Dating buried glacier ice using cosmogenic 3He in surface clasts: Theory and application to Mullins Glacier, Antarctica
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文摘

Cosmogenic nuclide accumulation in clasts transported by glacier ice is examined.

A modeling framework captures nuclide variability from various exposure pathways.

Surface clasts display a wide range of nuclide concentrations.

Nuclide concentrations are used to model a range of ice ages.

Application of modeling framework suggests ice in Mullins Glacier exceeds 1.6 Ma.

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