[1]ZHENG Qiuyue,HUANG Jiangpei,WU Yuqin,et al.Analysis of the Gravity Variation Index before the Yangbi MS6.4 Earthquake and Inversion of the Field Source Characteristics[J].Journal of Seismological Research,2025,(01):22-31.[doi:10.20015/j.cnki.ISSN1000-0666.2025.0003
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Journal of Seismological Research[ISSN 1000-0666/CN 53-1062/P] Volume:
Number of periods:
2025 01
Page number:
22-31
Column:
Public date:
2024-12-20
- Title:
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Analysis of the Gravity Variation Index before the Yangbi MS6.4 Earthquake and Inversion of the Field Source Characteristics
- Author(s):
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ZHENG Qiuyue; HUANG Jiangpei; WU Yuqin; CHEN Zhengyu; LIU Dong; WANG Qinghua
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(Yunnan Earthquake Agency,Kunming 650224,Yunnan,China)
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- Keywords:
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gravity segment differences; quantitative analysis; gravity variations index; field-source inversion; the Yangbi MS6.4 earthquake
- CLC:
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P315.726
- DOI:
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10.20015/j.cnki.ISSN1000-0666.2025.0003
- Abstract:
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In this paper,we use the visualization method of the gravity segment differences and the quantitative indicators of gravity variation G and C,to process the mobile gravity data obtained by repeated measurements in Yunnan from 2016 to 2021 and study the gravity variation before the Yangbi MS6.4 earthquake on May 21,2021.We further invert the distribution characteristics of seismic-related source in the study area.The results are as follows:①The scale and the direction of the gravity segment indicated more or less the migration direction of the subsurface material,and the gravity variation indicators G and C increased significantly before the Yangbi earthquake,then decreased rapidly after the earthquake.G and C can be used to evaluate the significance of the regional gravity changes in the area covered by the gravity observation network.②The inverted positions of the field-source mainly concentrated in the zone from the northern section of the Red River Fault Zone to the northwestern Yunnan,exhibiting a distribution pattern consistent with the Weixi-Qiaohou Fault and the Red River Fault Zone; this situation was possibly correlated with the migration of the deep material in the middle and upper Crust before the Yangbi earthquake.