[1] 孙东怀. 晚新生代黄土高原风尘序列的磁性地层与古气候记录[D]. 西安:中国科学院研究生院(地球环境研究所),1997:74-75.[SUN Donghuai. Magnetostratigraphy and paleoclimate records of late Cenozoic eolian sequence in the loess plateau of China[D]. Xi'an:University of Chinese Academy of Sciences, 1997:74-75.][2] 吉云平,夏正楷. 不同类型沉积物磁化率的比较研究和初步解释[J]. 地球学报,2007,28(6):541-549.[JI Yunping,XIA Zhengkai. Comparison and primarily interpretation of magnetic susceptibilities in different sediments[J]. Acta Geoscientica Sinica, 2007,28(6):541-549.][3] 刘东生. 黄土与环境[M]. 北京:科学出版社,1985:1-481.[LIU Dongsheng. Loess and the environment[M]. Beijing:Science Press,1985:1-481.][4] AN Z S,JOHN E K,WARREN P,et al. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since late Miocene times[J]. Nature,2001,(411):62-66.[5] ZHOU L P,OLDFIELD F,WINTLE A G,et al. Partly pedogenic origin of magnetic variations in Chinese loess[J]. Nature, 1990,(346):737-739.[6] 刘秀铭,刘东生,夏敦胜,等. 中国与西伯利亚黄土磁化率古气候记录-氧化和还原条件下的两种成土模式分析[J]. 中国科学D辑:地球科学,2007,37(10):1382-1391.[LIU Xiuming, LIU Donsheng,XIA Dunshng,et al. Loess susceptibility paleoclimate records in China and Siberia-two soil mode analysis under oxidizing and reducing conditions[J]. Science in China(Series D):Earth Science,2007,37(10):1382-1391.][7] 刘秀铭,夏敦胜,刘东生,等. 中国黄土和阿拉斯加黄土磁化率气候记录的两种模式探讨[J]. 第四纪研究,2007,27(2):210-220.[LIU Xiuming,XIA Dunshng,LIU Donsheng,et al. Discussion on two models of paleoclimatic records of magnetic susceptibility of Alaskan and Chinese loess[J]. Quaternary Sciences, 2007,27(2):210-220.][8] KUKLA G,AN Z. Loess stratigraphy in Central China[J]. Palaeogeography Palaeoclimatology Palaeoecology,1989,72(89):203-225.[9] 叶玮,矢吹真代,赵兴有,等. 中国西风区与季风区黄土沉积特征对比研究[J]. 干旱区地理,2006,28(6):789-794.[YE Wei, YABUKI Sadayo,ZHAO Xinyou,et al. Comparison of sedimentary features of loess between the westerly and monsoon regions in China[J]. Arid Land Geography:2006,28(6):789-794.][10] HELLERr F,LIU T. Magnetism of Chinese loess deposits[J]. Geophysical Journal of the Royal Astronomical Society,1984, 77(1):125-141.[11] 胡雪峰."黄土-古土壤"序列中氧化铁和有机质对磁化率的影响[J]. 土壤学报,2004,41(1):7-12.[HU Xuefeng. Influence of iron oxides and organic matter on magnetic susceptibility in the loess-paleosol sequence[J]. Acta Pedologica Sinica,2004, 41(1):7-12.][12] 史正涛,董铭,方小敏. 伊犁盆地晚更新世黄土-古土壤磁化率特征[J]. 兰州大学学报,2007,43(2):7-10.[SHI Zhengtao, DONG Ming,FANG Xiaoming. The characteristics of later Pleistocene loess-paleosol magnetic susceptibility in Yili Basin[J]. Journal of Lanzhou University,2007,43(2):7-10.][13] 贾佳,刘现彬,夏敦胜,等. 坎苏剖面记录的西天山地区黄土磁学性质及其控制因素初探[J]. 干旱区地理,2011,34(1):124-132.[JIA Jia,LIU Xianbin,XIA Dunsheng,et al. Magnetic property and its dominant fact of loess strata in western Tianshan area recorded by Kansu section[J]. Arid Land Geography:2011,34(1):124-132.][14] 魏海涛,夏敦胜,陈发虎,等. 新疆表土磁学性质及其环境意义[J]. 干旱区地理,2009,32(5):676-683.[WEI Haitao,XIA Dunsheng,CEHN Fahu,et al. Magnetic characteristics of surface soil and its significance in Xinjiang,China[J]. Arid Land Geography:2009,32(5):676-683.][15] 宋友桂,史正涛,方小敏,等. 伊犁黄土的磁学性质及其与黄土高原对比[J]. 