It is a major continuous depocenter in Dalangtan area,western Qaidam basin since Early Cenozoic,which is most important Neogene salt deposits center in Qaidam basin.The Miocene Saline lake was developed firstly
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机译:Comment on "Magnetostratigraphic study of the Kuche Depression, Tarim Basin, and Cenozoic uplift of the Tian Shan Range, Western China" Baochun Huang, John DA Piper, Shoutao Peng, Tao Liu, Zhong Li, Qingchen Wang, Rixiang Zhu [Earth Planet. Sci. Lett
机译:Comment on "Magnetostratigraphic study of the Kuche Depression, Tarim Basin, and Cenozoic uplift of the Tian Shan Range, Western China" Baochun Huang, John DA Piper, Shoutao Peng, Tao Liu, Zhong Li, Qingchen Wang, Rixiang Zhu [Earth Planet. Sci. Lett., 2006, doi : 10.1016/j.epsl.2006.09.020]