Aeolian Facies Belts in the Taklimakan Desert   总被引：4，自引：0，他引：4  

Li Baosheng  Dong Guangrong  Zhang Jiasheng  Li Sen  Jin Heling  Chen Huizhong  Wen Xiangle  Wang Yao  Lanzhou Desert Research Institute  Chinese Academy of Sciences  Lamhou  Gansuand Zhu YizhiXi''an Open Laboratory of Loess  Quaternary Geology  Chinese Academy of Sciences  Xi''an  Gansu Fei Zhenbi 《《地质学报》英文版》1995,69(3)

At least at the beginning of the last glacial epoch, the facies belts of dune sand, sandy loam and loess formed by winds had existed in the Taklimakan desert and areas south of it. There were no appreciable changes in the NE and NW wind systems and their wind fqrces that deposited dune sand, sandy loam and loess in the global cold stage since the last glacial epoch (accordingly no marked shifts of the boundaries of these aeolian facies belts took place. In the global warm stage since then, the climate in the Taklimakan desert and areas south of it became warm and dry, resulting in ablation of substantial volumes of ice and snow in their surrounding mountains and thus forming alluvial and diluvial deposits in the region. The alluvial-diluvial actions, however, failed to change the general framework of aeolian facies belts.  相似文献