Abstract
Pyroclastic deposits on Anafi Island, Cyclades, Greece, were initially related to the Minoan eruption (1613 BC), but later geochemical studies favored an older chronology that points at the Lower Pumice eruption of Santorini (172 ka). Here we attempt through OSL dating to provide a minimum age by dating sand-sized quartz from colluvium overlying the deposits. The chronological results excluded the possibility of being Minoan.
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