Metamorphic controls on seismic velocity of subducted oceanic crust at 100–250 km depth

Author:

Connolly J.A.D.,Kerrick D.M.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Deep seismic zone as an upper mantle reflector of body waves;Fukao;Nature,1978

2. Seismological constraints on the gabbro-eclogite transition in subducted oceanic crust;Gubbins;Earth Planet. Sci. Lett.,1994

3. Estimation of the thickness of the low velocity layer at the surface of the descending oceanic plate beneath the Northeastern Japan arc by using synthesized PS-wave;Matsuzawa;Tohoku Geophys. J.,1987

4. Study of the structure of the slab-mantle interface using reflected and converted seismic waves;Helffrich;Geophys. J. Int.,1993

5. Dispersion of regional body waves at 100–150 km depth beneath Alaska: in situ constraints on metamorphism in the subducted crust;Abers;Geophys. Res. Lett.,1996

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