Local Shear-Wave Splitting
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(Left) Map of shear-wave splitting parameters for local events within the subducting slab. These phases sample only the crust of the overriding plate, the mantle wedge, and a small portion of the slab. Magnitudes of lag times range between approximately 0.1-0.4 seconds. Dots indicate earthquake epicenters from slab earthquakes utilized for splitting measurements (not all earthquakes yielded a measurement). From Anderson et al. (2004), Fall AGU Meeting. |
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Publications and Recent Abstracts INVITED Anderson, M. L., Zandt, G., 2004, Multiple layers of anisotropy in the Chile-Argentina subduction zone, South
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Last Updated: 01/2005