长江三角洲地区晚新生代沉积物岩石磁学特征及其物源指示意义
|
摘要
对长江三角洲地区7个晚新生代钻孔沉积物的岩石地层和磁化率特征进行详细对比,并进一步选择浦东机场孔(PD孔)进行了详细的岩石磁学测试,讨论了该地区的晚新生代沉积物物源的演变。结果显示沉积物磁性的4次显著变化:1)各钻孔上新世磁性强弱差异明显;2)早更新世早期本区普遍表现出弱磁性;3)从早更新世中晚期至全新世,磁性强度一般随粒度粗细变化波动,即砂质沉积磁性强,泥质沉积磁性弱;4)晚更新世晚期以来,细颗粒沉积物的磁性较明显增强。磁性参数分析显示上新世和早更新世早期磁性矿物晶体颗粒较细,早更新世中晚期-晚更新世以粗晶粒磁性矿物为主,全新世细晶粒磁铁矿再次占主导。我们认为上述磁性变化反映构造沉降控制下现代长江三角洲地区物源区的不断扩大。
Lithostratigraphy and magnetic properties of sediments from 7 Late Cenozoic boreholes ( SG6, SG7, SG8, SG10, SG13 ,J18A, and PD)drilled in the Yangtze delta area were analyzed to reveal the sediment source and its change in this area. Paleomagnetism was measured for all boreholes with the sampling intervals of 1.0 ~ 1.5m. The sediments of PD were further measured for rock magnetic property with a mean sampling interval of ca. 4m. The results show that gravelly sand and hard clay dominate the sediments deposited during Pliocene to mid-Pleistocene. Fine-grained soft sediments mainly occur after Late Pleistocene. Results also show that magnetic susceptibility changes significantly among Pliocene sediments in 7 boreholes. The strongest magnetic susceptibility is found in SGT, exceeding 200, which is believed to be contributed by the local bedrock of basalt. By contrast, magnetic susceptibility is generally weak in other boreholes. Palaeotopography is suggested to control the spatial distribution of magnetic properties and the associated local sediment source. During early stage of Early Pleistocene, magnetic signals become extremely weak in all boreholes,suggesting a uniform sediment source. During the middle and late stages of Early Pleistocene to Holocene, magnetic susceptibility fluctuates along with the change of grain size of sediments. It is stronger in sandy sediments and weaker in muddy sediments, reflecting new sediment source of rich magnetic minerals. Since the Late Pleistocene, magnetic susceptibility of fine-grained sediments enhanced obviously. This indicates the increase of fine-grained magnetic mineral that is possibly contributed from the upper Yangtze drainage basin. Rock Magnetic property analysis of PD demonstrates that magnetite is the major magnetic mineral and its crystal particle size is smaller in Pliocene and the early stage of Early Pleistocene,and bigger during the middle and late stages of Early Pleistocene to Late Pleistocene. Fine-grained magnetite dominated Holocene sediments again. We believe that these magnetic changes reflect the sediment sources of the present Yangtze delta area which kept on expanding during Late Cenozoic era under the control of the tectonic subsidence.
Lithostratigraphy and magnetic properties of sediments from 7 Late Cenozoic boreholes ( SG6, SG7, SG8, SG10, SG13 ,J18A, and PD)drilled in the Yangtze delta area were analyzed to reveal the sediment source and its change in this area. Paleomagnetism was measured for all boreholes with the sampling intervals of 1.0 ~ 1.5m. The sediments of PD were further measured for rock magnetic property with a mean sampling interval of ca. 4m. The results show that gravelly sand and hard clay dominate the sediments deposited during Pliocene to mid-Pleistocene. Fine-grained soft sediments mainly occur after Late Pleistocene. Results also show that magnetic susceptibility changes significantly among Pliocene sediments in 7 boreholes. The strongest magnetic susceptibility is found in SGT, exceeding 200, which is believed to be contributed by the local bedrock of basalt. By contrast, magnetic susceptibility is generally weak in other boreholes. Palaeotopography is suggested to control the spatial distribution of magnetic properties and the associated local sediment source. During early stage of Early Pleistocene, magnetic signals become extremely weak in all boreholes,suggesting a uniform sediment source. During the middle and late stages of Early Pleistocene to Holocene, magnetic susceptibility fluctuates along with the change of grain size of sediments. It is stronger in sandy sediments and weaker in muddy sediments, reflecting new sediment source of rich magnetic minerals. Since the Late Pleistocene, magnetic susceptibility of fine-grained sediments enhanced obviously. This indicates the increase of fine-grained magnetic mineral that is possibly contributed from the upper Yangtze drainage basin. Rock Magnetic property analysis of PD demonstrates that magnetite is the major magnetic mineral and its crystal particle size is smaller in Pliocene and the early stage of Early Pleistocene,and bigger during the middle and late stages of Early Pleistocene to Late Pleistocene. Fine-grained magnetite dominated Holocene sediments again. We believe that these magnetic changes reflect the sediment sources of the present Yangtze delta area which kept on expanding during Late Cenozoic era under the control of the tectonic subsidence.
