Articles | Volume 11, issue 1
https://doi.org/10.5194/se-11-161-2020
© Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.
Research article
| 
29 Jan 2020
Research article |
| 29 Jan 2020
| 29 Jan 2020
The relative contributions of scattering and viscoelasticity to the attenuation of S waves in Earth's mantle
Related subject area
Subject area: Core and mantle structure and dynamics | Editorial team: Seismics, seismology, paleoseismology, geoelectrics, and electromagnetics | Discipline: Geophysics
Second-order scalar wave field modeling with a first-order perfectly matched layer
Solid Earth, 9, 1277–1298, 2018
Cited articles
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Choy, G. and Cormier, V. F.: Direct measurement of the mantle attenuation operator from broadband P and S waves, J. Geophys. Res., 91, 7326–7342, 1986.
Cormier, V., Li, X., and Choy, G.: Seismic attenuation of the inner core: Viscoelastic or stratigraphic?, Geophys. Res. Lett., 25, 4019–4022, 1998.
Cormier, V. F.: D′′ as a transition in the heterogeneity spectrum of the lowermost mantle, J. Geophys. Res.-Sol. Ea., 105, 16193–16205, 2000.
Cormier, V. F., Tian, Y., and Zheng, Y.: Heterogeneity spectrum of Earth's upper mantle obtained from the coherence of teleseismic P waves, Commun. Comput. Phys., https://doi.org/10.4208/cicp.OA-2018-0079, online first, 2019.
