[1] George Kukla, Friedrich Heller. Pleistocene climates in China dated by magnetic susceptibility[J]. Geology, 1988, 16: 811～814
[2] 安芷生, 吴锡浩. 最近2万年中国古环境变迁的初步研究. 黄土(第四纪地质)全球变化[C].1990. 1～26 [An Zhisheng, Wu Xihao. A pilot study about Chinese paleoenvironment evolution last 20kyr, Loess ( Quaternary Geology) Global Change, 1990.1～26]
[3] Rosenbaum J G. A Record of middle Pleistocene climate change from Buck Lake, Cascade range, southern Oregon-Evidence from sediment magnetism, trace-element geochemistry, and pollen[J]. Geological Society of American Bulletin, 1996, 108(10):1 328～1 332
[4] 胡守云,王苏民,Appel E等. 呼伦湖湖泊沉积物磁化率变化的环境磁学机制[J]. 中国科学(D),1998, 28(4): 334～339[Hu Shouyun, Wang Sumin, Appel E. Environmental magnetism mechanism of susceptibility changes in Hulun lake sediments[J]. Science in China(D), 1998, 28(4): 334～339]
[5] Teh-Quei Lee, Hwa-Sung Lin. Magnetic analysis on lacustring deposits of Yuan-Yang lake, Northern Taiwan[J]. Journal of the Geological Society of China, 1999, 41(1): 143～158
[6] Roy Thompson & Frank Oldfield. Environmental magnetism[M]. London: Allen & Unwin, 1986
[7] Peck J A, King J W. A rock-magnetic record from Lake Baikal, Siberia: Evidence for Late Quaternary climate change[J]. Earth Planet Sci.Lett., 1994, 122: 221～238
[8] Williams D F, Peck J. Lake baikal record of continental climate response to Orbital Insolation during the past 5 million years[J]. Science, 1997, 278: 1 114～1 117
[9] Jones B F, Bowser C J. The mineralogy and related chemistry of lake sediments[A]. In: Lerman A, ed. Lakes:Chemistry, Geology, Physics[C]. New York: Springer, 1978.
[10] Dell C I. An occurrence of greigite in Lake Superior sediments[J]. Am.Mineralogist 57, 1972
[11] Hilton J, Lishman J P. The effect of redox change on the magnetic susceptibility of sediments from a seasonally anoxic lake[J]. Limnol. Oceanogr., 1985, 30: 907～909
[12] 杨小强,李华梅. 泥河湾盆地典型剖面沉积物磁化率特征及其意义[J]. 海洋地质与第四纪地质,1999, 19(1): 75～84 [Yang Xiaoqiang, Li Huamei. The susceptibility characteristics of the typical sections in Nihewan basin and its implication[J]. Marine Geology & Quaternary Geology, 1999,19(1):75～84]
[13] Jef Vandenberghe, An Zhisheng. New absolute time scale for the Quaternary climate in the Chinese loess region by grain-size analysis[J]. Geology, 1997, 25(1): 35～38
[14] 鹿化煜、安芷生. 黄土高原黄土粒度组成的古气候意义[J]. 中国科学(D),1998, 3: 278～283[Lu, Huayu, An Zhisheng. Paleoclimatic significance of grain size of loess-palaeosol deposit in Chinese Loess Plateau[J]. Science in China(Series D, Earth Sciences), 1998, 41:626～631 1 006～1 313]
[15] 鹿化煜, 安芷生. 洛川黄土粒度组成的古气候意义[J]. 科学通报,1997, 42(1): 66～69 [Lu Huayu, An Zhisheng. Paleoclimate signifcance of grain size in Luochuan loess-palaeosol series[J]. Chinese Science Bulletin, 1997, 42(1): 66～69 ]
[16] Eutizio Vittori. Grain size of fluvial deposits and late Quaternary climate:A case study in the Po River Valley(Italy)[J]. Geology, 1995, 23(8): 735～738