Factors influencing seismic wave attenuation in the lithosphere in continental rift zones

Attenuation of seismic waves in the crust and the upper mantle has been studied in three global rift systems: the Baikal rift system (Eurasia), the North Tanzanian divergence zone (Africa) and the Basin and Range Province (North America). Using the records of direct and coda waves of regional earthq...

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Bibliografische gegevens
Hoofdauteurs: А. А. Dobrynina, V. A. Sankov, J. Déverchère, V. V. Chechelnitsky
Formaat: Artikel
Taal:Engels
Gepubliceerd in: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017-03-01
Reeks:Геодинамика и тектонофизика
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Online toegang:https://www.gt-crust.ru/jour/article/view/335
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