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The geographical name of Monegros has traditionally been used to describe a high‐quality, dark‐coloured chert originating in a carbonate lacustrine environment, being one of the most important long‐distance tracers in south‐west Europe during prehistory. This chert type outcrops in the Monegros region, situated in the Ebro Basin (north‐eastern Iberia), but not only there, as cherts with the same descriptions are found in other regions, some far from the homonymous area. Nevertheless, prehistorians working on the characterization of lithic sources have frequently used the term 'Monegros' to define this chert, basing their attributions solely on macroscopic descriptions. These are not sufficient as they do not allow cherts from the Monegros region to be distinguished from cherts from other regions. In this study, the area where Monegros cherts outcrop was delimited and fieldwork was carried out to identify the origin of the geological formations and the preserved outcrops. The classic approach has proved to be insufficient for this purpose, so geochemical fingerprinting using energy‐dispersive X‐ray fluorescence (ED‐XRF) spectroscopy was performed. The results obtained after this first geochemical approach show that some differences can be found between the different formations in the Monegros region in terms of their major and minor components. [ABSTRACT FROM AUTHOR]

In the area around Angkor, Cambodia, several ceramics kilns dating from the ninth to 15th centuries ce have been discovered since 1995. The technical, typological and compositional characterization of their production has been one of the main goals of the Cerangkor Project. Samples of green‐glazed 'Kulen‐type' stoneware and non‐glazed stoneware produced in five kiln sites in the Angkor region were analysed chemically by wavelength‐dispersive X‐ray fluorescence spectrometry (WDS‐XRF) and also petrographically. The data indicate that some workshops used similar raw materials for the same types of ceramics, suggesting the exploitation of the same geological formations in the whole region. Several references groups were established for each type of stoneware offering an important database for future provenance studies of sherds from consumption sites. [ABSTRACT FROM AUTHOR]

This study characterizes the opacifiers and colouring agents used in the glazed bricks of Persepolis (mid-first millennium bc) and the Mannean site of Tepe Rabat in north-western Iran (eighth to seventh centuries bc). Various analytical studies show that lead antimonate and brizziite (NaSbO3) were used as the yellow and white opacifiers in the glazes of Persepolis and Tepe Rabat. Brizziite is shown to be incorporated in the white, green and turquoise glazes, and is also associated with lead antimonate and CaSb2O6 in some yellow and white opacifiers. The simultaneous formation of these opacifiers in one glaze might have been accidental. A possible connection between the Achaemenid glaze industry and the Mannean glaze production at Tepe Rabat is discussed. [ABSTRACT FROM AUTHOR]

Recently, large-scale production sites for the production of bifacial tools (axes and adzes) were discovered in the Judean desert. The waste piles have resulted from the numerous knapping procedures carried out at these sites, extend over thousands of square metres and include, in addition to the waste, a profusion of unfinished tools. The raw material procured for their fabrication is larnite-bearing rock. The larnite-bearing rock is extremely rare in the Levant. It occurs only in the exposures of the Hatrurim geological formation. The use of larnite for the production of chipped stone tools was entirely unknown until now. This newly discovered production area produced thousands of bifacial tools, the destination of which is as yet unknown. [ABSTRACT FROM AUTHOR]