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Anomalies of Precursory Group and Grouped Strong Earthquakes in the Sichuan-Yunnan Region

机译:川滇地区前兆群异常和强地震群

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摘要

Three methods of extracting the information of anomalies of a precursory group are put forward, i.e., the mathematical analyses of the synthetic information of earthquake precursors (S), the inhomogeneous degree of precursory groups (ID) and the values of short-term and impending anomaly in near-source area (NS). Using these methods, we calculate the observational data of deformation, underground fluid and hydrochemical constituents obtained from different seismic stations in the Sichuan-Yunnan region and conclude that the synthetic precursory anomalies of a single strong earthquake with M_s 6.0 differ greatly from those of the grouped strong earthquakes, for the anomalous information of precursory groups are more abundant. The three methods of extracting the synthetic precursory anomaly and the related numerical results can be applied into the practice of prediction to the grouped strong earthquakes in the Sichuan-Yunnan region. Inhomogeneous degree (ID) of synthetic precursory anomaly can be identified automatically because it takes the threshold of distributive characteristics of the anomalies of precursory group as its criterion for anomaly.
机译:提出了提取前兆异常信息的三种方法,即地震前兆综合信息(S)的数学分析,前兆群的不均匀度(ID)以及短期和即将发生的值的数学分析。近源区(NS)异常。利用这些方法,我们计算了从川滇地区不同地震台站获得的形变,地下流体和水化学成分的观测数据,并得出结论,一次M_s 6.0级强地震的合成前兆异常与该组的差异很大。强地震,对于前兆群体的异常信息更为丰富。合成前兆异常的三种提取方法及相关数值结果可用于川滇地区成组强地震的预测实践。合成前兆异常的不均匀度(ID)可以自动识别,因为它以前兆基团的异常分布特征阈值为异常标准。

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