@article{224e79a9fa384f0d8f805ca307ae02e6,
title = "Comparing ray-theoretical and finite-frequency teleseismic traveltimes: Implications for constraining the ratio of S-wave to P-wave velocity variations in the lower mantle",
keywords = "Body waves, Composition and structure of the mantle, Seismic tomography, Wave propagation",
author = "Chaves, {Carlos A.M.} and Jeroen Ritsema and Paula Koelemeijer",
note = "Funding Information: The facilities of IRIS Data Services, and specifically the IRIS Data Management Center, were used for access to waveforms, related metadata, and/or derived products used in this study. IRIS Data Services are funded through the Seismological Facilities for the Advancement of Geoscience (SAGE) Award of the National Science Foundation under Cooperative Support Agreement EAR- 1851048. All figures were produced using the GMT software (Wessel et al. 2013). This research has been supported by FAPESP grants 2014/17779-3 and 2016/11580-6 to CC, NSF grant EAR- 1416695 to JR and a Junior Research Fellowship from University College Oxford and a Royal Society University Research Fellowship (URF\R1\180377) to PK. The authors acknowledge computing time provided on the Blue Gene/Q and DaVinci supercomputers supported by the CRC (Rice University) and LCCA (University of S?o Paulo) agreement and on the AGUIA supercomputer supported by HPC-STI (University of S?o Paulo). The SPECFEM3D Globe software has provided the Computational Infrastructure for Geodynamics (CIG). All data used in this study are available by contacting the corresponding author at
[email protected]. We thank editor Ian Bastow, Satoru Tanaka, and an anonymous reviewer for helpful comments. Publisher Copyright: {\textcopyright} The Author(s) 2020. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.",
year = "2021",
month = mar,
doi = "10.1093/gji/ggaa534",
language = "English",
volume = "224",
pages = "1540--1552",
journal = "Geophysical Journal International",
issn = "0956-540X",
publisher = "Wiley-Blackwell",
number = "3",
}