Depth-varying azimuthal anisotropy in the Tohoku subduction channel

Xin Liu, Dapeng Zhao

Research output: Contribution to journalArticlepeer-review

14 Citations (Scopus)

Abstract

We determine a detailed 3-D model of azimuthal anisotropy tomography of the Tohoku subduction zone from the Japan Trench outer-rise to the back-arc near the Japan Sea coast, using a large number of high-quality P and S wave arrival-time data of local earthquakes recorded by the dense seismic network on the Japan Islands. Depth-varying seismic azimuthal anisotropy is revealed in the Tohoku subduction channel. The shallow portion of the Tohoku megathrust zone (<30 km depth) generally exhibits trench-normal fast-velocity directions (FVDs) except for the source area of the 2011 Tohoku-oki earthquake (Mw 9.0) where the FVD is nearly trench-parallel, whereas the deeper portion of the megathrust zone (at depths of ∼30–50 km) mainly exhibits trench-parallel FVDs. Trench-normal FVDs are revealed in the mantle wedge beneath the volcanic front and the back-arc. The Pacific plate mainly exhibits trench-parallel FVDs, except for the top portion of the subducting Pacific slab where visible trench-normal FVDs are revealed. A qualitative tectonic model is proposed to interpret such anisotropic features, suggesting transposition of earlier fabrics in the oceanic lithosphere into subduction-induced new structures in the subduction channel.

Original languageEnglish
Pages (from-to)33-43
Number of pages11
JournalEarth and Planetary Science Letters
Volume473
DOIs
Publication statusPublished - 2017 Sep 1

Keywords

  • Tohoku
  • azimuthal anisotropy
  • megathrust earthquakes
  • subduction
  • tomography

ASJC Scopus subject areas

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

Fingerprint Dive into the research topics of 'Depth-varying azimuthal anisotropy in the Tohoku subduction channel'. Together they form a unique fingerprint.

Cite this