Repeated seismic swarms near paricutin volcano: precursors to the birth of a new monogenetic volcano in the michoacán-guanajuato volcanic field, méxico?

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SUMMARY

Propagating dike, with a clear temporal evolution in their hypocenters following the migration of the tip of the dike (Ukawa and Tsukahara 1996). The Omori law usually applies to a tectonic origin, such as for aftershock sequences, but does not apply for Bulletin of Volcanology also the case in the MGVF where several Holocene clusters have been identified (e_g, Hasenaka and Carmichael 1985a, b; 1987; Mahgoub et_al 2017). The same location of the different swarms suggests that the magma is following the same vertical dike network (below ~ 8 km depth), but is not necessarily . . .

 



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