Variation of b and p values from aftershocks sequences along the Mexican subduction zone and their relation to plate characteristics

Author:

Ávila-Barrientos L.,Zúñiga F.R.ORCID,Rodríguez-Pérez Q.,Guzmán-Speziale M.

Funder

UNAM DGAPA/PAPIIT program

CONACyT Cátedras program

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference58 articles.

1. Maximum likelihood estimate of b in the formula log N = a bM and its confidence limits;Aki;Bull. Earthq. Res. Inst.,1965

2. Scale-free networks of earthquakes and aftershocks;Baiesi;Phys. Rev. E,2004

3. Complex networks of earthquakes and aftershocks;Baiesi;Nonlinear Process. Geophys.,2005

4. The subducted Rivera-Cocos plate boundary: where is it, what is it, and what is its relationship to the Colima rift?;Bandy;Geophys. Res. Lett.,1995

5. Maximum likelihood estimation of b values for magnitude grouped data;Bender;Bull. Seismol. Soc. Am.,1983

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