引文
1 范代读,李从先,YokoyamaK等.长江三角洲晚新生代地层独居石年龄谱与长江贯通时间研究.中国科学(D辑),2004,34(11) :1015~1022Fan Daidu, Li Congxian, Yokoyama K et al. Monazite age spectra in the Late Cenozoic strata of the Changjiang delta and its implication on the Changjiang run-through time. Science in China ( Series D) ,2005,48(10) : 1718~1727
2 陈静,王哲,王张华等.长江三角洲东西部晚新生代地层中的重矿物差异及其物源意义.第四纪研究,2007,27(5) :700~708Chen Jing, Wang Zhe, Wang Zhanghua et al. Heavy mineral distribution and its provenance implication in Late Cenozoic sediments in western and eastern area of the Changjiang River delta.Quaternary Sciences ,2007 ,27 (5 ) : 700~708
3 杨守业,韦刚键,夏小平等.长江口晚新生代沉积物的物源研究:REE和Nd同位素地制约.第四纪研究,2007,27(3) :339~346Yang Shouye,Wei Cangjian,Xia Xiaoping et al. Provenance study of the Late Cenozoic sediments in the Changjiang delta: REE and Nd isotopic constraints. Quaternary Sciences,2007 ,27(3) : 339~346
4 范代读,李从先,Yokoyama K等.河口地层独居石Th(U)-Pb 年龄对长江贯通时限的约束.海洋地质动态,2006,22(7) :11~15Fan Daidu, Li Congxian, Yokoyama K et al. Constraints on the Yangtze River running-through time, using Th ( U )-Pb dating of Monazite. Marine Geology Letters ,2006,22(7) : 11~15
5 Thompson R, Oldfield F. Environmental Magnetism. London: George Allen & Unwin,1986. 227
6 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) :193~209Deng Chenglong, Liu Qingsong, Pan Yongxin et al. Environmental magnetism of Chinese loess-paleosol sequences. Quaternary Sciences,2007 ,27(2) : 193~209
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.第四纪研究,2007,27(2) :210~220Liu 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
8 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) :989~1000Fang 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
9 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) :1009~1015Zhu 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
10 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) :954~962Liu 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
11 夏敦胜,魏海涛,马剑英等.中亚地区现代表土磁学特征及其古环境意义.第四纪研究,2006,26(6) :937~946Xia Dunsheng, Wei Haitao, Ma Jianying et al. Magnetic characteristics of surface soil in arid region of Central Asia and their paleoenvironmental significance. Quaternary Sciences,2006 ,26(6) :937-946
12 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) :1001~1108Xia Dunsheng, Chen Fahu, Ma 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) : 1001~1108
13 张卫国,戴雪荣,张福瑞等.近7000年巢湖沉积物环境磁学特征及其指示的亚洲季风变化.第四纪研究,2007,27(6) :1053~1062Zhang Weiguo,Dai Xuerong,Zhang Furui et al. Magnetic properties of sediments from the Chaohu Lake for the last 7000 years and their implications for the evolution of Asian monsoon. Quaternary Sciences,2007,27(6) : 1053~1062
14 张春霞,黄宝春,骆仁松等.钢铁厂附近树木年轮的磁学性质及其环境意义.第四纪研究,2007,27(6) :1092~1104Zhang Chunxia, Huang Baochun, Luo Rensong et al. Magnetic properties of tree ring samples close to a smelting factory and their environmental significance. Quaternary Sciences, 2007, 27 ( 6 ) :1092~1104
15 沈明洁,胡守云,Blaha U等.土壤剖面的磁学特征及其对交通污染的指示意义--以北京首都机场高速公路为例.第四纪研究,2007,27(6) :1113~1120Shen Mingjie, Hu Shouyun, Blaha U et al. Mineral magnetic properties of soil profile and their application in traffic pollution measurements: A case study from the capital airport expressway in Beijing. Quaternary Sciences,2007 ,27(6) : 1113~1120
