Lacustrine Sedimentary Sequences and Palaeoclimatic Change in the Hinterland of the Qinghai-Tibet Plateau

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Lacustrine Sedimentary Sequences and Palaeoclimatic Change in the Hinterland of the Qinghai-Tibet Plateau
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During the comprehensive scientific investigations of the Qinghai - Tibet Plateau, sedimentary records of the sections of its hinterland were selected to conduct studies of stratigraphic climatology and isotope climatology. The response characteristics of

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Hu Dongsheng Zhang Huajing Li Bingyuan Wen JingchunCollege of Land, Hunan Normal University, Changsha,,College of Chemistry, Chemical Engineering, Hunan Normal University, Changsha,,Institute of Geography, Chinese Academy of Sciences, Beijing,.2000. Lacustrine Sedimentary Sequences and Palaeoclimatic Change in the Hinterland of the Qinghai-Tibet Plateau[J]. Acta Geologica Sinica,74(4):

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