supported by the National Department Public Benefit Research Foundation of China(grant No.201211077);National Natural Science Foundation of China(Grant No.40802033)
The eolian deposits distributed in the river valleys in the eastern margin of the Tibetan Plateau (TP) are very useful in neotectonic and paleoclimatic studies. Firstly, the climate in the eastern margin of the TP i...
supported by projects of Re’nacuo 1:50000 regional geological survey and State Key Laboratory of Biogeology and Environmental Geology(GBL2135)
The sedimentary sequences since 33 ka B.P. to 10 ka B.P. have been established in the Re'nacuo-Lake, Gaize area of north Tibet, through a study of a lacustrine section. The climate since 33 ka B.P. to 10 ka B.P. may ...
support was provided by the National Science Foundation of China grant (40472088)
Based on the study of magnetostratigraphy,magnetic susceptibility and grain size of Garze A section on the southeastern margin of the Qinghai-Tibetan Plateau since the late early-Pleistocene,the basal age of Garze loe...
The paper discusses the distribution of Quaternary sediments, occurrence of saline minerals and phases of neotectonic movements and their manifestations in the Qaidam basin. The formation of four successive lacustrine...