[1] 李俊武,代廷勇,李凤杰,等. 柴达木盆地鄂博梁地区古近系沉 积物源方向分析[J]. 沉积学报,2015,55(4):649-658.[LI Junwu, DAI Tingyong,LI Fengjie,et al. The analysis of ancient sediments source direction in Qaidam Basin Bayan Obo beam area[J]. Acta Sediementologica Sinica,2015,55(4):649-658.][2] 李小妹,严平,吴伟,等. 毛布拉格孔兑地表风沙沉积物粒度与 地球化学元素分布特征[J]. 干旱区地理,2016,39(3):468- 476.[LI Xiaomei,YAN Ping,WU Wei,et al. Spatial distribution characteristics of the grain size and geochemical elmments of surface sidiments of Mu Bulag Riaver[J]. Arid Land Geography, 2016,39(3):468-476.][3] 丁宏伟,姚吉禄,何江海. 张掖市地下水位上升区环境同位素特 征及补给来源分析[J]. 干旱区地理,2009,32(1):1-8.[DING Hongwei,YAO Jilu,HE Jianghai. Environmental isotope characteristics and groundwater recharge in groundwater level rise area in Zhangye City[J]. Arid Land Geography,2009,32(1):1-8.][4] THOMPOSON R,OLDFIELD F. Environmental magnetism[M]. London:Allen&Unwin,1986:1-227.[5] EVANSM,HELLER F. Environmental magnetise:principles and applications of enviromagneyics[M]. London:Academic Press,2003:68-77.[6] 陈杰,杨太保,曾彪,等. 中国帕米尔地区黄土磁化率特征及其 影响因素[J]. 干旱区地理,2016,39(4):761-769.[CHEN Jie, YANG Taibao,ZENG Biao,et al. Magnetic susceptibility features and influencing factors in Pamir,China[J]. Arid Land Geography, 2016,39(4):761-769.][7] PULLEY S,ROWNTREE K. Stages in the life of a magnetic grain:Sediment source discrimination,particle size effects and spatial variability in the South African Karoo[J]. Geoderma, 2016,271:134-143.[8] HANSON MA,ENKIN R J,BARENDREGT R W,et al. Provenance and deposition of glacial Lake Missoula lacustrine and flood sediments determined from rock magnetic properties[J]. Quaternary Research,2015,83(1):166-177.[9] PRAJITH A,RAO P V,KESSARKAR P M. Magnetic properties of sediments in cores from the Mandovi estuary,western India: inferences on provenance and pollution[J]. Marine Pollution Bulletin,2015,99(1-2):338-345.[10] 卢升高,俞劲炎,章明奎,等. 长江中下游第四纪沉积物发育土 壤磁性增强的环境磁性机制[J]. 沉积学报,2000,18(3):336- 340.[LU Shenggao,YU Jinyan,ZHANG Mingkui,et al. The enhance mechanism of the environmental development of quaternary sediments soil magnetism in the middle and lower reaches of the Yangtze River[J]. Acta Sediementologica Sinica,2000,18 (3):336-340.][11] 周立旻,郑详民,王辉,等. 长江中下游河流沉积物磁性特征初 探[J]. 华东师范大学(自然科学版),2008,6:24-30.[ZHOU Limin,ZHENG Xiangmin,WANG Hui. The analysis of magnetic properties of sediments in middle and lower Yangtze River[J]. Journal of East China Normal University(Natural Science), 2008,6:24-30.][12] 赵静,黄强,刘登峰. 渭河流域水沙演变规律分析[J]. 水力发电 学报,2015,34(3):14-20.[ZHAO Jing,HUANG Qiang,LIU Dengfeng. The analysis of water and sediment evolution law in Weihe River[J]. Journal of Hydroelectric Engineering,2015,34 (3):14-20.][13] 杨小刚,宋进喜,陈佳,等. 渭河陕西段潜流带沉积物重金属 变化初步分析[J]. 环境科学学报,2014,34(8):2051-2060.[YANG Xiaogang,SONG Jinxi,CHEN Jia,et al. The preliminary analysis of the changes for the sediments heavy metals in Weihe River[J]. Acta Scientiae Circumstantiae,2014,34(8): 2051-2060.][14] 石彬楠,黄春长,庞奖励,等. 渭河上游天水东段全新世古洪水 水文学恢复研究[J]. 干旱区地理,2016,39(3):573-581.[SHI Binnan,HUANG Chunchang,PANG Jiangli,et al. Hydrological reconstructions of the Holocene Palaeoflood in the Tianshui East Reach of the upper Weihe River[J]. Arid Land Geography, 2016,39(3):573-581.][15] 张朝锋. 渭河地堑的形成演化及其动力学机制[D]. 西安:西北 大学,2011.[ZHANG Chaofeng. The formation and evolution and its dynamics in Weihe graben[D]. Xi'an:Northwestern University, 2011.][16] 陈学刚,魏疆,孙慧兰,等. 乌鲁木齐市土壤环境磁学特征及其 空间变化研究[J]. 干旱区地理,2014,37(2):265-272.[CHEN Xuegang,WEI Jiang,SUN Huilan,et a1. Environmental magnetic properties and their spatial variability of topsoil in Urumqi City[J]. Arid Land Geography,2014,37(2):265-272.][17] LIU Q S,ROBERTS A P,LARRASOANA J C,et al. Environmental magnetism:principles and applications[J]. Reviews of Geophysics,2013,50(4):197-215.[18] DEARING J A,BIRD PM,DANN R J L,et a1. Secondary ferrimagnetic minerals in Welsh soils:a comparison of mineral magnetic detection methods and implications for mineral formation[J]. Geophysical Journal International,1997,130(3):727-736.[19] EVANS M E,HELLER F. Environmental magnetism:principles and applications of enviromagnetics[M]. London:Academic Press,2003:68-77.[20] 刘青松,邓成龙. 磁化率及其环境意义[J]. 地球物理学报, 2009,52(4):1041-1048.[LIU Qingsong,DENG Chenglong. Magnetic susceptibility and its environmental significance[J]. Chinese Journal of Geophysics,2009,52(4):1041-1048.][21] DENG C L,ZHU R X,JACKSON M J,et a1. Variability of the temperature-dependent susceptibility of the Holocene eolin deposits in the Chinese Loess Plateau:A pedogenesis indicator[J]. Physics and Chemistry of the Earth(Part A),2001,26(11-12): 873-878.[22] 秦华峰,刘青松,潘永信. 一阶反转曲线(FORC)图的原理及应 用实例[J]. 地球物理学报,2008,51(3):743-751.[QIN Huafeng, LIU Qingsong,PAN Yongxin. The first-order reversal curve (FORC)diagram:theory and case study[J]. Chinese Journal of Geophysics,2008,51(3):743-751.][23] KING J,BANERJEE S K,MARVIN J,et a1. A comparison of different magnetic methods for determining the relative grain size of magnetite in natural materials:some results from lake sediments[J]. Earth and Planetary Science Letters,1982,59(2): 404-419. |