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AGU: Geophysical Research Letters

 

Keywords

  • deep fault slip
  • low-frequency earthquake
  • triggered tremor

Index Terms

  • Seismology: Earthquake source observations
  • Seismology: Body waves

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 37, L16307, 6 PP., 2010
doi:10.1029/2010GL043918

Detecting low-frequency earthquakes within non-volcanic tremor in southern Taiwan triggered by the 2005 Mw8.6 Nias earthquake

Chi-Chia Tang

Institute of Seismology, National Chung Cheng University, Min-Hsiung, Taiwan

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

Zhigang Peng

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

Kevin Chao

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

Chau-Huei Chen

Institute of Seismology, National Chung Cheng University, Min-Hsiung, Taiwan

Cheng-Horng Lin

Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan

We use a matched filter technique to detect 41 low-frequency earthquakes (LFEs) within 700-s of triggered tremor signals in the Southern Central Range in Taiwan during the surface waves of the 2005 Mw8.6 Nias earthquake off the coast of northern Sumatra. The depth distributions of LFEs after double-difference relocations concentrate at the depth range of 12–38 km below the background seismicity and above the Moho depth inferred from receiver function studies. The locations of LFEs are close to the downward extension of the steep-dipping Chaochou-Lishan fault with only modestly high Vp/Vs ratios (1.75–1.85). Our observation indicates that at least portions of triggered tremor consists of many LFEs, similar to ambient tremor observed at other major plate boundary faults.

Received 17 May 2010; accepted 30 June 2010; published 25 August 2010.

Citation: Tang, C.-C., Z. Peng, K. Chao, C.-H. Chen, and C.-H. Lin (2010), Detecting low-frequency earthquakes within non-volcanic tremor in southern Taiwan triggered by the 2005 Mw8.6 Nias earthquake, Geophys. Res. Lett., 37, L16307, doi:10.1029/2010GL043918.

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