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Bulletin of the Seismological Society of America; February 2006; v. 96; no. 1; p. 348-354; DOI: 10.1785/0120040086
© 2006 Seismological Society of America
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QLg Distribution in the Basin and Range Province of the Western United States

Ghassan I. Aleqabi1 and Michael E. Wysession1

1 Department of Earth and Planetary Sciences
Washington University
St. Louis, Missouri 63130-4899


Figure 001
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  		Figure 1. Ray paths used in the tomographic inversion. Earthquakes are represented by diamonds, NTS explosions by circles, and Lawrence Livermore National Laboratory stations by triangles. Numbers indicate each event identification number (table 3 in Al-Eqabi et al., 2001).

 

Figure 002
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  		Figure 2. Figure 002 from tomographic inversion of Lg amplitudes. Darker shades represent areas of relatively high Figure 002, and lighter shades show areas of low Figure 002, which probably indicates high crustal temperatures. The shades and Figure 002 contour lines are superimposed on a topography gradient map; dashed boundaries distinguish various tectonic provinces.

 




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