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《Inland Earthquake》 1990-04
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A PRELIMINARY STUDY ON SELF - SIMILARITY PHENOMENA OF EARTHQUAKES

Li Haihua(Seismological Bureau of Hainan Province, Haikou)Zhang Yongli(Seismological Institute of Lanzhou,SSB)Zhang Wenxiao(Seismological Bureau of Ninxia Hui Autonomous Region, Yinchuan)Guo Yaping, Ma Wenjing(Seismological Bureau of Qinghai Province, Xining)  
The ratio of three main axies for a self-similarity ellipsoid earthquake source a:b:c=1 :0. 2 : 0.2 has been got according to the similarity of rupture process and physical parameters of the source. Based on the fractal theory and method,the reduction of dimension value before strong earthquake occurrence for self-similar earthquake distribution in time and space has been discussed.The result that scale of precursory anomaly area (red-swelling area) is five times larger than that of the source area could be obtained from extension area of precursors and characteristics of regional seismicity before large earthquake and seismic gap.et al.
【Fund】: 地震科学联合基金
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【Co-citations】
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