Heller F, Liu T S. Magnetostratigraphical dating of loess deposits in China[J]. Nature, 1982, 300(5891): 431-433.
[2]
Zhou L P, Oldfield F, Wintle A G, et al. Partly pedogenic origin of magnetic variations in Chinese Loess[J]. Nature, 1990, 346(6286): 737-739.
[3]
Liu Q S, Roberts A P, Larrasoa？a J C, et al. Environmental magnetism: Principles and applications[J]. Reviews of Geophysics, 2012, 50(4), doi: 10.1029/2012rg000393.
[4]
安芷生,Porter S, Kukla G,等. 最近13万年黄土高原季风变迁的磁化率证据[J]. 科学通报,1990,35(7):529-532. [An Zhisheng, Porter S, Kukla G, et al. Magnetic susceptibility evidence of season winds changes on loess plateau during the late 139kyr[J]. Chinese Science Bulletin, 1990, 35(7): 529-532.]
[5]
邓成龙,刘青松,潘永信,等. 中国黄土环境磁学[J]. 第四纪研究,2007,27(2):193-209. [Deng Chenglong, Liu Qingsong, Pan Yongxing, et al. Environmental magnetism of Chinese loess-paleosol sequences[J]. Quaternary Sciences, 2007, 27(2): 193-209.]
[6]
魏海涛,Banerjee S K,夏敦胜,等. 天山北麓黄土环境磁学特征及其古气候意义[J]. 地球物理学报,2013,56(1):150-158. [Wei Haitao, Banerjee S K, Xia Dunsheng, et al. Magnetic characteristics of loess-paleosol sequences on the north slope of the Tianshan Mountains, northwestern China and their paleoclimatic implications[J]. Chinese Journal Geophysics, 2013, 56(1): 150-158.]
[7]
安芷生,张培震,王二七,等. 中新世以来我国季风—干旱环境演化与青藏高原的生长[J]. 第四纪研究,2006,26(5):678-693. [An Zhisheng, Zhang Peizhen, Wang Erqi, et al. Changes of the monsoon-arid environment in China and growth of the Tibetan Plateau since the Miocene[J]. Quaternary Sciences, 2006, 26(5):678-693.]
[8]
吴翼,朱照宇,邱世藩,等. 1.95~0.40 Ma 黄土高原东南部风成沉积记录的亚洲冷干化进程[J]. 科学通报,2013,58(27):2823-2831. [Wu Yi, Zhu Zhaoyu, Qiu Shifan, et al. A rock magnetic record of Asian cooling and aridification processes during 1.95~0.40 Ma in the southeastern Chinese Loess Plateau[J]. Chinese Science Bulletin, 2013, 58(27): 2823-2831.]
[9]
朱立平,陈玲,张平中,等. 环境磁学反映的藏南沉错地区1300年来冷暖变化[J]. 第四纪研究,2001,21(6):520-527. [Zhu Liping, Chen Ling, Zhang Pingzhong, et al. Cold/warm fluctuations of the last 1300 years reflected by environmental magnetism in the Chen Co area, southern Tibet[J]. Quaternary Sciences, 2001, 21(6): 520-527.]
[10]
李永涛,顾延生,曲赞. 武汉天兴洲近代沉积物的磁性特征及其环境意义[J]. 地球科学(中国地质大学学报),2011,36(4):779-788[Li Yongtao, Gu Yansheng, Qu Zan. Magnetic properties of recent sediments at Tianxing central shoal of Wuhan: implication for sedimentary environment change in the middle reaches of the Yangtze River[J]. Earth Science(Journal of China University of Geosciences), 2011, 36(4): 779-788]
[11]
卢升高,白世强. 杭州城区土壤的磁性与磁性矿物学及其环境意义[J]. 地球物理学报,2008,51(3):762-769. [Lu Shenggao, Bai Shiqiang. Magnetic characterization and magnetic mineralogy of the Hang zhou urban soils and its environmental implications[J]. Chinese Journal Geophysics, 2008, 51(3): 762-769.]
[12]
田庆春,杨太保,张述鑫,等. 青藏高原腹地湖泊沉积物磁化率及其环境意义[J]. 沉积学报,2011,29(1):143-150. [Tian Qingchun, Yang Taibao, Zhang Shuxin, et al. Magnetic susceptibility and its environmental significance of lake sediments in Tibet Plateau[J]. Acta Sedimentologica Sinica, 2011, 29(1): 143-150.]
