方小敏,李吉均,朱俊杰等.甘肃临夏盆地新生代地层绝对年代测定与划分.科学通报,1997,42(14):1457～1471 Fang Xiaomin,Li Jijun,Zhu Junjie et al.Chronology and division of the Cenozoic stratigraphy in the Linxia Basin of Gansu Province.Chinese Science Bulletin,1997,42(14):1457～1471
[2]
Li Jijun,Feng Zhaodong,Tang Lingyu.Late Quaternary monsoon patterns on the Loess Plateau of China.Earth Surface Processes and Landforms,1988,13:125～135
[3]
宋春晖,白晋锋,赵彦德等.临夏盆地 13～4.4Ma湖相沉积物颜色记录的气候变化探讨.沉积学报,2005,23(3):507～513 Song Chunhui,Bai Jinfeng,Zhao Yande et al.The color of lacustrine sediments recorded climatic changes from 13 to 4.5Myr in Linxia Basin.Acta Sedimentologica Sinica,2005,23(3):507～513
[4]
李吉均,方小敏,马海洲等.晚新生代黄河上游地貌演化与青藏高原隆起.中国科学(D辑),1996,26(4):316～322 Li Jijun,Fang Xiaomin,Ma Haizhou et al.Geomorphological and environmental evolution in the upper reaches of the Yellow River during the Late Cenozoic.Science in China (Series D),1996,39(4):380～390
[5]
李吉均,方小敏.青藏高原隆起与环境变化研究.科学通报,1998,43(15):1569～1574 Li Jijun,Fang Xiaomin.Uplift of the Tibetan Plateau and environmental changes.Chinese Science Bulletin,1999,44(23):2117～2124
[6]
施雅风,汤懋苍,马玉贞.青藏高原二期隆升与亚洲季风孕育关系探讨.中国科学(D辑),1998,28(3):263～271 Shi Yafeng,Tang Maocang,Ma Yuzhen.Linkage between the second uplifting of the Qinghai-Xizang(Tibetan)Plateau and the initiation of the Asian monsoon system.Science in China(Series D),1999,29(3):303～312
[7]
李吉均,方小敏,朱俊杰等.临夏盆地新生代地层古地磁年代与模式序列.见:青藏项目专家委员会编.青藏高原形成演化、环境变迁与生态系统研究--学术论文年刊(1994).北京:科学出版社,1994.41～54 Li Jijun,Fang Xiaomin,Zhu Junjie et al.Paleomagnetic chronology and pattern sequence of the Cenozoic stratigraphy of the Linxia Basin in Gansu Province of China.In:The Expert Committee on the Qingzang Program ed.Study on the Formation and Evolution of the Qinghai-Xizang Plateau,Environmental Change and Ecological--Annual Academic(1994).Beijing:Science Press,1994.41～54
[8]
杨东,方小敏,宋友桂等.六盘山西侧山麓剥蚀面的发育与新构造隆升.沉积学报,2002,20(2):282～287 Yang Dong,Fang Xiaomin,Song Yougui et al.Pediment near the western Liupan Mountain and its implication on the neotectonic uplift.Acta Sedimentologica Sinica,2002,20(2):282～287
[9]
Li Jijun.Uplift of Qinghai-Xizang(Tibet)Plateau and Global Change.Lanzhou:Lanzhou University Press,1995.1～207
[10]
邱占祥,王伴月,邓涛等.甘肃省东乡族自治县龙担黄土底部新发现的哺乳动物群初步报道.第四纪研究,2002,22(1):33～38 Qiu Zhanxiang,Wang Banyue,Deng Tao et al.Notes on the mammal fauna from the bottom of loess deposits at Longdan,Dongxiang county,Gansu Province.Quaternary Sciences,2002,22(1):33～38
An Zhisheng,Kukla G J,Porter S C et al.Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130,000 years.Quaternary Research,1991,36(1):29～36
[13]
刘秀铭,刘东生,Heller F 等.中国黄土磁颗粒分析及其古气候意义.中国科学(B辑),1991,21(6):639～644 Liu Xiuming,Liu Tungsheng,Heller F et al.Study on magnetic grain size of loess in China and its implication on paleoclimate.Science in China(Series B),1991,21(6):639～644
[14]
Kukla G,Heller F,Liu Xiuming et al.Pleistocene climates in China dated by magnetic susceptibility.Geology,1988,16(9):811～814
[15]
