作者单位：
1] Institute of Cenozoic Geology and Environment, State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, X'ian 710069, China [2] State Key laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, X'ian 710075, China.
[1]
1] Institute of Cenozoic Geology and Environment, State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, X'ian 710069, China [2] State Key laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, X'ian 710075, China [3] Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China.
[2]
1] Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China [2] Institute of Cenozoic Geology and Environment, State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, X'ian 710069, China.
[3]
DOI
10.1038/srep09706
PMID
25913292
发布时间
2018-11-13
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