[13]
王心源,吴立,张广胜,等. 安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J]. 地理科学,2008,28(4):548-553. [Wang Xinyuan, Wu Li, Zhang Guangsheng, et al. Characteristics and environmental significance of magnetic susceptibility and grain size of lacustrine sediments since Holocene in Chaohu Lake, Anhui province[J]. Scientia Geographica Sinica, 2008, 28(4): 548-553.]
[14]
伏捷,李永化,张华,等. 辽东半岛晚新生代沉积物磁化率特征及初步解释[J]. 干旱区资源与环境,2014,28(3):135-141. [Fu Jie, Li Yonghua, Zhang Hua, et al. Characteristic of magnetic susceptibility and its primary interpretation of Late Cenozoic sediments in Liaodong Peninsula[J]. Journal of Arid Land Resources and Environment, 2014, 28(3): 135-141.]
[15]
张英,夏敦胜,赵瑞瑞,等. 新疆博斯腾湖湖滨沉积物的磁学特征及其环境意义[J]. 海洋地质与第四纪地质,2013,33(4): 93-102. [Zhang Ying, Xia Dunsheng, Zhao Ruirui, et al. Magnetic properties of the lakeshore sediments of the Bosten Lake, Xinjiang China and their environmental implications[J]. Marine Geology and Quaternary Geology, 2013, 33(4): 93-102.]
[16]
Hao Qingzhen, Guo Zhengtang. Spatial variations of magnetic susceptibility of Chinese loess for the last 600 kyr: implications for monsoon evolution[J].Journal of Geophysical Research: Solid Earth, 2005, 110(B12): B12101, doi: 10.1029/2005JB003765.
[17]
刘志锋,刘青松. 陕西延安两个坡度不同土壤剖面磁学性质及其在古降雨量重建中的意义[J]. 中国科学(D辑):地球科学,2013,43(12):2037-2048. [Liu Zhifeng, Liu Qingsong. The magnetic properties of different soil profiles and its significance in ancient rainfall reconstruction in Shannxi Xi'an[J]. Science China (Seri. D): Earth Sciences, 2013, 43(12): 2037-2048.]
[18]
Liu Zhifemg, Liu Qingsong, Torrent J, et al. Testing the magnetic proxy XFD/HIRM for quantifying paleoprecipitation in modern soil profiles from Shanxi Province, China[J]. Global and Planetary Change, 2013, 110(Part C): 368-378.
[19]
魏海涛,夏敦胜,陈发虎,等. 黄土高原及相邻地区表土磁化率与降水量的关系[J]. 冰川冻土,2008,30(3):433-439. [Wei Haitao, Xia Dunsheng, Chen Fahu, et al. Relationship between the magnetic susceptibility of surface soil and precipitation of Loess Plateau and adjacent area[J]. Journal of Glaciology and Geocryology, 2008, 30(3): 433-439.]
[20]
朱丽东,姜永见,张明强,等. 庐山JL剖面红土磁化率特征及古环境记录[J]. 山地学报,2011,29(4):385-394. [Zhu Lidong, Jiang Yongjian, Zhang Mingqiang, et al. Characteristics of magnetic susceptibility and its paleo-environmental records from JL red earth section, Lushan area[J]. Journal of Mountain Science, 2011, 29(4): 395-394.]
[21]
卢升高. 中国南方红土环境磁学[J]. 第四纪研究,2008,27(6):1016-1022. [Lu Shenggao. Environmental magnetism of Quaternary red Earth in the southern China[J]. Quaternary Sciences, 2008, 27(6): 1016-1022.]
[22]
卢升高. 第四纪红土的磁性与氧化铁矿物学特征及其古环境意义[J]. 土壤学报,2000,37(2):182-191. [Lu Shenggao. Characterization of magnetism and iron oxide minerals of Quaternary red earth and its paleo-environmental implications[J]. Acta Pedologica Sinica, 2000, 37(2): 182-191.]
[23]
卢升高,董瑞斌,俞劲炎,等. 中国东部红土的磁性及其环境意义[J]. 地球物理学报,1999,42(6):764-771. [Lu Shenggao, Dong Ruibin, Yu Jinyan, et al. Magnetic measurement characterisation of red earth profile in eastern China and its environmental implications[J]. Chinese Journal Geophysics, 1999, 42(6): 764-771.]
