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“Cryptic” diagenesis and its implications for speleothem geochronologies
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文摘

Isolated domains in apparently pristine speleothems can show open system behavior.

“Cryptic” diagenesis with very localized U-loss is observed in a Holocene speleothem.

Misinterpretation of U-Th age estimates in such samples can only be eliminated based on multi-aliquot age determinations.

Micro-CT scans recorded a limited number of voids in otherwise dense speleothem.

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