Mapping Crustal Shear Wave Velocity Structure and Radial Anisotropy Beneath West Antarctica Using Seismic Ambient Noise
Using 8- to 25-s-period Rayleigh and Love wave phase velocity dispersion data extracted from seismic ambient noise, we (i) model the 3-D shear wave velocity structure of the West Antarctic crust and (ii) map variations in crustal radial anisotropy. Enhanced regional resolution is offered by the UK A...
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Format: | Text |
Language: | unknown |
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ScholarWorks@CWU
2019
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Online Access: | https://digitalcommons.cwu.edu/cotsfac/100 https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1100&context=cotsfac |