UCL Discovery
UCL home » Library Services » Electronic resources » UCL Discovery

Source Characteristics of the 2016 Meinong (ML 6.6) Taiwan Earthquake Revealed from Dense Seismic Arrays: Double Sources and Pulse-like Velocity Ground Motion

Lin, YY; Yeh, TY; Ma, KF; Song, TRA; Lee, SJ; Huang, BS; Wu, YM; (2018) Source Characteristics of the 2016 Meinong (ML 6.6) Taiwan Earthquake Revealed from Dense Seismic Arrays: Double Sources and Pulse-like Velocity Ground Motion. Bulletin of the Seismological Society of America , 108 (1) pp. 188-199. 10.1785/0120170169. Green open access

[thumbnail of Linetal2017Meinong_accepted.pdf]
Preview
Text
Linetal2017Meinong_accepted.pdf - Accepted Version

Download (6MB) | Preview

Abstract

The 5 February 2016, Meinong, Taiwan, earthquake brought extensive damage to nearby cities with significant pulse‐like velocity ground motions. In addition to the spatial slip distribution determination using filtered strong‐motion data, we show that, with the advantage of the densely distributed seismic network as a seismic array, we can project the earthquake sources (asperities) directly using nearly unfiltered data, which is crucial to the understanding of the generation of the pulse‐like velocity ground motions. We recognize that the moderate but damaging ML 6.6 Meinong earthquake was a composite of an Mw 5.5 foreshock and an Mw 6.18 mainshock with a 1.8–5.0 s time delay. The foreshock occurred at the hypocenter reported by the official agency, followed by the mainshock with a centroid located at 12.3 km to the north‐northwest of the hypocenter and at a depth of 15 km. This foreshock–mainshock composition is not distinguishable in the finite‐fault inversion because it filtered the seismic data to low frequencies. Our results show that the pulse‐like velocity ground motions are mainly attributed to the source of mainshock with its directivity and site effects, resulting in the disastrous damages in the city of Tainan. Although finite‐fault inversion using filtered seismic data for spatial slip distribution on the fault has been a classic procedure in understanding earthquake rupture processes, using a dense seismic network as a seismic array for unfiltered records helps us delineate the earthquake sources directly and provide more delicate information for future understanding of earthquake source complexity.

Type: Article
Title: Source Characteristics of the 2016 Meinong (ML 6.6) Taiwan Earthquake Revealed from Dense Seismic Arrays: Double Sources and Pulse-like Velocity Ground Motion
Open access status: An open access version is available from UCL Discovery
DOI: 10.1785/0120170169
Publisher version: https://doi.org/10.1785/0120170169
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery.ucl.ac.uk/id/eprint/10037979
Downloads since deposit
164Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item