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Wavelet Analysis of Earthquake Activity in the West of the Chinese Mainland and Its Adjacent Area

机译:中国大陆西部及邻区地震活动的小波分析。

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摘要

Wavelets are a useful tool for analyzing the time-frequency of a non-stable series and are widely applied in many fields. The process of earthquake preparation and occurrence is a non-linear process. In the paper, the wavelet method is used to analyze the series of earthquake data for the time period from 1900 to 2003 in the west of the Chinese mainland and its adjacent area (WCMAA), and to obtain the characteristic information for different time scales. In the past 103 years, there were four primary periods of regional earthquake activity in the area with durations of 42, 22, 7 and 14 years, respectively and the intensity of earthquake activity changing with time. It doesn't make sense to talk about active or quiet periods of earthquake activity unless it is based on a specific time scale. In addition, the tendency analysis of earthquake activity using the primary period of seismic activity and wavelet coefficients of varied time scales indicates that the earthquake activity in this region will be high in the forthcoming years.
机译:小波是分析不稳定序列时间频率的有用工具,广泛应用于许多领域。地震的发生和发生过程是一个非线性过程。本文采用小波方法分析了中国大陆西部及其邻近地区(WCMAA)1900〜2003年的一系列地震资料,并获得了不同时标的特征信息。在过去的103年中,该地区有四个主要的区域地震活动时期,分别为42、22、7和14年,地震活动的强度随时间而变化。除非是基于特定的时间尺度,否则谈论地震活动的活跃或安静时期是没有意义的。此外,利用地震活动的主要时期和不同时标的小波系数对地震活动进行趋势分析,表明该地区的地震活动在未来几年将很高。

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