Affiliation:
1. School of Earth and Environmental Sciences Seoul National University Seoul Republic of Korea
2. Lamont‐Doherty Earth Observatory of Columbia University New York NY USA
3. Earthquake Research Center Korea Institute of Geoscience and Mineral Resources Daejeon Republic of Korea
Abstract
AbstractWe used local P and S waves, and regional Lg waves to investigate the Mw 4.9 Offshore Jeju Island earthquake, whose records show evidence of a complex rupture. This earthquake provides a rare window to understand the seismogenesis of moderate‐sized earthquakes on the southern Korea–East China Sea continental shelf. We computed the relative source time functions (RSTFs) by aligning the signals on the origin time of the main and its empirical Green's function (EGF) events, allowing us to use them as differential times of the EGF pair. We determined subevent locations using direct‐wave RSTFs, and captured the rupture variability of the two large subevents using waveform inversion of stacked Lg‐wave RSTFs. The first subevent rupture started by two weak nucleation phases and propagated slowly and bilaterally. Then the second subevent ruptured westward. Our analysis demonstrates that the Lg‐wave train observed at regional distances is useful in investigating detailed slip history.
Funder
National Research Foundation of Korea
Publisher
American Geophysical Union (AGU)
Cited by
1 articles.
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