安芷生,吴锡浩,汪品先等.最近130ka中国的古季风--Ⅱ.古季风变迁.中国科学(B辑),1991,21(11):1209～1215 An Zhisheng,Wu Xihao,Wang Pinxian et al.Monsoon changes in China during the last 130ka--Ⅱ.The variation of monsoon.Science in China(Series B),1991,21(11):1209～1215
[16]
Kukla G.Loess stratigraphy in Central China.Quaternary Science Reviews,1987,6(3～4):191～219
[17]
An Zhisheng,Porter S C,Zhou Weijian et al.Episode of strengthened summer monsoon climate of Younger Dryas age on the Loess Plateau of Central China.Quaternary Research,1993,39(1):45～54
[18]
Williams W A J,Dunkerley D L,De Deckker P et al.刘东生等编译.第四纪环境.北京:科学出版社,1997.1～304 Williams W A J,Dunkerley D L,De Deckker P et al.In:Liu Tungsheng et al.transalater and eds.Quaternary Environments.Beijing:Science Press,1997.1～304
[19]
Heller F,Liu Tungshengg.Magnetostratigraphical dating of loess deposits in China.Nature,1982,300:431～433
[20]
Heller F,Liu Tungsheng.Magnetism of Chinese loess deposits.Geophysical Journal International,1984,77(1):125～141
[21]
刘秀铭,刘东生,John Shaw.中国黄土磁性矿物特征及其古气候意义.第四纪研究,1993,(3):281～287 Liu Xiuming,Liu Tungsheng,John Shaw.Magnetic mineral characteristics of Chinese loess and its palaeoclimatic significance.Quaternary Sciences,1993,(3):281～287
[22]
吴汉宁,岳乐平.风成沉积物磁组构与中国黄土区第四纪风向变化.地球物理学报,1997,40(4):487～494 Wu Hanning,Yue Leping.The anisotropy of magnetic susceptibility of aeolian dust sediment:The paleowind field in Chinese Loess Plateau.Acta Geophysica Sinica,1997,40(4):487～494
[23]
Zhu Rixiang,Liu Qingsong,Jackson M J.Paleoenvironmental significance of the magnetic fabrics in Chinese loess-paleosols since the last interglacial(＜130ka).Earth and Planet Science Letters,2004,221(1～4):55～69
[24]
王建力,方小敏,张宇田等.青藏高原东北边缘黄土磁化率各向异性揭示古风向的初步研究.兰州大学学报(自然科学版),1995,31(4):155～159 Wang Jianli,Fang Xiaomin,Zhang Yutian et al.The anisotropy of loess magnetic susceptibility in the northeastern fringe of Qinghai-Xizang(Tibetan)Plateau as an indicator of paleowind direction.Journal of Lanzhou University(Natural Science),1995,31(4):155～159
[25]
刘秀铭,许同春,刘东生.中国黄土磁化率各向异性与成因及其对第四纪研究的意义.中国科学(B辑),1989,19(4):441～448 Liu Xiuming,Xu Tongchun,Liu Tungsheng.The causes of anisotropy of magnetic susceptibility of Chinese loess and its significance for Quaternary research.Science in China(Series B),1989,19(4):441～448
[26]
张家强,李从先,丛友滋.水成沉积与风成沉积及古土壤的磁组构特征.海洋地质与第四纪地质,1999,19(2):85～94 Zhang Jiaqiang,Li Congxian,Cong Youzi.Magnetic fabric characteristics of hydraulic deposit,eolian deposit and paleosol.Marine Geology & Quaternary Geology,1999,19(2):85～94
[27]
谢久兵,朱照宇,周厚云等.陕西蓝田公王岭黄土古土壤序列的磁组构特征及其古气候意义.地球化学,2007,36(2):185～192 Xie Jiubing,Zhu Zhaoyu,Zhou Houyun et al.Magnetic fabric of Gongwangling loess-paleosols from Lantian County,Shaanxi Province and its paleoenvironmental implications.Geochimica,2007,36(2):185～192
[28]
余志伟,丁仲礼,刘东生.2.5Ma以来地球轨道参数变化对黄土粒度变化的线性驱动.第四纪研究,1992,(2):118～127 Yu Zhiwei,Ding Zhongli,Liu Tungsheng.Astronomical forcing of loess grain-size record over the past 2.5Ma.Quaternary Sciences,1992,(2):118～127
[29]
Ding Zhongli,Ren Jianzhang,Yang Shiling et al.Climate instability during the penultimate glaciation:Evidence from two high-resolution loess records,China.Journal of Geophysical Research,1999,104(B4):20123～20132
