Mathematics
Logic
Scientist
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
Paleomagnetism Lab, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China 100101
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Laboratory of Palaeomagnetism, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101, China.
Paleomagnetism Laboratory, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, PR China
Key Laboratory of the Earth's Deep Interior, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Palaeomagnetism Lab, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
State Key Lab of LTE, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, PR China; Department of Earth and Environmental Science, Ludwig-Maximilians-University, Munich 80333, Germany
Palaeomagnetism Laboratory, Institute of Geology and Geophysics, Chinese Academy of Sciences, 100029, Beijing, China
Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9701, 100101, Beijing, China
Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100101, China
Key Laboratory of Earth's Deep Interior, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
A new method in mineral magnetism for the separation of weak antiferromagnetic signal from a strong ferrimagnetic background
An assessment of the reliability of palaeointensity results obtained from the Cretaceous aged Suhongtu section, Inner Mongolia, China
Biomineralization, crystallography and magnetic properties of bullet-shaped magnetite magnetosomes in giant rod magnetotactic bacteria
Determination of magnetic carriers of the characteristic remanent magnetization of Chinese loess by low-temperature demagnetization
Determining the climatic boundary between the Chinese loess and palaeosol: evidence from aeolian coarse-grained magnetite
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