“…Although release temperatures for Ne and Xe in these common minerals are currently uncertain, on the basis of their diffusivity decrease with increasing atomic numbers [ Ozima and Podosek , 2002], it is reasonable to assume that Ne release temperatures will fall between those of He and Ar (e.g., ∼70–250°C), while Xe release temperatures are expected to be greater than those of Ar (e.g., >275°C). These assumptions are supported by the increasing release temperatures for 4 He, 21 Ne, 84 Kr, and 136 Xe in zircons [ Honda et al , 2004; Gautheron et al , 2006], as well as the observed Xe release temperature in meteorites, which was shown to be greater than that of Ar [ Burkland et al , 1995]. Because of its currently low geothermal gradient (∼19°C/km) [ Vugrinovich , 1989], fluid temperatures in most of our sampled formations in the Michigan Basin are ∼40–80°C, far lower than release temperatures required for 40 Ar and 136 Xe.…”