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Nonlinear analysis of the frequency-magnitude relationship in the western circum-pacific region

机译:西部环太平洋区域频率量级关系的非线性分析

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摘要

It has long been realized that the linear Gutenberg-Richter model arduously describes the frequency-magnitude relationship for the magnitude span ranging from small to large earthquakes because of the breakdown of the self-similarity rule due to the changing scaling of the magnitude. Three different segments should be observed from small (usually M<3.0), through moderate (M
机译:早就意识到线性线性古腾堡-里希特(Gutenberg-Richter)模型很难描述从小地震到大地震的震级跨度的频率-幅度关系,这是由于震级的变化导致自相似性规则崩溃的缘故。从小(通常为M <3.0)到中等(M

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