Bulletin of the Seismological Society of America
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Bulletin of the Seismological Society of America; February 2006; v. 96; no. 1; p. 165-175; DOI: 10.1785/0120050082
© Seismological Society of America
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Figure 002


Figure 2. (a) Locations of two deep-borehole sites, SHM and FCH. The borehole array recordings from these sites are used for investigating the coherency characteristics of P waves. The data from events whose locations are shown by open triangles and open circles are used for stations SHM and FCH, respectively. (b) Locations of six borehole sites, SHM, FCH, IWT, EDZ, NRT, and ENZ. The borehole array recordings from these sites are used for investigating the coherency characteristics of SH waves. The data from events whose locations are shown by open triangles, open circles, open squares, open reverse triangles, open rhombuses, and solid circles are used for stations SHM, FCH, IWT, EDZ, NRT, and ENZ, respectively.





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