Comparative study of deep structures by means of passive microseismic sounding and seismic tomography

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Abstract

Modern surface wave–based approaches to the deep sounding of the Earth are compared, along with results from reconstructing deep structure of the Hawaiian plume, obtained by phase and amplitude methods. Ways of further improving these methods are proposed.

About the authors

R. A. Zhostkov

Schmidt Institute of Physics of the Earth

Author for correspondence.
Email: shageraxcom@yandex.ru
Russian Federation, Moscow, 123995

D. A. Presnov

Schmidt Institute of Physics of the Earth

Email: shageraxcom@yandex.ru
Russian Federation, Moscow, 123995

A. S. Shurup

Schmidt Institute of Physics of the Earth; Faculty of Physics

Email: shageraxcom@yandex.ru
Russian Federation, Moscow, 123995; Moscow, 119991

A. L. Sobisevich

Schmidt Institute of Physics of the Earth

Email: shageraxcom@yandex.ru
Russian Federation, Moscow, 123995

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