| 地震前兆异常时间分布非线性特征的初步探讨——以海城地震和唐山地震为例 |
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| 引用本文： | 邓志辉,马瑾.地震前兆异常时间分布非线性特征的初步探讨——以海城地震和唐山地震为例[J].地震地质,1993,15(3):213-219. |
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| 作者姓名： | 邓志辉 马瑾 |
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| 作者单位： | 国家地震局地质研究所，国家地震局地质研究所 北京 100029，北京 100029 |
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| 摘 要： | 震源系统是一个与外界既有物质交换又有能量交换的耗散系统,在其发展演化过程中会经历一系列的分岔突变。作者运用非线性动力学的方法,分析了海城地震和唐山地震的前兆资料。研究结果表明,前兆异常活动具有阶段性,相邻两个异常阶段的持续时间的比值为一常量(5左右)。这种前兆时间分布规律可用震源体内应变能密度随孕震时间的增加发生倍周期分岔进行解析。它可用于预测主震的发生时间
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| 关 键 词： | 震源非线性 地震前兆 地震预报 |
ON NONLINEAR CHARACTERISTICS OF EARTHQUAKE PRECURSOR TIME WITH REFERENCE TO HAICHENG AND TANGSHAN EARTHQUAKES |
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| Deng Zhihui Ma Jin.ON NONLINEAR CHARACTERISTICS OF EARTHQUAKE PRECURSOR TIME WITH REFERENCE TO HAICHENG AND TANGSHAN EARTHQUAKES[J].Seismology and Geology,1993,15(3):213-219. |
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| Authors: | Deng Zhihui Ma Jin |
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| Abstract: | Earthquake focus system is a dissipative system which continuously exchanges energy and mass with outside. There will be a series of bifurcations in the process of earthquake preparation. The precursors of 1975 Haicheng earthquake in Northeast China and 1976 Tangshan earthquake in North China are studied with nonlinear dynamic method. There are 5 similar precursor stages for the two earthquakes. The durations reduced sequentially from the first stage to the fifth stage. The ratio of the durations of the two adjacent precursor stages is a constant (about 5). Five stages bagan about 2.5 years, 5.5 months, 1 month, 6 days and 1 day separately before the earthquake occurred.The main precusor features are: (1) gravity anomaly, (2) strain and stress conversion or jump at the background of strain and stress anomaly, (3) anomaly of the groundwater in very large region, (4) great variation of the air temperature and the geotemperature, the fluctuation of air pressure and the abnormal behaviors of domestic animals, and (5) eaarthquake lighting, earthquake sounds frequently and seriously disturbed radiowave.This relationship of precursor stages resulted from the period-doubling bifurcations in earthquake focus body with the increase of earthquake preparation time. Each grade bifurcation point corresponds to one precursor stage start time. The ratio of the durations of two adjacent precursor stages approximates to well-known Feigenbaum number (4.67). According to this relationship, we can predict the start time of later precursor stages and main shock time when two or more precursor stages are known. |
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| Keywords: | Nonlinear focus Earthquake precursor Earthquake prediction |
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