【摘 要】
：
Based on the analysis of newly collected data of plate tectonics, distribution of active faults and crustal deformation, the Taiwan area is divided into two sei
【机 构】
：
Institute of Geology,Earthquake Administration of Fujian Province,China Aero Geophysical Survey and
【基金项目】
：
国家自然科学基金;This research was supported by the Joint Earthquake Science Foundation grant number;Special Thanks are due to two anonymous reviewers for their constructive comments
论文部分内容阅读
Based on the analysis of newly collected data of plate tectonics, distribution of active faults and crustal deformation, the Taiwan area is divided into two seismic regions and six seismic belts. Then, correlation fractal dimensions of all the regions and belts are calculated, and the fractal characteristics of hypocenteral distribution can be quantitatively analyzed. Finally, multifractal dimensions Dq andf(α) are calculated by using the earthquake catalog of the past 11 years in the Taiwan area. This study indicates that (1) there exists a favorable corresponding relationship between spatial images of seismic activity described with correlation fractal dimension analysis and tectonic settings; (2) the temporal structure of earthquakes is not single but multifractal fractal, and the pattem of Dq variation with time is a good indicator for predicting strong earthquake events.
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