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The oxygen isotopic composition of a stalactite from the Soreq Cave, Israel has been investigated by in situ high spatial resolution ion microprobe analysis. The δ 18 O record obtained on portions of the stalactite, which were deposited during the time interval of 18-14.3, 10.8-8.5 and 1.5-0.2 ka, has a temporal resolution ranging from ~1 to 25 years (depending on the deposition rate...
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