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作 者:V.H.Márquez-Ramírez F.A.Nava F.R.Zúiga
机构地区:[1]UNAM Campus Querétaro, México, Centro de Geociencias,Blvd.Juriquilla No 3001, 76230 México, Querétaro, México [2]Seismology Department, CICESE, Carretera Ensenada-Tijuana No 3918, Zona Playitas, 22860 Ensenada, BC, México
出 处:《Earthquake Science》2015年第2期129-134,共6页地震学报(英文版)
基 金:partially funded by UNAMDGAPA postdoctoral scholarship(VH Márquez-Ramírez);CONACYT grant 222795;UNAM-DGAPA-PAPIIT grant IN108115
摘 要:The effects of magnitude rounding and of the presence of noise in the rounded magnitudes on the estimation of the Gutenberg-Richter b-value are explored, and the ways to correct for these effects are proposed. For typical values, b = 1 and rounding interval △M = 0.1, the rounding error is approximately -10^-3 and it can be corrected to a negligible approximately -10^-5. For the same typical values, the effect of noise can be larger, depending on the characteristics of the noise distribution; for normally distributed noise with standard deviation σ = 0.1, the correct b-value may be underestimated by a factor - 0.97.The effects of magnitude rounding and of the presence of noise in the rounded magnitudes on the estimation of the Gutenberg-Richter b-value are explored, and the ways to correct for these effects are proposed. For typical values, b = 1 and rounding interval △M = 0.1, the rounding error is approximately -10^-3 and it can be corrected to a negligible approximately -10^-5. For the same typical values, the effect of noise can be larger, depending on the characteristics of the noise distribution; for normally distributed noise with standard deviation σ = 0.1, the correct b-value may be underestimated by a factor - 0.97.
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