This page bundles the available data for the qaidam (tsaidam) basin in the china. The basin lies in a crescent. Those sediments represent a unique archive of the evolution of the.
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The basin covers an area of approximately 120,000 km2. 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. The qaidam basin has recorded the uplift of the plateau with its complete cenozoic sequences.
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.
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 the largest cenozoic sedimentary basin on the tibetan plateau, situated in the northeastern part of the plateau within qinghai province, northwestern china. The qaidam, tsaidam, or chaidamu basin is a hyperarid basin that occupies a large part of haixi prefecture in qinghai province, china. The images are hyperlinks and will open up a separate window with a high resolution pdf image of the map.
The qaidam basin is the northeastern section of the plateau of tibet, occupying the northwestern part of qinghai province, western china. The basin covers an area of approximately 120,000 km 2. As the largest depression in the tibetan plateau, the qaidam basin preserves over 10 km thick of cenozoic sediments.
