FIGURE 1. Dhok Saira paleomagnetic log (with leporid localities) based on a stratigraphic section southeast of Padhri, northern Pakistan. This log, which correlates to chrons C4n.2n through C3An.2n, is the basis for dating the deposits in the Hasnot area (after Barry et al. 2002; magnetostratigraphic time scale of Gradstein et al. 2004).