[24]
杨浩,夏应菲,赵其国,等.红 土系列剖面的磁化率特征与古气候冷暖变换[J]. 土壤学报,1995,32(增刊2):195-200. [Yang Hao, Xia Yingfei, Zhao Qiguo, et al. The character of magnetic susceptibility of red earth profile in South China and palaeo-climate changes[J]. Acta Pedologica Sinica, 1995, 32(Suppl. 2): 195-200.]
[25]
袁大刚,张甘霖. 雨花台红土的磁化率特征及其古环境意义[J]. 土壤,2008,40(1):110-113. [Yuan Dagang, Zhang Ganlin. Characterization of magnetic susceptibility of red Earth at Yuhuatai and its paleo-environmental implications[J]. Soils, 2008, 40(1): 110-113.]
[26]
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 Dunsheng, Liu Tungsheng, 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.]
[27]
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 Tungsheng, Xia Dunsheng, et al. Two pedogenic models for paleoclimatic records of magnetic susceptibility from Chinese and Siberian Loess[J]. Science China (Seri. D): Earth Sciences, 2007, 37(10): 1382-1391.]
[28]
Dearing J A, Livingstone I P, Bateman M D, et al. Palaeoclimate records from OIS 8.0-5.4 recorded in loess-palaeosol sequences on the Matmata Plateau, southern Tunisia, based on mineral magnetism and new luminescence dating[J]. Quaternary International, 2001, 76-77: 43-56.
[29]
吕厚远,韩家懋,吴巧琴,等.中国现代土壤磁化率分析及其古气候意义[J]. 中国科学(B辑),1994,24(12):1290-1297. [Lü Houyuan, Han Jiamao, Wu Qiaoqin, et al. Analysis on magnetism and paleo-climate meaning in modern soil of China[J]. Science China (Seri. B), 1994, 24(12): 1290-1297.]
[30]
钱鹏,郑祥民,王晓勇,等. 江苏南通黄泥山黄土粒度与环境磁学特征及其成因[J]. 海洋地质与第四纪地质,2010,30(1):109-114.[Qian Peng, Zheng Xiangmin, Wang Xiaoyong, et al. Particle sizes, magnetic properties and origins of loess deposits from Huangnishan Hill in Nantong, Jiangsu province[J]. Marine Geology & Quaternary Geology, 2010, 30(1): 109-114.]
[31]
李勇,李海燕,白凌燕,等. 发育于石英岩之上的表土磁学性质及其环境磁学意义[J]. 土壤,2009,41(1):60-66.[Li Yong, Li Haiyan, Bai Lingyan, et al. Magnetic property and environmental magnetism significance of surface soil derived from quartzite[J]. Soils, 2009, 41(1): 60-66.]
[32]
贾松伟,韦方强. 利用磁性参数诊断泥石流沟道沉积物来源——以云南蒋家沟流域为例[J]. 泥沙研究,2009(1): 54-59.[Jia Songwei, Wei Fangqiang. Tracing sediment sources using magnetic measurements—A case study of Jiangjiagou valley, Yunnan province[J]. Journal of Sediment Research, 2009(1): 54-59.]
[33]
王辉,郑祥民,王晓勇,等. 长江中下游干流河底沉积物环境磁性特征[J]. 第四纪研究,2008,28(4):640-648.[Wang Hui, Zheng Xiangmin, Wang Xiaoyong, et al. Environmental magnetic properties of sediments from middle and lower reaches of Changjiang River[J].Quaternary Sciences, 2008, 28(4): 640-648.]
[34]
刘东生,等. 黄土与环境[M]. 北京:科学出版社,1985:191-208. [Liu Dongsheng, et al. Loess and the Environment[M]. Beijing: Science Press, 1985: 191-208.]
[35]
胡雪峰,龚子同,夏应菲,等. 安徽宣州黄棕色土和第四纪红土的比较研究及其古气候意义[J]. 土壤学报,1999,36(3):301-307. [Hu Xuefeng, Gong Zitong, Xia Yingfei, et al. Comparative study of Yellow-Brown Earth and Quaternary red clay in Xuanzhou, Anhui province and its palaeo-climate significance[J]. Acta Pedologica Sinica, 1999, 36(3): 301-307.]