16 段雪梅,胡守云,杨涛.武汉市汤逊湖沉积物重金属垂向变化的磁响应特征及环境意义.第四纪研究,2007,27(6) :1105~1112Duan Xuemei, Hu Shouyun, Yang Tao. Vertical variation of heavy metals and it's magnetic reponse property and environmental significance in core sediment from Lake Tangxun, Wuhan, China. Quaternary Sciences ,2007 ,27(6) : 1105~1112
17 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.第四纪研究,2008,28(4) :640~648Wang Hui, Zheng Xiangmin, Wang Xiaoyong et al. Environmental magnetic properties of sediments from middle and lower reaches of Changjiang River. Quaternary Sciences ,2008 ,28(4) : 640~648
18 葛淑兰,石学法,韩贻兵南黄海海底沉积物的磁化率特征.科学通报,2001,46(增刊):34~38Ge Shulan, Shi Xuefa, Han Yibing. Magnetic susceptibility characteristics of the South Yellow Sea seabed sediment. Chinese Science Bulletin ,2001 ,46(Suppl. ) : 34~38
19 Liu Jian, Zhu Rixiang,Li Guangxue. Rock magnetic properties of the fine~grained sediment on the outer shelf of the East China Sea: Implication for provenance. Marine Geology ,2003,193: 195~206
20 李萍,李培英,张晓龙等.冲绳海槽沉积物不同粒级的磁性特征及其与环境的关系.科学通报,2005,50(3) :262~268Li Ping,Li Peiying,Zhang Xiaolong et al. Okinawa Trough sediments magnetic characteristics with different grain size and their relationship between environment. Chinese Science Bulletin ,2005 ,50 (3) : 262~268
21 张玉芬,李长安,王秋良等.江汉平原沉积物磁学特征及对长江三峡贯通的指示.科学通报,2008,53(5) :577~582Zhang Yufen, Li Chang'an, Wang Qiuliang et al. Jianghan Plain magnetic characteristics of the sediments and the Three Gorges on the Yangtze River through the instructions. Chinese Science Bulletin,2008,53(5) : 577~582
22 (苏)金兹堡А И著,徐海江,王剑锋译.成因矿物学概论.北京:地质出版社,1982. 1~133Ginzburg A H, Translator by Xu Haijiang, Wang Jianfeng.OnepKHno feHeTHHecKoft MHHepa;iOTHH. Beijing: Geological Publishing House, 1982. 1-133
23 林师整.磁铁矿矿物化学、成因及演化的探讨.矿物学报,1982,(3) :166~174Lin Shizheng. A contribution to the chemistry, origin and evolution of magnetite. Acta Mineralogica Sinica, 1982,(3) : 166~174
24 王顺金.论磁铁矿的标型特征.矿物学岩石学论丛,1987,(3) :139~154 Wang Shunjin. The typical characteristics of magnetite. Collection of Mineralogy and Petrology,1987 ,(3) : 139~154
25 陈光远,孙岱生,殷辉安.成因矿物学与找矿矿物学.重庆:重庆出版社,1987. 234~235Chen Guangyuan, Sun Daisheng, Yin Hui'an. Genetic Mineralogy and Prospecting Mineralogy. Chongqing: Chongqing Press, 1987. 234~235
26 Nielsen R L, Forsythe L M, Gallahan W E et al. Major-and trace-element magnetite-melt equilibria. Chemical Geology, 1994 , 117 :167~191
27 王张华,张丹,李晓等.长江三角洲地区晚新生代沉积物磁性和磁性矿物分布特征及其对物源、古地理环境演变的指示意义.中国地质,2008,35(4) :670~682Wang Zhanghua, Zhang Dan , Li Xiao et al. Magnetic properties and relevant minerals of Late Cenozoic sediments in the Yangtze River delta and their implications. Geology in China ,2008 ,35(4) : 670~682
28 孙秀荣,戴纯俊,刘志高等.长江三角洲南翼晚更新世-全新世沉积物地球物理研究.物探与化探,2002,26(3) :175~178Sun Xiurong,Dai Chunjun,Liu Zhigao et al. Geophysical studies of Epipleistocene-Holocene sediments in the southern limb of the Yangtze Delta. Geophysical and Geochemical Exploration ,2002 ,26(3) : 175~178
29 魏子新.长江三角洲东部第四纪沉积环境演化新构造运动古气候与海平面变化的耦合作用.上海:华东师范大学资源与环境科学学院博士论文,2003. 1~116Wei Zixin. Quaternary Environmental Evolution in Eastern Yangtze Delta: Coupling of Neotectonic Movement, Paleoclimate and Sealevel Fluctuation. Shanghai: East China Normal University, Ph. D Dissertation, 2003. 1~116
30 王张峤,陈中原,魏子新等.长江口第四纪沉积物中构造与古气候耦合作用的探讨.科学通报,2005,50(14) :1503~1511Wang Zhangjiao,Chen Zhongyuan , Wei Zixin et al. Coupling controls of neotectonism and paleoclimate on the Quaternary sediments of the Yangtze ( Changjiang ) coast. Chinese Science Bulletin, 2005, 50 (14) : 1503~1511
