Cosmogenic 21Ne concentrations and exposure ages of summit bedrocks in the Grove Mountains, Antarctica

Various sources of 21 Ne and 22 Ne exist in surface rocks: cosmogenic, in situ nucleogenic from internal U and Th, trapped crustal nucleogenic and trapped atmospheric. This paper reports the first measurement, in China, of cosmogenic 21 Ne and 22 Ne in surface bedrocks. We developed a unique sample...

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Veröffentlicht in:Science China. Earth sciences 2010-04, Vol.53 (4), p.518-521
Hauptverfasser: Kong, Ping, Ding, Lin, Lai, QingZhou, Huang, FeiXin
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description Various sources of 21 Ne and 22 Ne exist in surface rocks: cosmogenic, in situ nucleogenic from internal U and Th, trapped crustal nucleogenic and trapped atmospheric. This paper reports the first measurement, in China, of cosmogenic 21 Ne and 22 Ne in surface bedrocks. We developed a unique sample pre-treatment procedure that effectively removed inclusions inside quartz grains, and thus maximally reduced nucleogenic contributions of 21 Ne and 22 Ne. Step-heating experiments show that concentrations of cosmogenic 21 Ne and 22 Ne in summit bedrock samples R9202 and R9203 from Grove Mountains, Antarctica, are (3.83±0.87)×10 8 and (5.2280.51)×10 8 atoms/g, respectively. The corresponding minimum exposure ages are 2.2±0.5 and 3.0±0.3 Ma. This indicates that the ice sheet in East Antarctica was uncovered the crest of Mount Harding, a typical nunatak in Grove Mountains, since at least mid-Pliocene.
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subjects Earth and Environmental Science
Earth Sciences
Experiments
Ice
Measurement techniques
Mountains
Pliocene
Quartz
Research Paper
title Cosmogenic 21Ne concentrations and exposure ages of summit bedrocks in the Grove Mountains, Antarctica
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