[30]
Guo Zhengtang,Peng Shuzhen,Hao Qingzhen et al.Origin of the Miocene-Pliocene Red-Earth Formation at Xifeng in Northern China and implications for paleoenvironments.Palaeogeography,Palaeoclimatology,Palaleoecology,2001,170(1～2):11～26
[31]
Ding Zhongli,Derbyshire E,Yang Shiling et al.Stacked 2.6Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18 O record.Paleoceanography,2002,17(3):1033,10.1029/2001PA000725
[32]
Zijderveld J D A.AC demagnetization of rocks:Analysis of results.In:Collinson D W,Reer M,Runcorn S K eds.Methods in Paleomagnetism.New York:Elsevier,1967.254～286
[33]
Kirschvink J L.The least-squares line and plane and the analysis of paleomagnetic data.Geophysical Journal International,1980,62(3):699～718
[34]
朱日祥,李景春,吴汉宁等.中国黄土磁学性质与古气候意义.中国科学(B辑),1994,24(9):992～997 Zhu Rixiang,Li Jingchun,Wu Hanning et al.Magnetic characteristics of Chinese loess and its paleoclimatic signature.Science in China(Series B),1994,24(9):992～997
[35]
朱日祥,岳乐平,白立新.中国第四纪古地磁学研究进展.第四纪研究,1995,(2):162～173 Zhu Rixiang,Yue Leping,Bai Lixin.Progress of Quaternary paleomagnetism in China.Quaternary Sciences,1995,(2):162～173
[36]
方小敏,徐先海,宋春晖等.临夏盆地新生代沉积物高分辨率岩石磁学记录与亚洲内陆干旱化过程及原因.第四纪研究,2007,27(6):989～1000 Fang Xiaomin,Xu Xianhai,Song Chunhui et al.High resolution rock magnetic records of Cenozoic sediments in the Linxia Basin and their implications on drying of Asian inland.Quaternary Sciences,2007,27(6):989～1000
[37]
徐先海,方小敏.临夏盆地新生代沉积物岩石磁学记录与亚洲内陆干旱化.海洋地质与第四纪地质,2007,27(4):103～110 Xu Xianhai,Fang Xiaomin.Rock magnetic record of Cenozoic lake sediments from the Linxia Basin and the aridification of Asian Inland.Marine Geology & Quaternary Geology,2007,27(4):103～110
[38]
邓涛,王晓鸣,倪喜军等.临夏盆地的新生代地层及其哺乳动物化石证据.古脊椎动物学报,2004,42(1):45～66 Deng Tao,Wang Xiaoming,Ni Xijun et al.Cenozoic stratigraphic sequence of the Linxia Basin in Gansu,China and its evidence from mammal fossils.Vertebrata PalAsiatica,2004,42(1):45～66
[39]
邓涛.甘肃临夏盆地发现已知最早的披毛犀化石.地质通报,2002,21(10):604～608 Deng Tao.The earliest known wooly rhino discovered in the Linxia Basin,Gansu Province,China.Geological Bulletin of China,2002,21(10):604～608
[40]
王伴月,邱占祥.青藏高原东北缘黄土底部发现松鼠一新亚科.科学通报,2003,48(2):183～186 Wang Banyue,Qiu Zhanxiang.Aepyosciurinae:A new subfamily of Sciuridae(Rodentia,Mammalia)from basal loess deposits at the northeastern border of Tibetan Plateau.Chinese Science Bulletin,2003,48(7):691～695
[41]
邱占祥.泥河湾哺乳动物群与中国第四系下限.第四纪研究,2000,20(2):142～154 Qiu Zhanxiang.Nihewan fauna and Q/N boundary in China.Quaternary Sciences,2000,20(2):142～154
[42]
Cande S C,Kent D V.Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic.Journal of Geophysical Research,1995,100(B4):6093～6095
[43]
钟巍,方小敏,曹继秀等.甘肃临夏盆地东山顶剖面沉积物磁组构特征研究.兰州大学学报(自然科学版),1996,32(1):116～120 Zhong Wei,Fang Xiaomin,Cao Jixiu et al.Study on the magnetic fabric features of the samples taken from Dongshanding profile in Linxia Basin,Gansu Province.Journal of Lanzhou University(Natural Science),1996,32(1):116～120
[44]
