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


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Resumo

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.

Sobre autores

R. Zhostkov

Schmidt Institute of Physics of the Earth

Autor responsável pela correspondência
Email: shageraxcom@yandex.ru
Rússia, Moscow, 123995

D. Presnov

Schmidt Institute of Physics of the Earth

Email: shageraxcom@yandex.ru
Rússia, Moscow, 123995

A. Shurup

Schmidt Institute of Physics of the Earth; Faculty of Physics

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

A. Sobisevich

Schmidt Institute of Physics of the Earth

Email: shageraxcom@yandex.ru
Rússia, Moscow, 123995

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