Mid-late Pleistocene glacial evolution in the Grove Mountains, East Antarctica, constraints from cosmogenic 10Be surface exposure dating of glacial erratic cobbles
This work was supported by the National Natural Science Foundation of China (Grant Nos. 41176166, 41230523, and 41271018). We are grateful to Jennifer C. H. Newall from Stockholm University and an anonymous reviewer for their thorough reviews that helped significantly improve this manuscript. The samples were processed in the Key Laboratory of Tibetan Environment Changes and Land Surface Process, Institute of Tibetan Plateau Research at Lhasa. We thank Baojin Qiao and Jinhua Liu from Institute of Tibetan Plateau Research, Chinese Academy of Sciences for their help in sample preparation. We appreciate Tom Clifton at PRIME lab, Purdue University for sample measurements. We thank George Burr from the University of Arizona and Xiangke Xu from Institute of Tibetan Plateau Research, Chinese Academy of Sciences for their constructive suggestions.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China; Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing, China; Shaanxi Provincial Key Laboratory of Accelerator Mass Spectrometry Technology and Application, National Center for Accelerator Mass Spectrometry in Xi'an, Xi'an, China; Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China; Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, China; Department of Physics and Astronomy, Purdue University, West Lafayette, United States; Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, United States
Recommended Citation:
Dong G.,Huang F.,Yi C.,et al. Mid-late Pleistocene glacial evolution in the Grove Mountains, East Antarctica, constraints from cosmogenic 10Be surface exposure dating of glacial erratic cobbles[J]. Quaternary Science Reviews,2016-01-01,145