The lack of strong splitting of seismic shear waves below central Nevada is in marked contrast to the surrounding region. Seismic data and numerical experiments suggest that a skinny, cylindrical drip of lithosphere may be to blame.
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References
Jones, C. H. et al. Tectonophysics 213, 57–96 (1992).
West, J. D., Fouch, M. J., Roth, J. B. & Elkins-Tanton, L. T. Nature Geosci. 2, 439–444 (2009).
Houseman, G. A. & Molnar, P. Geophys. J. Int. 128, 125–150 (1997).
Savage, M. K. & Sheehan, A. F. J. Geophys. Res. 105, 13715–13734 (2000).
Zandt, G. & Humphreys, E. Geology 36, 295–298 (2008).
Burdick, S. et al. Seismol. Res. Lett. 79, 384–392 (2008).
Yang, Y. & Ritzwoller, M. H. Geophys. Res. Lett. 35, L04308 (2008).
Saltus, R. W. & Thompson, G. A. Tectonics 14, 1235–1244 (1995).
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Schulte-Pelkum, V. Draining Nevada. Nature Geosci 2, 381–382 (2009). https://doi.org/10.1038/ngeo532
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DOI: https://doi.org/10.1038/ngeo532
