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CHARACTERIZATION OF LATE CHALCOLITHIC MICRO‐BEADS FROM ÇAMLIBEL TARLASI, NORTH‐CENTRAL ANATOLIA

2012/03/09 by C. PICKARD, Catriona Pickard, U.‐D. SCHOOP +1 · 1 citation
Chemistry · Earth and Planetary Sciences · Social Sciences · #Archaeology #Archaeology and Rock Art Studies #Archaeology and ancient environmental studies #Bead #Bronze Age #Chalcolithic #Characterization (materials science) #Chemistry #Composite material #Energy-dispersive X-ray spectroscopy #Geography #Geology #Indus #Materials science #Metallurgy #Microanalysis #Mineralogy #Nanotechnology #Pleistocene-Era Hominins and Archaeology #Scanning electron microscope #Talc

paper · doi:10.1111/j.1475-4754.2012.00672.x

openalex publication_date 2012/03/09 · openalex created_date 2025/10/10 · openalex updated_date 2026/05/21

Abstract

Micro‐bead manufacture is geographically widespread from the fifth millennium bc . Previous studies of comparable micro‐beads from sites in the Indus Valley region and the Near East suggest that many of these beads were formed from synthetic enstatite. Characterization of micro‐beads from the Late Chalcolithic site of Çamlıbel Tarlası was carried out by optical microscopy (OM), scanning electron microscopy (SEM) and microanalysis with energy‐dispersive X‐ray spectroscopy (EDS), and X‐ray diffraction analysis (XRD). The chemical composition of the micro‐beads analysed indicated that they were made from three distinctive materials; namely, bulk talc (i.e., synthetic enstatite precursor), apatite and mineral‐rich clay pastes.

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