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[4]
Magnetostratigraphy of the late Cenozoic Laojunmiao anticline in the northern Qilian Mountains and its implications for the northern Tibetan Plateau uplift[J]. FANG Xiaomin1,2, ZHAO Zhijun3,2, LI Jijun2, YAN Maodu2, PAN Baotian2, SONG Chunhui2 & DAI Shuang2 1. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China;2. Key Laboratory of Western China’s Environmental Systems, Ministry of Education & College of Resources and Environment, Lanzhou University, Lanzhou
[5]
The vegetation and climate change during Neocene and Early Quaternary in Jiuxi Basin, China[J]. MA Yuzhen 1 , FANG Xiaomin 1,2 , LI Jijun 1 , WU Fuli 1 & ZHANG Jun 1 1. Key Laboratory of Western China’s Environmental Systems and College of Resources and Environment, Lanzhou University, Lanzhou 730000, China;2. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China.Science in China(Series D:Earth Sciences). 2005(05)
[7]
Paleomagnetic dating of the topmost terrace in Kouma,Henan and its indication to the Yellow River’s running through Sanmen Gorges[J]. PAN Baotian1, WANG Junping1, GAO Hongshan1, GUAN Qingyu1, WANG Yong1, SU Huai1, LI Bingyuan2 & LI Jijun1 1. Key Laboratory of Western China’s Environmental Systems, Ministry of Education, and Department of Geography, Lanzhou University, Lanzhou 730000, China;2. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences (CAS), Beij
[8]
Geomorphologic evidence of phased uplift of the northeastern Qinghai-Tibet Plateau since 14 million years ago[J]. LU Huayu1, WANG Xiaoyong1, AN Zhisheng1, MIAO Xiaodong1, ZHU Rixiang3, MA Haizhou2, LI Zhen4, TAN Hongbing2 & WANG Xianyan1 1. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075 China;2. Qinghai Institute of Salt Lakes, Chinese Academy of Sciences. Xining 810008, China;3. Institute of Geology and Geophysics,