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2006) is irrelevant for this study as discussed in Scaillet Monitoring of the instrumental mass-fractionation is achieved by daily calibration of the atmospheric 40 Ar/ 36 Ar isotope ratio on air shots interspersed with the unknowns at different peak intensities to correct for nonlinearity and counting dead-time (for every isotope) using in-house software The mass discrimination factor varied between 0.9984 ± 0.0016 (2#) and 0.9967 ± 0.0016 (2#) pmu, assuming a linear mass-bias law. Unless otherwise stated, age errors are plotted and tabulated at 2! and include corrections for (1) counting dead-time for every isotope, ) system blanks, (3) massdiscrimination , (4) post-irradiation decay of 39 Ar, 37 Ar, and 36 Cl) isotope interference corrections from K, Ca and Cl) neutron-flux gradients, and (8) monitor's age error. Additional references not cited in main text, 2008. ,
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Ar dating of the Green Tuff, Pantelleria ,
URL : https://hal.archives-ouvertes.fr/insu-00862611