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模糊分维及其在地震研究中的某些应用
引用本文:冯德益,林命周.模糊分维及其在地震研究中的某些应用[J].地球物理学报,1992,35(4):459-468.
作者姓名:冯德益  林命周
作者单位:1. 天津市地震局 天津 300201; 2. 上海市地震局 上海 200062
摘    要:在模糊集理论与分形理论的基础上,引进了模糊分维的概念;给出了模湖容量维D0与模糊关联维D2的定义与确定方法;讨论了模糊分维与常用的分维(清晰分维)的关系.给出了模糊分维在地震研究中的应用结果: 1.根据模糊容量维D0随时间的上升趋势变化,可以划分出大地震活动的高潮期;由模糊容量维D0与模糊关联维D2随时间变化的曲线,可以分析识别大地震前的中长期前兆异常. 2.根据模糊容量维D0随空间和时间的变化,可以划分出未来大震所在的地区,并可发现大震前数年D0呈现增大或减小的趋势. 3.根据前兆数据的模糊时间分维D0随时间的变化,可以发现大地震的短期前兆异常.

关 键 词:模糊分维  模糊关联维  模糊时间分维  模饰空间分维  大地震前兆  
收稿时间:1990-06-26

FUZZY FRACTAL DIMENSION AND ITS SOME APPLICATIONS IN EARTHQUAKE RESEARCHES
FENG DE-YI LIu XI-LAN JIANG CHUN ZHENG XI-MING.FUZZY FRACTAL DIMENSION AND ITS SOME APPLICATIONS IN EARTHQUAKE RESEARCHES[J].Chinese Journal of Geophysics,1992,35(4):459-468.
Authors:FENG DE-YI LIu XI-LAN JIANG CHUN ZHENG XI-MING
Institution:Seismological Bureau of Tianjin, Tianjin 300201; 2. Seismological Bureau of Shanghai, Shanghai 200062
Abstract:At first, based on the theory of fuzzy sets and fractal theory, the concepts of fuzzy fractal dimensions has been further introduced, the definitions and methods for determination of fuzzy Hausdorff fractal dimension D0 and fuzzy relative fractal dimension D2 were given, and the relation between fuzzy fractal dimension and usual (clear) fractal dimension was discussed.Then, three results of the applications of the fuzzy fractal dimension in earthquake researches were obtained. They are as follows:1.The characteristics of fuzzy temporal fractal dimension of the activity- of large earthquakes. According to the variation of fuzzy temporal fractal dimension D0(1) with respect to time, the periods of high seismicity of large earthquakes corresponding to the periods of increase of D0(1) can be distinguished. By using the temporal variation curves of fuzzy Hausdorff fractal dimension D0(1) and fuzzy relative fractal dimension D2 the long-medium term precursory anomalous variations in seismicity before large earthquakes may be recognized.2.The characteristics of fuzzy spatial fractal dimension of the activity of strong and moderate earthquakes. According to the temporal and spatial variations of D0(2), the riskful regions of forthcoming large earthquakes corresponding to the regions of increase or decrease of D0(2) and the anomalous variations of seismicity in several years before large earthquakes may be recognized.3.The characteristics of fuzzy temporal fractal dimension of the earthquake precursors. According to the variation of fuzzy temporal fractal dimension D0(1) of precursors data with respect to time,the short term precursory anomalies before large earthquakes may be discovered.
Keywords:Fuzzy fractal dimension Q0  Fuzzy relative fractal dimension D2  Fuzzy temporal fractal dimension  Fuzzy spatial fractal dimension  Large earthquake precursor  
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