刘秀铭,刘东生,Heller F.黄土频率磁化率与古气候冷暖变换.第四纪研究,1990,(1):42～50 Liu Xiuming,Liu Tungsheng,Heller F.Frequencey-dependent susceptibility of loess and Quaternary paleoclimate.Quaternary Sciences,1990,(1):42～50
[45]
Liu Xiuming,Liu Tungsheng,Xu Tongchun et al.The Chinese loess in Xifeng:Ⅰ.The primary study on magnetostragraphy of loess profile in Xifeng area,Gansu Province.Geophysical Journal International,1988,92(2):345～348
[46]
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.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.Quaternary Sciences,2007,27(2):210～220
[47]
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.中国科学(D辑),2007,37(10):1382～1391 Liu Xiuming,Liu Tungsheng,Paul Hesse et al.Two pedogenic models for paleoclimatic records of magneitc susceptibility from Chinese and Siberian loess.Science in China(Series D),2008,51(2):284～293
[48]
邓成龙,刘青松,潘永信等.中国黄土环境磁学.第四纪研究,2007,27(2):193～209 Deng Chenglong,Liu Qingsong,Pan Yongxin et al.Environmental magnetism of Chinese loess-paleosol sequences.Quaternary Sciences,2007,27(2):193～209
[49]
夏敦胜,陈发虎,马剑英等.黄土高原-阿拉善高原典型断面表土磁学特征研究.第四纪研究,2007,27(6):1001～1008 Xia Dunsheng,Chen Fahu,Wu Jianying et al.Environmental magnetic investigations of surface soils along a NW-SE transect from the Chinese Loess Plateau to the Alxa Plateau.Quaternary Sciences,2007,27(6):1001～1008
[50]
刘青松,邓成龙,潘永信.磁铁矿和磁赤铁矿磁化率的温度和频率特性及其环境磁学意义.第四纪研究,2007,27(6):954～962 Liu Qingsong,Deng Chenglong,Pan Yongxin.Temperature-dependency and frequency-dependency of magnetic susceptibility of magnetite and maghemite and their significance for environmental magnetism.Quaternary Sciences,2007,27(6):954～962
[51]
An Zhisheng,Kukla G,Porter S C et al.Late Quaternary dust flow on the Chinese Loess Plateau.Catena,1991,18(2):125～132
[52]
Ding Zhongli,Yu Zhiwei,Rutter N W et al.Towards an orbital time scale for Chinese loess deposits.Quaternary Science Reviews,1994,13(1):39～70
[53]
Xiao Jule,Porter S C,An Zhisheng et al.Grain size of quartz as an indicator of winter monsoon strength on the Loess Plateau of Central China during the last 130000yr.Quaternary Research,1995,43(1):22～29
[54]
Sun Youbin,Lu Huayu,An Zhisheng.Grain size of loess,palaeosol and red clay deposits on the Chinese Loess Plateau:Significance for understanding pedogenic alteration and palaeomonsoon evolution.Palaelgeography,Palaeoclimatology,Palaeoecology,2006,241(1):129～138
[55]
Sun Donghuai,Su Ruixia,Bloemendal J et al.Grain-size and accumulation rate records from Late Cenozoic aeolian sequences in Northern China:Implications for variations in the East Asian winter monsoon and westerly atmospheric circulation.Palaeogeography,Palaeoclimatology,Palaleoecology,2008,264(1～2):39～53
[56]
Lu Huayu,Liu Xiaodong,Zhang Fuqing et al.Astronomical calibration of loess-paleosol deposits at Luochuan,Central Chinese Loess Plateau.Palaeogeography,Palaeoclimatology,Palaleoecology,1999,154(3):237～246
[57]
Porter S C,An Zhisheng.Correlation between climate events in the North Atlantic and China during the last glaciation.Nature,1995,375:305～308
[58]
