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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Bibliografiset tiedot
Päätekijät: А. А. Dobrynina, V. A. Sankov, J. Déverchère, V. V. Chechelnitsky
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Institute of the Earth's crust, Siberian Branch of RAS 2017-03-01
Sarja:Geodinamika i Tektonofizika
Aiheet:
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
Linkit:https://www.gt-crust.ru/jour/article/view/335
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