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Imaging Upper-Mantle Structure under USArray using Long-period Reflection Seismology

The USArray seismic data have led to greatly improved images of upper-mantle structure under the contiguous United States, both from tomography to invert for volumetric heterogeneity and receiver-function studies to probe mantle discontinuities.  Here I introduce an alternative approach to imaging mantle discontinuities that exploits long-period S-wave reflections seen in teleseisms.    Analysis of USArray transverse-component data from 3250 earthquakes shows clear reflections off the 410- and 660-km discontinuities, which can be used to map the depth and brightness of these features.  We also observe intriguing reflectors at shallower depths in many regions, including a negative polarity reflection that may delineate the top of the lithosphere-asthenosphere boundary (LAB) in some areas.  We observe a dipping reflector in the west that aligns with the top of the high-velocity Farallon slab anomaly seen in some tomography models, but which also may be an artifact caused by near-surface scattering of incoming S waves.

Speaker: Peter Shearer, UC San Diego

Room 350/372

Thursday, 05/16/19


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Mitchell Earth Sciences Building (04-560)

397 Panama Mall
Stanford University
Stanford, CA 94305