A shallow double seismic zone beneath the central New Hebrides (Vanuatu): evidence for fragmentation and accretion of the descending plate?-Reference-Cited by-同舟云学术

A shallow double seismic zone beneath the central New Hebrides (Vanuatu): evidence for fragmentation and accretion of the descending plate?

Published:1994-09-15 Issue:19 Volume:21 Page:2159-2162
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Prévot Richard,Chatelain J-L.,Roecker S. W.,Grasso J-R.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/v021/i019/94GL01961/94GL01961.pdf

Reference19 articles.

1. Patterns of seismicity associated with asperities in the central New Hebrides islands arc;Chatelain;J. Geophys. Res.,1986

2. Detachment of part of the downgoing slab and uplift of the New Hebrides (Vanuatu) islands;Chatelain;Geophys. Res. Lett.,1992

3. Unfolding the subducting plate in the central New Hebrides island arc: geometrical argument for detachment of part of the downgoing slab;Chatelain;Geophys. Res. Lett.,1993

4. Shear velociry fom differential travel times of short period ScS-P in New Hebrides, Fiji-Tonga, and Banda Sea regions;Choudhury;Bull. Seis. Soc. Am.,1975

5. Recent tectonics associated with the subduction/ collision of the D'Entrecasteaux zone in the central New Hebrides;Collot;Tectonophysics,1985

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