Complex anisotropy in D″ beneath the eastern Pacific from SKS-SKKS splitting discrepancies. Earth Planet. Sci. Lett. 283, 181-189.Long, M. (2009), Complex anisotropy in D″ beneath the eastern Pacific from SKS‐SKKS splitting discrepancies, Earth Planet. Sci. Lett., 283, 181-189, doi:...
SKKS-SKS and S3KS SKKS travel-time residuals have been computed with respect to the mean Earth model Preliminary Reference Earth Model (PREM), and corrected for ellipticity. The SKKS-SKS residuals plotted as a function of epicentral distance exhibit a general positive slope for distances greater ...
Differential travel times of SKS, SKKS and S3KS seismic phases are analysed to specify the structure of the outermost liquid core, which is poorly sampled by the PKP waves currently used for core tomography. The data are mainly broadband records at epicentral distances of 83-140°. They have ...
a new approach combines a derived from the minimisation approach for measuring shear-wave with an existing splitting combined approach we identify 30 SKS-SKKS event-station pairs as discrepant. These predominantly along a backazimuth range of 260° 290°. our results we interpret a region of aniso...
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Arrival times, amplitudes, and periods of the seismic phases SKS and SKKS have been investigated for shallow, intermediate, and deep earthquakes recorded at Pasadena and Huancayo, Peru. New observed time-distance curves are constructed for depths of <60, 100, 200, and 600 kilometers. Travel tim...
Difference traveltimes SKKS‐SKS for 12 Tonga‐Fiji events observed from 96‐117° at North and South American WWSSN and CSN stations exceed the difference times of standard earth model PREM by 2‐3 s. Also the amplitude ratios SKS/SKKS at American stations from 96‐107° are lower than the...
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