The Altun Mountains is a collisional orogenic belt strongly modified by strike-slip-faults, constituting the current northern tectonic boundary of Qinghai-Tibetan Plateau. Its uplift is remarkable part of the Cenozoic uplift of Qinghai-Tibetan Plateau. This contribution presents LA-ICP-MS U-Pb dating results of detrital zircons, together with heavy mineral assemblages from sandstones of the Xiaganchaigou Formation and lower segment of the Xiayoushashan Formation from northwest Qaidam Basin. The results show that there are significant Indosinian and Caledonian age populations in all samples. However, significant differences in age spectrums exist between the samples from Xiaganchaigou Formation ages and those from Xiayoushashan Formation.
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