31 丁元陶.长江三角洲东部沉积物粒度特征及其环境意义.资源调查与环境,2006,27(4) :261~267Ding Yuantao. Grain-size characteristics of the eastern Yangtze delta sediments and its environmental implication. Resources Survey & Environment ,2006 ,27(4) : 261~267
32 王建华,周洋,郑卓等.杭州湾晚第四纪沉积与古环境演变.古地理学报,2006,8(4) :551~558Wang Jianhua, Zhou Yang, Zhen Zhuo et al. Late Quaternary sediments and paleoenvironmental evolution in Hangzhou Bay. Journal of Palaeogeography, 2006,8(4) : 551~558
33 郭玉贵,李延成,许东禹等.黄东海大陆架及邻域大地构造演化史.海洋地质与第四纪地质,1997,17(1) :1~11Guo Yugui, Li Yanchen, Xu Dongyu et al. Tectonic evolution of Yellow Sea, East China Sea and continental shelf and adjacent areas. Marine Geology & Quaternary Geology, 1997 ,17( 1) : 1~11
34 程三友.中国东北地区区域构造特征与中新生代盆地演化.北京:中国地质大学(北京)博士论文,2006. 1~121Cheng Sanyou. Regional Tectonic Characters and Meso-Cenozoic Basin Evolution in North Eastern China. Beijing: China University of Geosciences, Ph. D Dissertation ,2006. 1~121
35 李延栋,莫杰.中国滨太平洋构造域构造格架和东海地质演化.海洋地质与第四纪地质,2002,22(4) :1~6Li Yangdong, Mo Jie. Tectionic framework of the West Circumpacific tectonic tract and the geological evolution of the East China Sea. Marine Geology & Quaternary Geology ,2002 ,22(4) : 1~6
36 Chen Zhongyuan, Stanley D J. Quaternary subsidence and river channel migration in the Yangtze Delta Plain, Eastern China. Journal of Coastal Research, 1995 ,11: 927~945
37 陈中原.长江三角洲之沉降.火山地质与矿产,2001,22(2) :95~101Chen Zhongyuan. Yangtze delta subsidence. Volcanology & Mineral Resources,2001,22(2) : 95~101
38 秦大正.上海覆盖区活断层.地震地质,1994,16(2) :160~166
Qin Dazhen. The active fault in Shanghai overburden area. Seismology and Geology,1994 ,16(2) : 160~166
39 章震铨,刘昌森.上海两条隐伏第四纪断裂的研究.地震地质,2001,23(4) :545~555Zhang Zhenshuan, Liu Changsen. Research on two buried Quaternary faults in Shanghai. Seismology and Geology, 2001 , 23 (4) : 545~555
40 Oldfield F. Environmental magnetism--A personal perspective. Quaternary Science Reviews, 1991 ,10: 73~85
41 董瑞斌,张卫国,卢升高等.土壤和沉积物的磁参数及其在环境科学中的应用.科技通报,2000,16(6) :479~483Dong Ruibin,Zhang Weiguo,Lu Shenggao et al. The magnetic indexes for soil and sediment and their applications on environmental studies. Bulletin of Science and Technology, 2000,16(6) : 479-483
42 王润华,郭坤一,于振江等.长江三角洲地区第四纪磁性地层学研究.地层学杂志,2005,29(增刊):612~617Wang Runhua,Guo Kunyi,Yu Zhenjiang et al. Quaternary magneto-stratigraphy of the Yangtze delta area. Journal of Stratigraphy,2005,29 (Suppl. ): 612~617
43 汪品先.亚洲形变与全球变冷--探索气候与构造的关系.第四纪研究,1998,(3) :213~221Wang Pingxian. Deformation of Asia and global cooling: Searching links between climate and tectonics. Quaternary Sciences, 1998,(3) : 213~221
44 施雅风,李吉均,李炳元等.晚新生代青藏高原的隆升与东亚环境变化.地理学报,1999,54(1) :10~20Shi Yafeng,Li Jijun,Li Bingyuan et al. Uplift of the Qinghai-Xizang ( Tibetan) Plateau and East Asia environmental change during Late Cenozoic. Acta Geographica Sinica, 1999,54 (1) : 10-20
2 陈静,王哲,王张华等.长江三角洲东西部晚新生代地层中的重矿物差异及其物源意义.第四纪研究,2007,27(5) :700~708Chen Jing, Wang Zhe, Wang Zhanghua et al. Heavy mineral distribution and its provenance implication in Late Cenozoic sediments in western and eastern area of the Changjiang River delta.Quaternary Sciences ,2007 ,27 (5 ) : 700~708
