GROUND MOTION IN CENTRAL MEXICO. PATH EFFECTS DUE TOTHE TRANSMEXICAN VOLCANIC BELT

机译：墨西哥中部的地面运动。穿越墨西哥火山带的路径效应

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In this work the influence of the Transmexican Volcanic Belt on the propagation of surface waves withperiods between 1 and 10 s is studied. The data used are acceleration records of 13 events recorded alongtwo lines of stations. We considered different paths epicenter-Mexico City. The results show that, forperiods smaller than a given value, the seismic motion that propagates towards Mexico City fromearthquakes that occur in the subduction zone of the Pacific coast are affected by presence of the TVB.This period value depends on the path.

机译：在这项工作中，研究了跨墨西哥火山带对周期在1到10 s之间的表面波传播的影响。所使用的数据是沿两站线记录的13个事件的加速度记录。我们考虑了震中-墨西哥城的不同路径。结果表明，在小于给定值的时期内，从太平洋沿岸俯冲带发生的地震向墨西哥城传播的地震运动受到TVB的影响，该周期值取决于路径。

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《World conference on earthquake engineering;WCEE》|2004年|1-12|共12页
会议地点 Vancouver(CA);Vancouver(CA)
作者
Hugo FERRER-TOLEDO; Francisco CHáVEZ-GARCíA; Martín CáRDENAS-SOTO;
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Institute of Geophysics. Earth Science Graduate Program UNAM. Circ.de la Investigación Científicas/n Ciudad Universitaria Coyoacán 04510. México D.F. Ferrer@upaep.mx;

Institute of Engineering. Seismological Engineering UNAM. Ciudad Universitaria Apartado Postal04510 México D.F. paco@hermes.iingen.unam.mx;

DICT School of Engineering UNAM. Circuito Interior s/n Ciudad Universitaria Coyoacán 04510 México D.F. martinc@servidor.unam.mx;

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GROUND MOTION IN CENTRAL MEXICO. PATH EFFECTS DUE TOTHE TRANSMEXICAN VOLCANIC BELT

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