1Raisbeck G M,et a1.~ (10) Be deposition at Vostok, Antarctica, during the last 50, 000 years and its relationship to possible cosmogenic production variations during this period[].The Last Deglaciation: Absolute and Radiocarbon Chronologies.1992
2Beer J,et al.(10) Be peaks as time markers in polar ice cores[].The Last Deglaciation: Absolute and Radiocarbon Chronologies.1992
3Tric E,et al.Paleointensity of the geomagnetic field during the last 80, 000 years[].Journal of Geophysical Research.1992
4Schneider D A.An estimate of late Pleistocene geomagnetic intensity variation from Sulu Sea sediments[].Earth and Planetary Science.1993
5Channell J E T,et al.O at ODP 983 （Gardar Drift, North Atlantic） since 350 ka[].Earth and Planetary Science.1997
6Meynadier L,et al.Saw-toothed variations of relative paleointensity and cumulative viscous remanence: Testing the record and the model[].Journal of Geophysical Research.1998
7Tauxe L,et al.Normalized remanence in sediments of the Western Equatorial Pacific: Relative paleointensity of the geomagnetic field[].Journal of Geophysical Research.1990
8Yamazak T,et al.Long-term secular variation of the geomagnetic field during the last 200 kyr recorded in sediment cores frorn the western equatorial Pacific[].Earth and Planetary Science.1994
9Yamazaki T,et al.Relative paleointensity of the geomagnetic field during the Brunhes Chron[].Earth and Planetary Science.1995
10Schneider D A,et al.A high-resolution marine sedimentary record of geomagnetic intensity during Brunhes Chron[].Earth and Planetary Science.1996
10Guyodo Y, Valet j P. A comparison of relative paleointensity records of the Matuyama Chron for the period 0.75-1.25 Ma. Phys Earth Planet Inter, 2006, 156:205--212.
