Abstract

The main goal of this study was to develop an updated and refined catalog of earthquakes in Taiwan (1900–2014) with homogenized M w magnitudes that are compatible with the Harvard M w . We hope that such a catalog of earthquakes will provide a fundamental database for definitive studies of the distribution of earthquakes in Taiwan as a function of space, time, and magnitude, as well as for realistic assessments of seismic hazards in Taiwan. In this study, for completeness and consistency, we start with a previously published catalog of earthquakes from 1900 to 2006 with homogenized M w magnitudes. We update the earthquake data through 2014 and supplement the database with 188 additional events for the time period of 1900–1935 that were found in the literature. The additional data resulted in a lower magnitude from M w 5.5–5.0. The broadband-based Harvard M w , United States Geological Survey (USGS) M, and Broadband Array in Taiwan for Seismology (BATS) M w are preferred in this study. Accordingly, we use empirical relationships with the Harvard M w to transform our old converted M w values to new converted M w values and to transform the original BATS M w values to converted BATS M w values. For individual events, the adopted M w is chosen in the following order: Harvard M w > USGS M > converted BATS M w > new converted M w . Finally, we discover that use of the adopted M w removes a data gap at magnitudes greater than or equal to 5.0 in the original catalog during 1985–1991. The new catalog is now complete for M w ≥ 5.0 and significantly improves the quality of data for definitive study of seismicity patterns, as well as for realistic assessment of seismic hazards in Taiwan.

Highlights

  • Taiwan is located at the juncture of the Philippine Sea plate on the east side and the Eurasian plate on the west side

  • We develop a catalog of Taiwan earthquakes with homogenized Mw magnitudes covering the time period of 1900–2006 (Chen and Tsai 2008)

  • We found a relationship between MD(A) and Mw based on common earthquakes in this time period listed in both the National Earthquake Information Center (NEIC) and Taiwan catalogs, as follows: MD(A) = 1.316 + 0.720Mw ± 0.43 (2)

Read more

Summary

Introduction

Taiwan is located at the juncture of the Philippine Sea plate on the east side and the Eurasian plate on the west side. The Longitudinal Valley in eastern Taiwan marks the suture zone of the two colliding plates. The Philippine Sea plate subducts northwardly under the Eurasian plate along the Ryukyu Trench in the eastern offshore region of Taiwan. Along the Manila Trench in the southern offshore region of Taiwan, the South China Sea Basin on the Eurasian plate subducts eastwardly under the Philippine Sea plate. Earthquakes occur very frequently in this region, many of which are disastrous.

Objectives
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call