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

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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Bibliographic Details
Main Authors:	А. А. Dobrynina, V. A. Sankov, J. Déverchère, V. V. Chechelnitsky
Format:	Article
Language:	English
Published:	Institute of the Earth's crust, Siberian Branch of RAS 2017-03-01
Series:	Geodinamika i Tektonofizika
Subjects:	baikal rift system east african rift system north american basin and range province attenuation of seismic waves seismic quality factor seismicity coda waves intrinsic attenuation scattering attenuation heat flow
Online Access:	https://www.gt-crust.ru/jour/article/view/335

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