The qaidam basin is the largest cenozoic sedimentary basin on the tibetan plateau, situated in the northeastern part of the plateau within qinghai province, northwestern china. The basin lies in a crescent. In this contribution we report on the chemical composition of salt lakes and inflows to the qaidam basin (analysis of 30 water samples collected in the summer of 2008 and 2009) together.
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A key motivation of our study is that the qaidam basin is one of the few places in the. 3 with an elevation of around 3,000 m (10,000 ft), qaidam forms a kind of. The basin covers an area of approximately 120,000 km 2.
The qaidam basin is the northeastern section of the plateau of tibet, occupying the northwestern part of qinghai province, western china.
The qaidam, tsaidam, or chaidamu basin is a hyperarid basin that occupies a large part of haixi prefecture in qinghai province, china. The qaidam basin is located at the northern margin of the tibetan plateau, the largest tectonic feature on the earth. Qaidam basin is china’s highest and most evaporative inland basin situated in the border area of the provinces of qinghai, gansu and the autonomous region of xinjiang.