汪海斌,陈发虎,张家武.黄土高原西部地区黄土粒度的环境指示意义.中国沙漠,2002,22(1):21～26 Wang Haibin,Chen Fahu,Zhang Jiawu.Environmental significance of grain size of loess-paleosol sequence in western part of Chinese Loess Plateau.Journal of Desert Research,2002,22(1):21～26
[59]
鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义.中国科学(D辑),1998,28(3):278～283 Lu Huayu,An Zhisheng.Paleoclimatic significance of grain size of loess-paloesol deposit in Chinese Loess Plateau.Science in China(Series D),1998,41(6):626～631
[60]
刘东生等著.黄土与环境.北京:科学出版社,1985.1～481 Liu Tungsheng et al.Loess and the Environment.Beijing:Science Press,1985.1～481
[61]
安芷生,Kukla G,刘东生.洛川黄土地层学.第四纪研究,1989,(2):155～168 An Zhisheng,Kukla G,Liu Tungsheng.Loess stratigraphy in Luochuan of China.Quaternary Sciences,1989,(2):155～168
[62]
杨小强,李华梅.泥河湾盆地沉积物粒度组分与磁化率变化相关性研究.沉积学报,2002,20(4):675～679 Yang Xiaoqiang,Li Huamei.The correlation between the content of the different grain size and magnetic susceptibility in lacustrine sediments,Nihewan Basin.Acta Sedimentologica Sinica,2002,20(4):675～679
[63]
刘平,靳春胜,张崧等.甘肃龙担早第四纪黄土-古土壤序列磁组构特征与古风场恢复.科学通报,2007,52(24):2922～2924 Liu Ping,Jin Chunsheng,Zhang Song et al.Magnetic fabric of Early Quaternary loess-paleosols of Longdan profile in Gansu Province and the reconstruction of the paleowind directions.Chinese Science Bulletin,2008,53(9):1450～1452
[64]
黄孝刚,孙继敏.末次冰期以来黄土-古土壤序列的磁组构特征及其指示的古风向.第四纪研究,2005,25(4):516～522 Huang Xiaogang,Sun Jimin.Study of the magnetic fabrics in Chinese loess-paleosols since the last interglacial:Implication of the paleowind direction.Quaternary Sciences,2005,25(4):516～522
[65]
孙继敏,丁仲礼,刘东生等.黄土与古土壤磁组构测定在重建冬季风风向上的初步应用.科学通报,1995,40(21):1976～1978 Sun Jimin,Ding Zhongli,Liu Tungsheng et al.Primary application of magnetic susceptibility measurement of loess and paleosols for reconstruction of winter monsoon direction.Chinese Science Bulletin,1995,40(21):1976～1978
[66]
吴海斌,陈发虎,王建民等.现代风成沉积物磁化率各向异性与风向关系的研究.地球物理学报,1998,41(6):811～817 Wu Haibin,Chen Fahu,Wang Jianmin et al.A study on the relationship between magnetic anisotropy of modern eolian sediments and wind direction.Acta Geophysica Sinica,1998,41(6):811～817
[67]
钟巍.中国陇西盆地风成黄土沉积磁组构特征研究.新疆大学学报(自然科学版),1996,13(1):84～87 Zhong Wei.The preliminary study on the magnetic fabric features of eolian loess deposits in Longxi Basin,China.Journal of Xinjiang University(Natural Science),1996,13(1):84～87
[68]
朱艳明,周力平,张世红.中国北方上新世晚期-更新世早期风成沉积物磁化率各向异性初探.第四纪研究,2007,27(6):1009～1015 Zhu Yanming,Zhou Liping,Zhang Shihong.A preliminary study on anisotropy of magnetic susceptibility of the Late Pliocene-Early Pleistocene aeolian deposits in Northern China.Quaternary Sciences,2007,27(6):1009～1015
[69]
朱日祥,邓成龙,潘永信.泥河湾盆地磁性地层定年与早期人类演化.第四纪研究,2007,27(6):922～944 Zhu Rixiang,Deng Chenglong,Pan Yongxin.Magnetochronology of the fluvio-lacustrine sequences in the Nihewan Basin and its implications for early human colonization of North East Asia.Quaternary Sciences,2007,27(6):922～944
[70]
Deng Chenglong,Zhu Rixiang,Zhang Rui et al.Timing of the Nihewan formation and faunas.Quaternary Research,2008,69(1):77～90
