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ISSN 2096-7780 CN 10-1665/P

弱震背景下沂沭带周边小震前后流动重力场变化特征研究

Study on Variation Characteristics of Mobile Gravity Field Before and After Small Earthquakes Around the Yishu Belt Under the Background of Weak Seismic Activity

  • 摘要: 为探究弱震背景下山东地区小震与重力场变化的关联性,本研究以沂沭断裂带周边为核心区域,选取2013年莱州ML4.9、2015年平邑ML3.9(塌陷)、2020年长清ML4.6等ML3.0以上地震为研究对象,基于山东省地震局全省流动重力观测网数据(2010-2022年,观测周期1年2次,采用LGADJ软件经典平差方法处理数据后,分析地震前后不同时间尺度(相邻两期间隔0.5年左右、1年/2年/5年多年累积)的重力场变化特征。结果表明:小震发震前后的相邻两期重力场变化中,震中周边均出现幅度超阈值(相邻两期50 μGal、1年期80 μGal)的区域,且震中多位于0值线或10 μGal等值线的拐弯处;时间尺度上,相邻两期及1年间隔变化图中震中附近变化显著,2年及以上多年累积图中变化不明显;显著变化测点仅在发震前后出现剧烈变化,其它时间保持平稳。综上,山东地区沂沭断裂带周边小震发生前后,重力场变化通常在半年至1年内呈现显著异常,震中位置与0值线或10 μGal等值线拐弯处高度关联,可为该区域小震监测与中期预测提供科学依据。

     

    Abstract: To explore the correlation between small earthquakes and gravity field changes in Shandong Province under the background of weak seismic activity, this study takes the area around the Yishu Fault Zone as the core region. It selects earthquakes with magnitudes of ML3.0 and above, including the 2013 Laizhou ML4.9 earthquake, the 2015 Pingyi ML3.9 (collapse-induced) earthquake, and the 2020 Changqing ML4.6 earthquake, . Based on the data from the provincial mobile gravity observation network of Shandong Earthquake Agency , the data were processed using the classical adjustment method of LGADJ software. Subsequently, the characteristics of gravity field changes before and after the earthquakes were analyzed across different time scales, including adjacent phases (with an interval of approximately 0.5 years) and multi-year accumulations (1-year, 2-year, and 5-year).The results show that: In the gravity field changes between adjacent phases before and after the occurrence of small earthquakes, areas with changes exceeding the threshold (50 μGal for adjacent phases and 80 μGal for 1-year scale) appear around the epicenters, and the epicenters are mostly located at the bends of the 0 μGal contour line or 10 μGal contour line. In terms of time scales, the changes near the epicenters are significant in the maps of adjacent phases and 1-year interval changes, while the changes are not obvious in the maps of multi-year accumulations (2 years and above). The measuring points with significant changes only show drastic variations before and after the earthquakes, and remain stable at other times.In conclusion, before and after the occurrence of small earthquakes around the Yishu Fault Zone in Shandong Province, significant anomalies in the gravity field usually appear within 6 months to 1 year, and the epicenter location is highly correlated with the bends of the 0 μGal contour line or 10 μGal contour line. This study can provide a scientific basis for the monitoring and medium-term prediction of small earthquakes in this region.

     

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