The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordings

On September 8, 2018, an MS 5.9 earthquake struck Mojiang, a county in Yunnan Province, China. We collect near-field seismic recordings (epicentral distances less than 200 km) to relocate the mainshock and the aftershocks within the first 60 hours to determine the focal mechanism solutions of the ma...

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Main Authors: Xu Zhang, Zhen Fu, LiSheng Xu, ChunLai Li, Hong Fu
Format: Article
Language:English
Published: Science Press 2019-05-01
Series:Earth and Planetary Physics
Subjects:
Online Access:http://www.eppcgs.org/article/doi/10.26464/epp2019028?pageType=en
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author Xu Zhang
Zhen Fu
LiSheng Xu
ChunLai Li
Hong Fu
author_facet Xu Zhang
Zhen Fu
LiSheng Xu
ChunLai Li
Hong Fu
author_sort Xu Zhang
collection DOAJ
description On September 8, 2018, an MS 5.9 earthquake struck Mojiang, a county in Yunnan Province, China. We collect near-field seismic recordings (epicentral distances less than 200 km) to relocate the mainshock and the aftershocks within the first 60 hours to determine the focal mechanism solutions of the mainshock and some of the aftershocks and to invert for the finite-fault model of the mainshock. The focal mechanism solution of the mainshock and the relocation results of the aftershocks constrain the mainshock on a nearly vertical fault plane striking northeast and dipping to the southeast. The inversion of the finite-fault model reveals only a single slip asperity on the fault plane. The major slip is distributed above the initiation point, ~14 km wide along the down-dip direction and ~14 km long along the strike direction, with a maximal slip of ~22 cm at a depth of ~6 km. The focal mechanism solutions of the aftershocks show that most of the aftershocks are of the strike-slip type, a number of them are of the normal-slip type, and only a few of them are of the thrust-slip type. On average, strike-slip is dominant on the fault plane of the mainshock, as the focal mechanism solution of the mainshock suggests, but when examined in detail, slight thrust-slip appears on the southwest of the fault plane while an obvious part of normal-slip appears on the northeast, which is consistent with what the focal mechanism solutions of the aftershocks display. The multiple types of aftershock focal mechanism solutions and the slip details of the mainshock both suggest a complex tectonic setting, stress setting, or both. The intensity contours predicted exhibit a longer axis trending from northeast to southwest and a maximal intensity of Ⅷ around the epicenter and in the northwest.
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spelling doaj.art-dbd19872c32349efa6bf30e392fdd28b2022-12-22T03:42:35ZengScience PressEarth and Planetary Physics2096-39552019-05-013326828110.26464/epp2019028xulisheng1The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordingsXu Zhang0Zhen Fu1LiSheng Xu2ChunLai Li3Hong Fu4Institute of Geophysics, China Earthquake Administration, Beijing 100081, ChinaInstitute of Geophysics, China Earthquake Administration, Beijing 100081, ChinaInstitute of Geophysics, China Earthquake Administration, Beijing 100081, ChinaInstitute of Geophysics, China Earthquake Administration, Beijing 100081, ChinaEarthquake Administration of Yunnan Province, Kunming 650224, ChinaOn September 8, 2018, an MS 5.9 earthquake struck Mojiang, a county in Yunnan Province, China. We collect near-field seismic recordings (epicentral distances less than 200 km) to relocate the mainshock and the aftershocks within the first 60 hours to determine the focal mechanism solutions of the mainshock and some of the aftershocks and to invert for the finite-fault model of the mainshock. The focal mechanism solution of the mainshock and the relocation results of the aftershocks constrain the mainshock on a nearly vertical fault plane striking northeast and dipping to the southeast. The inversion of the finite-fault model reveals only a single slip asperity on the fault plane. The major slip is distributed above the initiation point, ~14 km wide along the down-dip direction and ~14 km long along the strike direction, with a maximal slip of ~22 cm at a depth of ~6 km. The focal mechanism solutions of the aftershocks show that most of the aftershocks are of the strike-slip type, a number of them are of the normal-slip type, and only a few of them are of the thrust-slip type. On average, strike-slip is dominant on the fault plane of the mainshock, as the focal mechanism solution of the mainshock suggests, but when examined in detail, slight thrust-slip appears on the southwest of the fault plane while an obvious part of normal-slip appears on the northeast, which is consistent with what the focal mechanism solutions of the aftershocks display. The multiple types of aftershock focal mechanism solutions and the slip details of the mainshock both suggest a complex tectonic setting, stress setting, or both. The intensity contours predicted exhibit a longer axis trending from northeast to southwest and a maximal intensity of Ⅷ around the epicenter and in the northwest.http://www.eppcgs.org/article/doi/10.26464/epp2019028?pageType=en2018 ms 5.9 mojiang earthquakenear-field seismic recordingfinite-fault modelintensity predictionfocal mechanism solution
spellingShingle Xu Zhang
Zhen Fu
LiSheng Xu
ChunLai Li
Hong Fu
The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordings
Earth and Planetary Physics
2018 ms 5.9 mojiang earthquake
near-field seismic recording
finite-fault model
intensity prediction
focal mechanism solution
title The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordings
title_full The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordings
title_fullStr The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordings
title_full_unstemmed The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordings
title_short The 2018 MS 5.9 Mojiang Earthquake: Source model and intensity based on near-field seismic recordings
title_sort 2018 ms 5 9 mojiang earthquake source model and intensity based on near field seismic recordings
topic 2018 ms 5.9 mojiang earthquake
near-field seismic recording
finite-fault model
intensity prediction
focal mechanism solution
url http://www.eppcgs.org/article/doi/10.26464/epp2019028?pageType=en
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