Abstract

Concentration and isotopic composition of He, Ne and Ar have been measured in 14 samples from 12 locations along a 35 cm long drill core through the geometrical center of the 271-kg amphoterite St. Severin. The concentrations of spallogenic 3He and 21Ne increase with depth by about 14% and 35%, respectively. The observed data are in agreement with the model for production of spallogenic nuclides given by Trivedi and Goel (1973). The spallogenic 20Ne/ 22Ne ratio is constant (0.84 ± 0.01), whereby the 22Ne/ 21Ne correlates with the 3He/ 21Ne. This relation can be used to correct the depth effect of noble gas production rates. All measurements of the core are thus in agreement with an exposure age of 10.8 ± 0.2 m.y.

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