[36]
李敬卫,乔彦松,王燕,等. 江西九江红土堆积的粒度特征及成因研究[J]. 地质力学学报,2009,15(1):95-104. [Li Jingwei, Qiao Yansong, Wang Yan, et al. Aeolian origin of the red Earth tormation in Jiujiang city of Jiangxi province, China: evidence from grain-size analysis [J]. Journal of Geomechanic, 2009, 15(1): 95-104.]
[37]
李徐生,杨达源,鹿化煜.镇江下蜀黄土粒度特征及其成因初探[J].海洋地质与第四纪地质,2001,21(1):25-32. [Li Xusheng, Yang Dayuan, Lu Huayu. Grain-size features and genesis of the Xiashu loess in Zhenjiang[J].Marine Geology & Quaternary Geology, 2001, 21(1): 25-32.]
[38]
蔡方平,胡雪峰,杜艳,等. 安徽郎溪黄棕色土—红土二元结构土壤剖面的成因与长江流域第四纪晚期古气候演变[J]. 土壤学报,2012,49(2):220-229. [Cai Fangping, Hu Xuefeng,Du Yan, et al. Pedogenesis of Yellow-Brown Earth-Red Clay profile in Langxi county, Anhui province and paleoclimatic change in the Yangtze River Valley Southeast China in the Late Quaternary Period[J]. Acta Pedologica Sinica, 2012, 49(2): 220-229.]
[39]
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):67-69. [Lu Huayu, An Zhisheng. Palaeo-climatic implication of grain-size composition record in Luochuan Loess[J]. Chinese Science Bulletin, 1997, 42(1): 67-69.]
[40]
席承藩. 关于中国红色风化壳的几个问题[J]. 第四纪研究,1965,4(2):42-54. [Xi Chengfan. Some problems of Chinese red residuum[J]. Quaternary Sciences, 1965, 4(2): 42-54.]
[41]
叶玮,杨立辉,朱丽东,等. 中亚热带网纹红土的稀土元素特征与成因分析[J]. 地理科学,2008,28(1):40-44. [Ye Wei, Yang Lihui, Zhu Lidong, et al. Characteristics and origin of rare earth elements of vermicular red earth in middle sub-tropic zone[J]. Scientia Geographica Sinica, 2008, 28(1): 40-44.]
[42]
胡雪峰,龚子同. 江西九江泰和第四纪红土成因的比较研究[J]. 土壤学报,2001,38(1):1-8. [Hu Xuefeng, Gong Zitong. Comparative study of the origin of Quaternary Red Earth in Jiujiang and Taihe, Jiangxi province [J]. Acta Pedologica Sinica, 2001, 38(1): 1-8.]
[43]
Bronger A, Heinkele T. Micromorphology and genesis of paleosols in the Luochuan loess section,China: Pedostratigraphic and environmental implications[J]. Geoderma, 1989, 45(2): 123-143.
[44]
卢升高. 中国土壤磁性与环境[M]. 北京:高等教育出版社,2003:240. [Lu Shenggao. Magnetism of Soils in China and Its Environment Implication[M]. Beijing:Higher Education Press, 2003: 240.]
[45]
Fine P, Singer M J. Contribution of ferrimagnetic minerals to oxalate and dithionite extractable iron[J]. Soil Science Society of America Journal, 1989, 53(1):191-196.
[46]
Evans M E, Heller F. Environmental Magnetism: Principles and Applications of Enviromagnetics[M]. London: Academic Press, 2003:69-74.
[47]
Hu Xuefeng, Wei Ji, Xu Liangfeng, et al. Magnetic susceptibility of the Quaternary red clay in subtropical China and its paleoenvironmental implications[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 279 (3/4): 216-232.
[48]
Thompson R, Oldfield F. Environmental Magnetism[M].London: Allen and Unwin, 1986:76.
[49]
Liu Qingsong, Jackson M J, Banerjee S K, et al. Mechanism of the magnetic susceptibility enhancements of Chinese loess[J]. Journal of Geophysical Research: Solid Earth,2004,109(B12): , doi: 10.1029/2004JB003249.
[50]
Nie Junsheng, Song Yougui, King J W, et al. HIRM variations in the Chinese red-clay sequence: Insights into pedogenesis in the dust source area[J]. Journal of Asian Earth Sciences, 2010, 38(3/4): 96-104.
[51]
朱景郊. 网纹红土的成因及其研究意义[J]. 地理研究,1988,17(4):12-20. [Zhu Jingjiao. Genesis and research significance of the plinthitic horizon[J]. Geographical Research, 1988, 17(4): 12-20.]
