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华东地区b值时空变化特征

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选取华东地区1980年至2023年10月ML≥2.0地震资料,利用最大似然法计算b值,分析研究区b值时空变化及近十年Δb空间分布特征,主要得到以下认识:(1)时变特征上,多数地震发生在b值下降时段,震后出现b值回升现象,也有少数其他对应情况;(2)空间特征上,多数中强地震都发生在低b值及其边界区域;(3)安徽与邻省边界地区(以豫鄂皖交界地区较为突出)、湖北中部等地区近十年应力水平有所升高,后续需持续关注其强震危险性.
Spatial and Temporal Variation of b-value in East China
The seismic data of ML≥2.0 from 1980 to October 2023 in East China were selected,and the b-value was calculated using the maximum likelihood method. The spatial and temporal changes of b-value and the spatial distribution characteristics of Δb in the study area in recent ten years were analyzed,and the following understandings were obtained:(1) In terms of time-varying characteristics,most earthquakes occur in the period when b-value drops,and b-value rises after earthquakes,and there are a few other cor-responding situations;(2) In terms of spatial characteristics,most moderate earthquakes occur in low b-values and their boundary regions;(3) The stress level in the border areas between Anhui and neighboring provinces (especially the border areas between Henan,Hubei and Anhui) and central Hubei have increased in recent ten years,and the risk of strong earthquakes should be continuously paid attention to in the future.

East China areamaximum likelihood methodb-valueΔb-valuespatio-temporal variation characteristics

翟娟、王俊、田雨桐、赵梦强、杨震

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淮南市地震局,安徽 淮南 232001

安徽省地震局,安徽 合肥 230031

华东地区 最大似然法 b值 Δb值 时空变化特征

2024

防灾减灾学报
辽宁省地震局,吉林省地震局,黑龙江省地震局,中国灾害防御学会

防灾减灾学报

影响因子:0.127
ISSN:1674-8565
年,卷(期):2024.40(3)