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Intracontinental extension in central China is accommodated by Cenzoic grabens flanking the Ordos Block,such as the Weihe graben,which accommodate 5-6 mm/yr of extension.To define the onset and evolution of major Cenozoic extension,we examine the cooling history of exhumed footwall rocks in the North Qinling range adjacent to the Weihe graben.We present results from 47 new apatite fission track (AFT) samples – primarily from two vertical transects of 1.5-2.5 km relief located on the northern flank of the North Qinling footwall.