“…XRF has been most commonly applied to ceramic assemblages, including collections from Africa (Aronson et al, 1994;Jacobson et al, 2002), Syria (Bakraji, 2004), Turkey (Birgul et al, 1979), the Roman Empire (Devereaux et al, 1983), prehistoric North America (Elam et al, 1992), the Middle East (Grave et al, 1996), the Mediterranean (Grimanis et al, 1980), Mesoamerica , and ancient China (Yap and Tang, 1985), to name but a few applications (see also Bertin, 1975;Garrison, 2003;Herz, 2003;Whitbread, 2001 for summaries of trace element studies of ceramics and lithics). Less commonly, XRF has been applied to lithic materials, most commonly obsidian (e.g., Kunselman, 1991Kunselman, , 1998 since volcanic outcrops can vary significantly in terms of trace element chemistry over relatively short distances, and less often to non-volcanic materials (e.g., Jones et al,1996).…”