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ABSTRACTS Minor and trace elements (K, Sr, Ba, Al, Fe, Mn, Si, Ti) have been measured in marbles from classical mediterranean quarries (Afyon, Denizli, Aphrodisias, Ephesus, Marmara and Carrara). A distinctive characterization of the classical marble sources by means of such chemical parameters seems very difficult, although some distinctions can be attempted between a few different areas and zones, within an area.
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