S-wave velocity structure beneath the Kaapvaal Craton from surface-wave inversions compared with estimates from mantle xenoliths
Results from two-station surface-wave inversions across the Archean Kaapvaal craton of southern Africa are compared with seismic velocities estimated from approximately 100 mantle xenoliths brought to the surface in kimberlite pipes. As the xenoliths represent a snapshot of the mantle at the time of...
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Virginia Tech
2014
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| Online Access: | http://hdl.handle.net/10919/34200 http://scholar.lib.vt.edu/theses/available/etd-07272004-145628 |