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Comment on: 'Can horizontal P waves be trapped and resonate in a shallow sedimentary basin?' by F. J. Sácnhez-Sesma and F. LuzÓ
Authors:J. L. Mateos  O. Novaro  T. H. Seligman  J. Flores
Affiliation:Instituto de Fisica, Universidad Nacional Autónoma de México, Apartado Postal 20–364, 01000 México, DF, México;Laboratorio de Cuernavaca, Instituto de Fisica, Universidad Nacional Autónoma de México, Apartado Postal 139-B, 62190 Cuernavaca, Morelos, México;Centro Universitario de Comunicación de la Ciencia, Universidad Nacional Autónoma de México, Apartado Postal 70–487, 04510 México, DF, México
Abstract:
We show that most of the arguments in the above paper are either incorrect or irrelevant to the point the authors are trying to make. We show that their results have no bearing on the model proposed by our group, as they claim. They discuss the seismic response of a valley with a 2-D trapezoidal cross-section in a vertical plane, whereas we dealt with a closed basin with a 2-D cross-section but of arbitrary geometry and in the horizontal plane. Even more significantly, the width of the valley they use is much smaller than the wavelength of the horizontal P waves that can resonate, thereby precluding any possibility of them being trapped. Therefore, their arguments do not clarify the issue posed in the title of their article.
Keywords:P waves    sedimentary basins
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