Efectos arqueosismológicos del terremoto de Acambay de 1912 (Michoacan, Mexico)
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Miguel A. Rodríguez Pascua [1] ; V.H. Garduño Monroy [2] ; R. Pérez López [1] ; M.A. Perucha [1] ; I. Israde Alcántara [2]
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[1] Instituto Geológico y Minero de España
Instituto Geológico y Minero de España
Madrid, España
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[2] Universidad Michoacana de San Nicolás de Hidalgo
Universidad Michoacana de San Nicolás de Hidalgo
México
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- Localización: El Cuaternario Ibérico: investigación en el s. XXI: VIII Reunión de Cuaternario Ibérico (Sevilla - La Rinconada 2013) / Rafael Baena Escudero (ed. lit.), José Juan Fernández Caro (ed. lit.), Inmaculada Guerrero Amador (ed. lit.), 2013, ISBN 978-84-695-8601-3, págs. 186-189
- Idioma: español
- Títulos paralelos:
- Archaeoseismological effects of the 1912 Acambay Earthquake, Michoacan, Mexico
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Resumen
The Acambay earthquake of 1912 was one of the most destructive intraplate earthquake in the XX Century located in central Mexico. Urbina and Camacho, geologist and seismologist respectively, researchers of the Mexican Geological Survey made one of the most complete and interesting field reports about destructive earthquakes. These authors reported the geological and archaeoseismological effects in the macroseismic zone. All of these data are useful so far and this paper revisited the macroseismic zone 100 years after and applies modern structural analysis in order to obtain new vision of the real consequences and the spatial distribution of the effects. It allow trace the mean direction of ground movement in the macroesismic zone (N-S).
