“…Gosse and Phillips, 2001;Niedermann, 2002) and the rock density, ρ = 3.0 g/cm 3 (e.g. Maré and Cole, 2006 He production rates normalised to sea level and latitudes > 60 º are given in Table 3. These values were calculated on a sample specific basis, through the application of the mineral chemistry-dependent production rates proposed by Fenton…”