S-Pconversion from the transition zone beneath Tonga and the nature of the 670 km discontinuity-Reference-Cited by-同舟云学术

S-Pconversion from the transition zone beneath Tonga and the nature of the 670 km discontinuity

Published:1990-04 Issue:1 Volume:101 Page:1-35
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Richards Mark. A.,Wicks Charles W.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/101/1/1/2196679/101-1-1.pdf

Reference45 articles.

1. Thermally induced phase changes, lateral heterogeneity of the mantle, continental roots, and deep slab anomalies;Anderson;J. geophys. Res.,1987

2. The origin of complexity in some P seismograms from deep earthquakes;Barley;Geophys. J. R. astr. Soc.,1977

3. S to P scattering at the 650 km discontinuity;Barley;Geophys. J. R. astr. Soc.,1982

4. Billington, S. , 1980. The morphology and tectonics of the subducted lithosphere in the Tonga-Fiji-Kermadec region from seismicity and focal mechanism solutions, PhD thesis, Cornell University, Ithaca, New York.

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