中国科学D辑:地球科学,2010,40(1):61-72.[SONG Yougui,SHI Zhengtao,FANG Xiaoming,et al. Loess magnetic properties in the Ili Basin and their correlation with the Chinese Loess Plateau[J]. Science in China(Series D):Earth Science,2010,40(1):61-72.][16] 张国宏,李智才,宋燕,等. 中国降水量变化的空间分布特征与东亚夏季风[J]. 干旱区地理,2011,34(1):34-42.[ZHANG Guohong,LI Zhaicai,SONG Yan,et al. Spatial patterns of change trend in rainfall China and the of role of East Asia summer monsoon[J]. Arid Land Geography:2011,34(1):34-42.][17] 刘秀铭,刘东生,HELLER F,等. 黄土频率磁化率与古气候的冷暖变换[J]. 第四纪研究,1990,(1):42-50.[LIU Xiuming, LIU Dungsheng,HELLER F. Frequency-dependent susceptibility of loess and quaternary paleoclimate[J]. Quaternary Sciences, 1990,(1):42-50.][18] 韩家懋,HUS J J,刘东生,等. 马兰黄土和离石黄土的磁学性质[J]. 第四纪研究,1991,12(4):310-325.[HAN Jiafan,Hus J J, LIU Dongsheng,et al. Magnetic properties of the Malan and Lishi formations[J]. Quaternary Sciences,1991,12(4):310-325.][19] 夏敦胜,陈发虎,马剑英,等. 新疆伊犁地区典型黄土磁学特征及其环境意义初探[J]. 第四纪研究,2010,30(5):902-910.[XIA Dunsheng,CHEN Fahu,MA Jianying,et al. Typical loess magnetic characteristics and environmental significance Preliminary in Yili of Xinjiang[J]. Quaternary Sciences,2010,30(5):902-910.][20] TORRENT J,BARRON V,LIU Qingson. Magnetic enhancement is linked to and precedes hematite formation in aerobic soil[J]. Geophysical Research Letters,2006,33(2):1-4.[21] 何柳,孙有斌,安芷生. 中国黄土颜色变化的控制因素和古气候意义[J]. 地球化学,2010,39(5):447-455.[HE Liu,SUN Youbin,AN Zhisheng. Changing color Chinese loess:Controlling factors and paleoclimatic significances[J]. Geochimica, 2010,39(5):447-455.][22] 周玮,季峻峰,BALSAM W,等. 利用漫反射光谱鉴定红粘土中针铁矿和赤铁矿[J]. 高校地质学报,2007,13(4):730-736.[ZHOU Wei,JI Junfeng,BALSAM W,et al. Determination of goethite and hematite in red clay by diffuse reflectance spectroscopy[J]. Geological Journal of China Universities,2007,13(4):730-736.][23] 邓少福,杨太保,秦宏毅,等. 新疆塔城黄土-古土壤磁化率特征及其影响因素[J]. 中国沙漠,2011,31(4):848-854.[DENG Shaofu,YANG Taibao,QIN Hongyi,et al. Magnetic susceptibility and its influencing factors from loess-paleosol in Tacheng, Xinjiang,China[J]. Journal of Desert Research,2011,31(4):848-854.][24] 贾蓉芬,刘东生,林本海. 陕西兰田段家坡黄土剖面有机质磁性的初步研究[J]. 地球化学,1992,(3):234-242.[JIA Rongfen, LIU Dongsheng,LIN Benhai. A preliminary study on magnetism of organic matter in Duanjiapo loess section(Q2-Q3)at Lantian,Shaanxi Province,China[J]. Geochimica,1992,(3):234-242.][25] MAHER B A,TAYLOR R M. Formation of ultrafine-grained magnetite in soils[J]. Nature,1988,(336):368-370.[26] 邓少福,杨太保,鄂崇毅,等. 新疆博乐黄土磁化率特征及影响因素[J]. 土壤通报,2012,43(5):1054-1059.[DENG Shaofu, YANG Taibao,E Chongyi,et al. Magnetic susceptibility and influencing factors from Bole,Xinjiang province[J]. Chinese Journal of Soil Science,2012,43(5):1054-1059.][27] 李传想,宋友桂. 新疆伊犁黄土磁化率增强机制差异性分析[J]. 地球学报,2011,32(1):80-86.[LI Chuanxiang,SONG Yougui. Differences in magnetic susceptibility enhancement in Ili loess, xinjiang[J]. Acta Geoscientica Sinica,2011,32(1):80-86.][28] BEGET J E,HAWKINS D B. Influence of orbital parameters on Pleistocene loess deposition in central Alaska[J]. Nature,1989, (337):151-153. |