Physics
Scientist
Instituto de Ingeniería, UNAM, Cd. Universitaria, Apdo 70-472, Coyoacán CP 04510, México DF, Mexico. de Ingeniería, UNAM, Cd. Universitaria, Apdo 70-472, Coyoacán 04510, México. ; Instituto Mexicano del Petróleo, Eje Central L. Cárdenas 152, CP 07730, México. de Ingeniería, UNAM, Cd. Universitaria, Apdo. 70-472, Coyoacán 04510, México DF, Mexico. de Ingeniería, UNAM; Cd. Universitaria, Apdo. Postal 70-472; C.P. 04510; México D.F., México. de Ingeniería, Universidad Nacional Autónoma de México, Cd. Universitaria, Circuito Escolar s / n, Coyoacán 04510, México D. F., Mexico
Instituto de Ingeniería, Universidad Nacional Autónoma de México, Coyoacán, Mexico
Instituto de Ingeniería, Universidad Nacional Autónoma de México Cd. Universitaria, Apdo 70-472; Coyoacán 04510; México D.F., Mexico.
Instituto de Ingeniería, UNAM; Cd. Universitaria, Coyoacán 04510, México D. F., Mexico. de Ingeniería, UNAM; Cd. Universitaria, Apdo, 70-472, Coyoacán 04510, México D.F., Mexico
Instituto de Ingeniería, UNAM, México
An approximate elastic two-dimensional Green's function for a constant-gradient medium
Can horizontal P waves be trapped and resonate in a shallow sedimentary basin?
Comment on `evidence of the dominance of higher-mode surface waves in the lake-bed zone of the valley of Mexico by Shapiro et al. (2001)'
Diffraction of P, S and Rayleigh waves by three-dimensional topographies
Diffraction of SH cylindrical waves by a finite crack: an analytical solution
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