Crustal stress field perturbations in the continental margin around the Korean Peninsula and Japanese islands

Junhyung Lee, Tae-Kyung Hong, Chandong Chang

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

Seismic activity and focal mechanisms are governed by the effective stress field that is a combined result of regional tectonic processes and local stress perturbation. This study investigates the regional variation in the stress field in the eastern continental margin of the Eurasian plate around the Korean Peninsula and Japanese islands using a damped stress inversion technique based on the focal mechanism solutions of regional earthquakes. The dominant compressional stress is directed ENE–WSW around the Korean Peninsula and eastern China, E–W at the central East Sea and northern and southern Japan, NW–SE at central Japan, and N–S around the northern Nankai trough. The dominant compression direction changes rapidly in the East Sea and Japanese islands, which may be due to the combined effects of tectonic loading in the subduction zones off the Japanese islands and the India-Eurasia plate boundary. The crustal stress fields around the subduction zones off the Japanese islands present characteristic depth-dependent orientations. The orientations of the largest horizontal stress components, σH, in the subduction zones are subparallel with the plate convergence directions at shallow depths. The σH orientations are observed to rotate clockwise with the depth owing to slab subduction and lithospheric deformation. The regional stress field around the Japanese islands was perturbed temporally by the 2011 M9.0 Tohoku-Oki megathrust earthquake. The regional stress field was recovered in a couple of years. The stress field and tectonic structures are mutually affected, causing stress field distortion and a localized mixture of earthquakes in different faulting types.

Original languageEnglish
Pages (from-to)140-149
Number of pages10
JournalTectonophysics
Volume718
DOIs
Publication statusPublished - 2017 Oct 30

Fingerprint

peninsulas
continental shelves
stress field
stress distribution
continental margin
perturbation
subduction zone
tectonics
earthquakes
Eurasian plate
focal mechanism
earthquake
Japan
plate convergence
tectonic structure
effective stress
plate boundary
India
troughs
China

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth-Surface Processes

Cite this

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abstract = "Seismic activity and focal mechanisms are governed by the effective stress field that is a combined result of regional tectonic processes and local stress perturbation. This study investigates the regional variation in the stress field in the eastern continental margin of the Eurasian plate around the Korean Peninsula and Japanese islands using a damped stress inversion technique based on the focal mechanism solutions of regional earthquakes. The dominant compressional stress is directed ENE–WSW around the Korean Peninsula and eastern China, E–W at the central East Sea and northern and southern Japan, NW–SE at central Japan, and N–S around the northern Nankai trough. The dominant compression direction changes rapidly in the East Sea and Japanese islands, which may be due to the combined effects of tectonic loading in the subduction zones off the Japanese islands and the India-Eurasia plate boundary. The crustal stress fields around the subduction zones off the Japanese islands present characteristic depth-dependent orientations. The orientations of the largest horizontal stress components, σH, in the subduction zones are subparallel with the plate convergence directions at shallow depths. The σH orientations are observed to rotate clockwise with the depth owing to slab subduction and lithospheric deformation. The regional stress field around the Japanese islands was perturbed temporally by the 2011 M9.0 Tohoku-Oki megathrust earthquake. The regional stress field was recovered in a couple of years. The stress field and tectonic structures are mutually affected, causing stress field distortion and a localized mixture of earthquakes in different faulting types.",
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Crustal stress field perturbations in the continental margin around the Korean Peninsula and Japanese islands. / Lee, Junhyung; Hong, Tae-Kyung; Chang, Chandong.

In: Tectonophysics, Vol. 718, 30.10.2017, p. 140-149.

Research output: Contribution to journalArticle

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