Lithospheric structure of the Arabian Shield from the joint inversion of receiver functions and surface-wave group velocities

By J. Julià, C. Ammon, R. Herrmann. 2003

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Crustal structure of the Arabian Plate: New constraints from the analysis of teleseismic receiver functions (2005, background): “The significant variations (~ 10 km) in crustal thickness values at stations YNBS and LTHS receiver functions may be the result of lateral variations along the Red Sea, and the fact that they are located in terranes of oceanic affinity where the crust-mantle transition have been observed to be gradu”
Transdimensional inversion of receiver functions and surface wave dispersion (2012, methodology): “…increasing computational power, methods to jointly invert RF and SWD are gaining in popularity [e.g., Özalaybey et al., 1997; Du and Foulger, 1999; Juliá et al., 2000, 2003; Chang et al., 2004; Lawrence and Wiens, 2004; Yoo et al., 2007; Tkalčić et al., 2006; Moorkamp et al., 2010; Tokam et al.,…”