Seismological Research Letters; September/October 2009; v. 80; no. 5;
p. 694-706; DOI: 10.1785/gssrl.80.5.694
© 2009 Seismological Society of America
ARTICLES: SPECIAL SECTION ON EARTHQUAKE EARLY WARNING |
Evolution of the Mexican Seismic Alert System (SASMEX)
J. M. Espinosa-Aranda,
A. Cuellar,
A. Garcia,
G. Ibarrola,
R. Islas,
S. Maldonado, and
F. H. Rodriguez
Centro de Instrumentación y Registro
Sísmico, A. C. (CIRES), Mexico
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BACKGROUND
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The seismic activity along the Mexican coastline, where the Cocos, Rivera,
and Pacific plates collide with the North American plate, represents the
source of most of the strong earthquakes experienced by the different
civilizations that have developed over the centuries in the Mexican territory,
as documented by the inhabitants of the Valley of Mexico prior to the arrival
of the Spaniards (Figure 1),
who referred to an earthquake that occurred in the year Uno Pedernal
(One Flint), corresponding to the year 1480
(Suarez and Acosta 1996).
The Pacific Mexican coast, consisting of the states of Jalisco, Colima,
Michoacan, Guerrero, Oaxaca, and Chiapas, is part of the so called fire belt
and has been regarded as one of the regions with the highest seismic activity
in the world. From 1875 to 2008 more than 160 large earthquakes (magnitude
M > 6.5) occurred in this region
(Figure 2).
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INTRODUCTION
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One of the major seismic catastrophes in recent Mexican history took place
the morning of 19 September 1985 in Mexico City, resulting from the ground
motion amplification of the M 8.1 earthquake that occurred off the
coast of Michoacan. The effects of that earthquake caused at least 10,000
deaths and 30,000 injuries in Mexico City, which is located about 400 km away
from the epicenter. The analysis of seismic records from that event allowed
scientists to determine that the effect of the energy in the subsoil of Mexico
City induced resonance in the structure of several buildings, which caused
their collapse and the high toll in casualties; in addition, neither early
warnings nor previous training for a quick emergency response in case of a
major earthquake were available (Esteva
1988).
After experiencing the serious seismic effects of the 1985 earthquake, both
national and international experts recommended . . . [Full Text of this Article]
Centro de Instrumentación y Registro Sísmico, A. C.
Anaxagoras Av., No. 814
Narvarte Sec., Benito Juarez, 03020 Mexico, D.
F.
Mexico
espinosajm@cires.org.mx
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