Taking into Account the Influence of Relief in the Method of Microseismic Sounding


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The traveling of surface waves in a model geophysical medium with a nonsmooth boundary is studied. It is shown that relief significantly distorts the microseismic noise field recorded at the day surface. This result should be taken into consideration when interpreting the data of passive surface-wave geophysical studies of deep crustal inhomogeneities.

Sobre autores

A. Sobisevich

Schmidt Institute of Physics of the Earth

Email: shageraxcom@yandex.ru
Rússia, Moscow, 123810

R. Zhostkov

Schmidt Institute of Physics of the Earth

Autor responsável pela correspondência
Email: shageraxcom@yandex.ru
Rússia, Moscow, 123810

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