Fractal (correlation)dimension and b-value are determined from seismic catalog recorded in Mongolia and its surrounding area.The spatial correlation of 1.56 is indicative of more or less clustered events in the region, while a b-value of 0.962 implies a highly active seismic region.A detailed study of the frequency-magnitude distribution and fractal dimension as a function of depth is also made.The results suggest structural variability at different depth levels in the Mongolia seismic zone that reflects highly heterogeneous and differential stress distribution in the region. Our result also shows that positive is the relationship between the b-value of the Gutenberg-Richter relation and the fractal dimension D of earthquakes in Mongolia region.
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徐伟进,高孟潭.蒙古国及其周边地区地震分形维度及b值研究[J].地震工程学报,2014,36(1):75-79. XU Wei-jin, GAO Meng-tan. Fractal Dimension and b-value of Earthquakes in Mongolia and Its Surrounding Area[J]. China Earthquake Engineering Journal,2014,36(1):75-79.