Shear velocity structure in the Aegean area obtained by inversion of Rayleigh waves-Reference-Cited by-同舟云学术

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Shear velocity structure in the Aegean area obtained by inversion of Rayleigh waves

Published:2004-12-21 Issue:1 Volume:160 Page:127-143
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Karagianni E. E.,Papazachos C. B.,Panagiotopoulos D. G.,Suhadolc P.,Vuan A.,Panza G. F.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/160/1/127/5920469/160-1-127.pdf

Reference97 articles.

1. Active tectonics of the Adriatic Region;Anderson;Geophys. J. R. astr. Soc.,1987

2. The resolving power of gross Earth data;Backus;Geophys. J. R. astr. Soc.,1968

3. The relationship between seismic velocity and density in the continental crust-a useful constraint?;Barton;Geophys. J. R. astr. Soc.,1986

4. Birch , F. 1969 Density and Composition of the Upper Mantle: First Approximation as an Olivine Layer, in the Earth's Crust and Upper Mantle 18 36 10.1029/96JB03730

5. The structure of the upper mantle under the United States from the dispersion of Rayleigh waves;Biswas;Geophys. J. R. astr. Soc.,1974

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