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Fig. 1 | Journal of Analytical Science and Technology

Fig. 1

From: Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect

Fig. 1

Normal behavior of Ar isotopes during measurement. All isotope signals are expected to decrease (left) due to the ionization by electron bombardment in the ion source chamber. For samples with small Ar contents (right), the increasing trends are prominent. The red numbers represent the variation of each isotope signal at the beginning and end of the analysis

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