From freshwater inflows to salt lakes and salt deposits in the Qaidam Basin, W China
Abstract The Qaidam basin in W China is an immense hyperarid intramontane basin with flat vast playas and salt lakes on the Qinghai-Tibet Plateau. The central basin is about 2800–2900 m a.s.l. elevation and enclosed by mountain ranges reaching > 5800 m in the Qilian Mountains and > 6200 m in t...
Main Authors: | I. Stober, J. Zhong, K. Bucher |
---|---|
Format: | Article |
Language: | English |
Published: |
SpringerOpen
2023-05-01
|
Series: | Swiss Journal of Geosciences |
Subjects: | |
Online Access: | https://doi.org/10.1186/s00015-023-00433-4 |
Similar Items
-
Halogenases of Qarhan Salt Lake in the Qaidam Basin: Evidence From Halite Fluid Inclusions
by: Jun Li, et al.
Published: (2021-06-01) -
Origin and evolution of intercrystalline brine in the northern Qaidam Basin based on hydrochemistry and stable isotopes
by: Qianhui Ren, et al.
Published: (2023-01-01) -
Origin of the Dolomitic Ooids Formed in the Pliocene Shizigou Formation in the Qaidam Basin, Northern Tibet Plateau and Implications for Climate Change
by: Lewei Hao, et al.
Published: (2022-12-01) -
Lake Expansion under the Groundwater Contribution in Qaidam Basin, China
by: Xi Zhang, et al.
Published: (2022-04-01) -
Detailed Processes and Potential Mechanisms of Pliocene Salty Lake Evolution in the Western Qaidam Basin
by: Qingda Su, et al.
Published: (2021-09-01)