Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratio

The sub-instability refers to a stress state that exists between the maximum stress the rock can withstand and its final failure. This stress state should be an indicator of impending large earthquakes, as it occurs in the final stage of earthquake nucleation. We apply the Load/Unload Response Ratio...

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Main Authors: Huaizhong Yu, Donghui Jia, Chieh-Hung Chen, Yue Liu, Haitao Wang, Jie Liu, Rui Yan, Binbin Zhao, Jianming Liu, Yuchuan Ma, Guihong Han, Wen Yang, Zhengyi Yuan, Zeping Li
Format: Article
Language:English
Published: Taylor & Francis Group 2024-12-01
Series:Geomatics, Natural Hazards & Risk
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Online Access:https://www.tandfonline.com/doi/10.1080/19475705.2024.2380911
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author Huaizhong Yu
Donghui Jia
Chieh-Hung Chen
Yue Liu
Haitao Wang
Jie Liu
Rui Yan
Binbin Zhao
Jianming Liu
Yuchuan Ma
Guihong Han
Wen Yang
Zhengyi Yuan
Zeping Li
author_facet Huaizhong Yu
Donghui Jia
Chieh-Hung Chen
Yue Liu
Haitao Wang
Jie Liu
Rui Yan
Binbin Zhao
Jianming Liu
Yuchuan Ma
Guihong Han
Wen Yang
Zhengyi Yuan
Zeping Li
author_sort Huaizhong Yu
collection DOAJ
description The sub-instability refers to a stress state that exists between the maximum stress the rock can withstand and its final failure. This stress state should be an indicator of impending large earthquakes, as it occurs in the final stage of earthquake nucleation. We apply the Load/Unload Response Ratio (LURR) method to explore sub-instability in the source media before large earthquakes. The earthquake-related observation data such as the groundwater, crustal deformation, electromagnetism and so on were adopted as data input. The load and unload phases at each observation station are discriminated by the change of Coulomb failure stress caused by earth tides along the tectonically optimal sliding direction. Retrospective studies of this approach on the 2020 Mw6.0 Jiashi, Xinjiang, 2022 Mw6.6 Menyuan, Qinghai, and Mw6.6 Luding, Sichuan earthquakes show that the LURR time series derived from the observation stations near the epicenter exceed 2 standard deviations of the mean within several days to years before the mainshocks. Additionally, as the time of mainshock approaches, the distance between the stations detecting LURR anomaly and epicenter decreases. The LURR anomalies indicate the presence of sub-instability prior to a large earthquake, and their spatio-temporal evolution may suggest the weakening processes in the source media.
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institution Kabale University
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publishDate 2024-12-01
publisher Taylor & Francis Group
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series Geomatics, Natural Hazards & Risk
spelling doaj-art-ca0238fe387b4192a57d45c638c4269b2024-12-12T18:11:18ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132024-12-0115110.1080/19475705.2024.2380911Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratioHuaizhong Yu0Donghui Jia1Chieh-Hung Chen2Yue Liu3Haitao Wang4Jie Liu5Rui Yan6Binbin Zhao7Jianming Liu8Yuchuan Ma9Guihong Han10Wen Yang11Zhengyi Yuan12Zeping Li13Xinjiang Pamir Intracontinental Subduction National Field Observation and Research Station, Urumqi, ChinaEarthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi, ChinaChengdu University of Technology, Chengdu, ChinaInstitute of Earthquake Forecasting, China Earthquake Administration, Beijing, ChinaChina Earthquake Networks Center, Beijing, ChinaChina Earthquake Networks Center, Beijing, ChinaChina Earthquake Networks Center, Beijing, ChinaEarthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi, ChinaEarthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi, ChinaChina Earthquake Networks Center, Beijing, ChinaEarthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi, ChinaChina Earthquake Networks Center, Beijing, ChinaChina Earthquake Networks Center, Beijing, ChinaChina Earthquake Networks Center, Beijing, ChinaThe sub-instability refers to a stress state that exists between the maximum stress the rock can withstand and its final failure. This stress state should be an indicator of impending large earthquakes, as it occurs in the final stage of earthquake nucleation. We apply the Load/Unload Response Ratio (LURR) method to explore sub-instability in the source media before large earthquakes. The earthquake-related observation data such as the groundwater, crustal deformation, electromagnetism and so on were adopted as data input. The load and unload phases at each observation station are discriminated by the change of Coulomb failure stress caused by earth tides along the tectonically optimal sliding direction. Retrospective studies of this approach on the 2020 Mw6.0 Jiashi, Xinjiang, 2022 Mw6.6 Menyuan, Qinghai, and Mw6.6 Luding, Sichuan earthquakes show that the LURR time series derived from the observation stations near the epicenter exceed 2 standard deviations of the mean within several days to years before the mainshocks. Additionally, as the time of mainshock approaches, the distance between the stations detecting LURR anomaly and epicenter decreases. The LURR anomalies indicate the presence of sub-instability prior to a large earthquake, and their spatio-temporal evolution may suggest the weakening processes in the source media.https://www.tandfonline.com/doi/10.1080/19475705.2024.2380911Sub-instabilityearthquake nucleationload/unload response ratioearthquake-related observationsstrain release point
spellingShingle Huaizhong Yu
Donghui Jia
Chieh-Hung Chen
Yue Liu
Haitao Wang
Jie Liu
Rui Yan
Binbin Zhao
Jianming Liu
Yuchuan Ma
Guihong Han
Wen Yang
Zhengyi Yuan
Zeping Li
Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratio
Geomatics, Natural Hazards & Risk
Sub-instability
earthquake nucleation
load/unload response ratio
earthquake-related observations
strain release point
title Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratio
title_full Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratio
title_fullStr Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratio
title_full_unstemmed Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratio
title_short Detecting sub-instability before three Mw > 6.0 earthquakes on Chinese mainland in 2020–2022 with load/unload response ratio
title_sort detecting sub instability before three mw 6 0 earthquakes on chinese mainland in 2020 2022 with load unload response ratio
topic Sub-instability
earthquake nucleation
load/unload response ratio
earthquake-related observations
strain release point
url https://www.tandfonline.com/doi/10.1080/19475705.2024.2380911
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