Fig. 7
From: Plio-Pleistocene landscape evolution in Northern Switzerland
Envelope of apatite fission track age scatter, as shown in Fig. 6, fitted to cooling ages (from Mazurek et al. 2006) from the apatite partial annealing zone (APAZ) of three boreholes in the Molasse foreland basin: a Herdern; b Hünenberg; c Boswil. The potential missing overburden is estimated using the method explained in Fig. 6