdf
Reference73 articles.
1. The thermal structure of subduction zones constrained by seismic imaging: implications for slab dehydration and wedge flow;Abers;Earth planet. Sci. Lett.,2006
2. The isolation of receiver effects from teleseismic P waveforms;Ammon;Bull. seism. Soc. Am.,1991
3. On the nonuniqueness of receiver function inversions;Ammon;J. geophys. Res.,1990
4. Shallow morphology of the subducted Pacific plate along the Hikurangi margin, New Zealand;Ansell;Phys. Earth planet. Inter.,1996
5. Anomalous high-frequency wave propagation from the Tonga-Kermadec seismic zone to New Zealand;Ansell;Geophys. J. R. astr. Soc.,1986
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