Supplementary Figure 1 and Table 1 for Cenozoic exhumation of the Qilian Shan in the northeastern Tibetan Plateau: Evidence from low-temperature thermochronology

Supplementary Fig.1 is apatite (U-Th)/He ages versus effective uranium content [eU] for the samples collected from the transects in the Qilian Shan region. There are no clear relationships with the effective Uranium（eU）and (U-Th)/He ages suggesting that the ages do not affect by (eU).
Supplementary Table 1 is Thermal history model input table for simulations of low-temperature transects collected from the eastern Qilian Shan. For the geological constraints, the present surface temperature was set to 10 ± 10 °C; the geothermal gradient was in the range of 30 ± 30 °C/km. We did not impose any other temperature constraint for all modeling samples

补充图1展示了采自祁连山地区各剖面的样品的磷灰石（apatite）（U-Th）/He年龄与有效铀含量（eU）的对应关系。二者未呈现明确的相关关系，表明该年龄不受有效铀（eU）的影响。
补充表1为针对采自祁连山东部的低温剖面开展热史模拟所用的热史模型输入表。在地质约束条件中，现今地表温度设置为10±10℃；地热梯度取值范围为30±30℃/km。本次所有模拟样品均未施加其他温度约束条件。