Late Holocene Moisture Changes in the Core Area of Arid Central Asia Reflected by Rock Magnetic Records of Glacier Lake Kalakuli Sediments in the Westernmost Tibetan Plateau and their Influences on the Evolution of Ancient Silk Road
WU Xudong LIU Xingqi Erwin APPEL
地质学报(英文版)2020,Vol.94Issue(3):658-667,10.
地质学报(英文版)2020,Vol.94Issue(3):658-667,10.
Late Holocene Moisture Changes in the Core Area of Arid Central Asia Reflected by Rock Magnetic Records of Glacier Lake Kalakuli Sediments in the Westernmost Tibetan Plateau and their Influences on the Evolution of Ancient Silk Road
Late Holocene Moisture Changes in the Core Area of Arid Central Asia Reflected by Rock Magnetic Records of Glacier Lake Kalakuli Sediments in the Westernmost Tibetan Plateau and their Influences on the Evolution of Ancient Silk Road
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moisture changes/rock magnetic records/Kalakuli Lake/Arid Central Asia/Ancient Silk RoadKey words
moisture changes/rock magnetic records/Kalakuli Lake/Arid Central Asia/Ancient Silk Road引用本文复制引用
WU Xudong,LIU Xingqi,Erwin APPEL..Late Holocene Moisture Changes in the Core Area of Arid Central Asia Reflected by Rock Magnetic Records of Glacier Lake Kalakuli Sediments in the Westernmost Tibetan Plateau and their Influences on the Evolution of Ancient Silk Road[J].地质学报(英文版),2020,94(3):658-667,10.基金项目
We thank Dr. Qi Zhang for her assistance in the laboratory. This work is granted by National Key Research and Development Programme of China (Grant No. 2018YFA0606400), the National Natural Science Foundation of China (Grant No. 41502165 and 41572338) and China Scholarship Council (CSC). (Grant No. 2018YFA0606400)