Artigo Revisado por pares

Macroseismic Study of the Devastating 22–23 October 1749 Earthquake Doublet in the Northern Colima Graben (Trans‐Mexican Volcanic Belt, Western Mexico)

2019; Seismological Society of America; Volume: 90; Issue: 6 Linguagem: Inglês

10.1785/0220190162

ISSN

1938-2057

Autores

Max Suter,

Tópico(s)

Geological and Tectonic Studies in Latin America

Resumo

ABSTRACT This detailed macroseismic study of a locally devastating earthquake doublet in the western part of the Trans‐Mexican volcanic belt, north of Fuego de Colima Volcano, on 22 and 23 October 1749 is based on contemporary documentary sources. The shocks razed the towns of Zapotlán el Grande (now Ciudad Guzmán) and Sayula and caused major damage in Amacueca and Atoyac. A first mainshock on 22 October 1749 at 4 p.m. was devastating in Sayula and Zapotlán el Grande and caused some damage in Amacueca. A stronger second mainshock ∼20 hr later, on 23 October 1749 at about noon, was destructive in Sayula, Amacueca, and Zapotlán el Grande where only three residential buildings remained standing. Estimates of the intensity magnitude MI of the mainshocks range between 5.7 and 6.0, with a preferred magnitude of 5.8. The macroseismic intensity distribution, limited area of destruction, and prolonged sequence of aftershocks, lasting at least until August 1750, indicate a local earthquake source in the northern Colima graben, most likely on the major fault bounding the Sayula half‐graben in the west.

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