[52]
朱丽东,叶玮,周尚哲,等. 中亚热带第四纪红粘土的粒度特征[J]. 地理科学,2006,26(5):5586-5591[Zhu Lidong, Ye Wei, Zhou Shangzhe, et al. Grain- size features of red earth in mid- subtropics[J]. Scientia Geographica Sinica, 2006, 26(5): 5586-5591]
[53]
Van Houten F B. Origin of red beds: a review—1961-1972[J]. Annual Review of Earth and Planetary Science, 1973, 1: 39-61.
[54]
胡忠行,朱丽东,张卫国,等. 江西九庐公路红土剖面的磁学特征及其反映的风化成土作用[J]. 地球物理学报,2011,54(5):1319-1326. [Hu Zhongxing, Zhu Lidong, Zhang Weiguo, et al. Magnetic properties of red clay section along the Jiu-Lu highway at Jiujiang, Jiangxi and implications for pedogenesis[J]. Chinese Journal Geophysics, 2011, 54(5): 1319-1326.]
[55]
刘彩彩,邓成龙. 南方红土的磁性矿物组成及其区域性差异[J]. 第四纪研究,2012,32(4):626-634. [Liu Caicai, Deng Chenglong. Magnetic mineralogy of the red soil sequences in Southern China and its variety[J]. Quaternary Sciences, 2012, 32(4): 626-634.]
[56]
叶玮,朱丽东,李凤全,等. 中国亚热带风尘沉积物磁学特征对比研究[J]. 第四纪研究,2013,33(5):911-924. [Ye Wei, Zhu Lidong, Li Fengquan, et al. Magnetic properties of the Quaternary sediments with aeolian dust characteristics in present subtropical China and their implications for climate[J]. Quaternary Sciences, 2013, 33(5): 911-924.]
[57]
卢升高. 亚热带富铁土的磁学性质及其磁性矿物学[J]. 地球物理学报,2000,43(4):498-504. [Lu Shenggao. Magnetic properties of subtropical ferrisoils and its magnetic mineralogical study[J]. Chinese Journal Geophysics, 2000, 43(4): 498-504.]
[58]
俞劲炎. 土壤磁学—土壤学研究的新领域[J]. 土壤学进展,1979(4):1-12. [Yu Jinyan. Soil magnetism-New field of soil science research[J]. Progress in Soil Science, 1979(4): 1-12.]
[59]
胡雪峰,程天凡,巫和昕. 南方网纹红土内是否可能存在多个"沉积—成土"过程的旋回?[J]. 科学通报,2003,48(9):969-975. [Hu Xuefeng, Cheng Tianfan, Wu Hexin. Do multiple cycles of Aeolian deposit pedogenesis exist in the reticulate red clay sections in southern China?[J]. Chinese Science Bulletin, 2003, 48(9): 969-975.]
[60]
尹秋珍,郭正堂.中国南方的网纹红土与东亚季风的异常强盛期[J].科学通报,2006,51(2):186-193. [Yin Qiuzhen, Guo Zhentang. Mid-Pleistocene vermiculated red soils in Southern China as an indication of unusually strengthened East Asia monsoon[J]. Chinese Science Bulletin, 2006, 51(2): 186-193.]
[61]
Han Jiamao, Liu Houyuan, Wang Naiqin, et al. The magnetic susceptibility of modern soils in China and its use for paleoclimate reconstruction[J]. Studia Geophysica et Geodaetica, 1996, 40(3): 262-275.
[62]
韩志勇,李徐生,陈英勇,等. 矫顽力组分定量分析揭示下蜀黄土磁化率异常降低的原因[J]. 地球物理学报,2008,51(6):1835-1843. [Han Ziyong, Li Xusheng, Chen Yiyong, et al. Quantification of magnetic coercivity components reveals the cause of anomalous decrease of magnetic susceptibility of the Xiashu loess[J]. Chinese Journal Geophysics, 2008, 51(6): 1835-1843.]
[63]
Bassinot F C, Labeyrite L D, Vincent E, et al. The astronomical theory of climate and the age of the Brunhes Matuyama magnetic reversal[J]. Earth and Planetary Science Letters, 1994, 126(1/2/3): 91-108.
[64]
Alexander A, Douglas P, Williams F, et al. Muted climate variations in continental Siberia during the mid-Pleistocene epoch[J]. Nature, 2002, 418: 65-68.
