Relationship between Crustal Deformation and Thermal Anomalies in the 2022 Ninglang Ms 5.5 Earthquake in China: Clues from InSAR and RST

Author:

Lai Zhibin1,Chao Jiangqin23,Zhao Zhifang145,Wen Mingchun2,Yang Haiying12,Chai Wang1,Yao Yuan1,Zhao Xin2,Chen Qi1,Liu Jianyu2

Affiliation:

1. School of Earth Sciences, Yunnan University, Kunming 650500, China

2. Institute of International Rivers and Eco-Security, Yunnan University, Kunming 650500, China

3. School of Geographical Sciences and Tourism, Zhaotong University, Zhaotong 657000, China

4. Engineering Research Center of Domestic High-Resolution Satellite Remote Sensing Geology for Universities of Yunnan Province, Kunming 650500, China

5. MNR Key Laboratory of Sanjiang Metallogeny and Resources Exploration & Utilization, Kunming 650051, China

Abstract

On 2 January 2022, an earthquake of Ms 5.5 occurred in Ninglang County, Lijiang City, the earthquake-prone area of northwestern Yunnan. Whether this earthquake caused significant deformation and thermal anomalies and whether there is a relationship between them needs further investigation. Currently, multi-source remote sensing technology has become a powerful tool for long-time-series monitoring of earthquakes and active ruptures which mainly focuses on single crustal deformation and thermal anomaly. This study aims to reveal the crustal deformation and thermal anomaly characteristics of the Ninglang earthquake by using both Interferometric Synthetic Aperture Radar (InSAR) and Robust Satellite Techniques (RST). First, Sentinel-1A satellite SAR data were selected to obtain the coseismic deformation field based on Differential InSAR (D-InSAR), and the Small Baseline Set InSAR (SBAS-InSAR) technique was exploited to invert the pre- and post-earthquake displacement sequences. Then, RST was used to extract the thermal anomalies before and after the earthquake by using Moderate Resolution Imaging Spectroradiometer Land Surface Temperature (MODIS LST). The results indicate that the seismic crustal deformation is dominated by subsidence, with 23 thermal anomalies before and after the earthquake. It is speculated that the Yongning Fault in the deformation area is the main seismogenic fault of the Ninglang earthquake, which is dominated by positive fault dip-slip motion. Meanwhile, the seismic fault system composed of NE- and NW-oriented faults is an important factor in the formation of thermal anomalies, which are accompanied by changes in stress at different stages before and after the earthquake. Moreover, the crustal deformation and seismic thermal anomalies are correlated in time and space, and the active rupture activities in the region produce deformation accompanied by changes in thermal radiation. This study provides clues from remote sensing observations for analyzing the Ninglang earthquake and provides a reference for the joint application of InSAR and RST for earthquake monitoring.

Funder

National Natural Science Foundation of China

China-Myanmar Joint Laboratory for Ecological and Environmental Conservation

the Scientific Research Foundation of Yunnan Province Education Department

the China Geological Survey Project

Science and Technology Plan Project of Yunnan Province Science and Technology Department

the List of Key Science and Technology Projects in the Transportation Industry of the Ministry of Transport in 2021

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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