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1 Department of Earth, Atmospheric, and
Planetary Sciences
Massachusetts Institute of Technology
77 Massachusetts
Avenue
Cambridge, Massachusetts
02139
mlong{at}mit.edu
hilst{at}mit.edu
The goal of this study was to evaluate the performance of different splitting measurement techniques in the particularly complicated tectonic setting of subduction beneath Japan. We use data from the broadband Japanese F-net array and consider the methods of Silver and Chan (1991), Levin et al. (1999), and Chevrot (2000). We find that the results generally agree well, although discrepancies arise if the anisotropy beneath the station is more complex than the simple single-layer anisotropic model often assumed in splitting studies. A combination of multichannel and single-record methods may serve as a powerful tool for recognizing complexities and for characterizing upper-mantle anisotropy beneath a station.
This article has been cited by other articles:
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A. Sieminski, H. Paulssen, J. Trampert, and J. Tromp Finite-Frequency SKS Splitting: Measurement and Sensitivity Kernels Bulletin of the Seismological Society of America, August 1, 2008; 98(4): 1797 - 1810. [Abstract] [Full Text] [PDF] |
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