Physics
Scientific paper
Jul 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30m..15c&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 13, pp. 15-1, CiteID 1682, DOI 10.1029/2002GL016330
Physics
19
Seismology: Body Wave Propagation, Mineralogy And Petrology: General Or Miscellaneous, Seismology: Core And Mantle, Tectonophysics: Dynamics Of Lithosphere And Mantle-General, Tectonophysics: Earth'S Interior-Composition And State (1212)
Scientific paper
We demonstrate a rare, unequivocal case of anisotropy in the transition zone (TZ), evident from many horizontal-polarized shear-waves (SH) that arrive up to 3 s earlier than vertical-polarized shear-waves (SV). The anisotropic region correlates with deep earthquakes away from the active subduction zone and known boundaries of lateral heterogeneities in compression- and shear-wave speeds. We interpret the anisotropy as strong fabric associated with a large petrologic anomaly in the core of remnant lithosphere which is buoyant and stagnates in the TZ. Fast subduction of cold slab actually favors such a configuration, so slab penetration into the lower mantle does not uniformly occur.
Brudzinski Michael R.
Chen Wang-Ping
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