The continental lithosphere: Reconciling thermal, seismic, and petrologic data

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On the origin of the asthenosphere (2012, background): “Temperature of ~1300 K would correspond to a depth of ~100–150 km in the typical old continental upper mantle (e.g., Artemieva, 2009).”
3-D shear wave radially and azimuthally anisotropic velocity model of the North American upper mantle (2011, background): “…in a depth range that falls consistently within the range of lithosphere thickness estimated from seismic, petrologic, electrical and geothermal inversion studies (Jones et al. 2001; van der Lee 2002; Grifﬁn et al. 2004; Moorkamp et al. 2007; Artemieva 2009; Eaton et al. 2009; Miller & Eaton 2010).”