Elastogravity Waves and Dynamic Ground Motions in the Korean Peninsula Generated by the March 11, 2011 MW9.0 Tohoku-Oki Megathrust Earthquake

Tae Kyung Hong, Ilgoo Kim, Seongjun Park, Dongwoo Kil

Research output: Contribution to journalArticlepeer-review

Abstract

The mass dislocations caused by large coseismic slips in megathrust earthquakes are large enough to produce elastogravity waves. Despite, successful identification of elastogravity-wave development during megathrust earthquakes, the nature of ground motions and hazard potentials in regional and teleseismic distances remains unknown. The dynamic ground motions from the March 11, 2011 MW9.0 Tohoku-Oki megathrust earthquake are retrieved from broadband seismic records throughout the Korean Peninsula. The dynamic ground motions of the megathrust earthquake are dominated by low-frequency (<0.1 Hz) energy that is a mixture of elastogravity waves and seismic waves. The peak dynamic ground displacements in the Korean Peninsula reached ∼20 cm with horizontal permanent displacements of ∼2 cm or more. Radially-polarized elastogravity waves developed instantly at the event origin time. Very-long-period (<0.004 Hz) energy is a mixture of seismic waves and coseismic permanent displacements, presenting radially polarized retrograde particle motions for ∼600 s. The peak ground displacements (PGDs) and velocities for the Tohoku-Oki earthquake are larger than those for a local MW5.4 earthquake. The peak ground motions vary azimuthally following the source radiation pattern. The tangential PGD increases with distance along continental ray paths due to the development of crustally guided waves. Large and slow dynamic ground motions cause dynamic stress changes of ∼1.8 MPa in the lithosphere of the Korean Peninsula, while the properties of the mantle are scarcely affected by slow dynamic motions. The large long-period displacements induced by megathrust earthquakes may cause considerable long-duration distortion on large buildings at regional and teleseismic distances. The characteristic elastogravity-wave features may be used for detection of mass-dislocation events.

Original languageEnglish
Article numbere2020JB020628
JournalJournal of Geophysical Research: Solid Earth
Volume126
Issue number2
DOIs
Publication statusPublished - 2021 Feb

Bibliographical note

Funding Information:
The authors thank Dr Rachel Abercrombie (editor), associate editor, Dr Iris van Zelst (reviewer), and two anonymous reviewers for fruitful review comments to improve the presentation of the manuscript. This work was supported by the Korea Meteorological Administration Research and Development Program under grant KMI2018‐02910. Additionally, this research was partly supported by the Basic Science Research Program of National Research Foundation of Korea (NRF‐2017R1A6A1A07015374 and NRF‐2018R1D1A1A09083446).

Publisher Copyright:
© 2021. The Authors.

All Science Journal Classification (ASJC) codes

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

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