Variation of Shear-wave Residuals and Splitting Parameters from Array Observations in Southern Tibet
—A tight array of seismographs spanning a 500 km traverse of southern Tibet resolved anisotropy from SKS with a spatial variation of its direction and an increase northward of the splitting delay, as well as of its first arrival residual. Both waves split by velocity anisotropy are slow relative to...
|Published in:||Pure and Applied Geophysics : pageoph, Vol. 151, No. 2/4 (1998), p. 407-431|
|Other Involved Persons:||; ;|
|Item Description:||Received November 1, 1996, revised July 1, 1997, accepted July 5, 1997|
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