3 杨守业,韦刚键,夏小平等.长江口晚新生代沉积物的物源研究:REE和Nd同位素地制约.第四纪研究,2007,27(3) :339~346Yang Shouye,Wei Cangjian,Xia Xiaoping et al. Provenance study of the Late Cenozoic sediments in the Changjiang delta: REE and Nd isotopic constraints. Quaternary Sciences,2007 ,27(3) : 339~346
4 范代读,李从先,Yokoyama K等.河口地层独居石Th(U)-Pb 年龄对长江贯通时限的约束.海洋地质动态,2006,22(7) :11~15Fan Daidu, Li Congxian, Yokoyama K et al. Constraints on the Yangtze River running-through time, using Th ( U )-Pb dating of Monazite. Marine Geology Letters ,2006,22(7) : 11~15
5 Thompson R, Oldfield F. Environmental Magnetism. London: George Allen & Unwin,1986. 227
6 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) :193~209Deng Chenglong, Liu Qingsong, Pan Yongxin et al. Environmental magnetism of Chinese loess-paleosol sequences. Quaternary Sciences,2007 ,27(2) : 193~209
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.第四纪研究,2007,27(2) :210~220Liu 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
8 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) :989~1000Fang 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
9 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) :1009~1015Zhu 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
10 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) :954~962Liu 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
11 夏敦胜,魏海涛,马剑英等.中亚地区现代表土磁学特征及其古环境意义.第四纪研究,2006,26(6) :937~946Xia Dunsheng, Wei Haitao, Ma Jianying et al. Magnetic characteristics of surface soil in arid region of Central Asia and their paleoenvironmental significance. Quaternary Sciences,2006 ,26(6) :937-946
12 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) :1001~1108Xia Dunsheng, Chen Fahu, Ma 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) : 1001~1108
13 张卫国,戴雪荣,张福瑞等.近7000年巢湖沉积物环境磁学特征及其指示的亚洲季风变化.第四纪研究,2007,27(6) :1053~1062Zhang Weiguo,Dai Xuerong,Zhang Furui et al. Magnetic properties of sediments from the Chaohu Lake for the last 7000 years and their implications for the evolution of Asian monsoon. Quaternary Sciences,2007,27(6) : 1053~1062
14 张春霞,黄宝春,骆仁松等.钢铁厂附近树木年轮的磁学性质及其环境意义.第四纪研究,2007,27(6) :1092~1104Zhang Chunxia, Huang Baochun, Luo Rensong et al. Magnetic properties of tree ring samples close to a smelting factory and their environmental significance. Quaternary Sciences, 2007, 27 ( 6 ) :1092~1104
15 沈明洁,胡守云,Blaha U等.土壤剖面的磁学特征及其对交通污染的指示意义--以北京首都机场高速公路为例.第四纪研究,2007,27(6) :1113~1120Shen Mingjie, Hu Shouyun, Blaha U et al. Mineral magnetic properties of soil profile and their application in traffic pollution measurements: A case study from the capital airport expressway in Beijing. Quaternary Sciences,2007 ,27(6) : 1113~1120
16 段雪梅,胡守云,杨涛.武汉市汤逊湖沉积物重金属垂向变化的磁响应特征及环境意义.第四纪研究,2007,27(6) :1105~1112Duan Xuemei, Hu Shouyun, Yang Tao. Vertical variation of heavy metals and it's magnetic reponse property and environmental significance in core sediment from Lake Tangxun, Wuhan, China. Quaternary Sciences ,2007 ,27(6) : 1105~1112
17 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.第四纪研究,2008,28(4) :640~648Wang Hui, Zheng Xiangmin, Wang Xiaoyong et al. Environmental magnetic properties of sediments from middle and lower reaches of Changjiang River. Quaternary Sciences ,2008 ,28(4) : 640~648
18 葛淑兰,石学法,韩贻兵南黄海海底沉积物的磁化率特征.科学通报,2001,46(增刊):34~38Ge Shulan, Shi Xuefa, Han Yibing. Magnetic susceptibility characteristics of the South Yellow Sea seabed sediment. Chinese Science Bulletin ,2001 ,46(Suppl. ) : 34~38
19 Liu Jian, Zhu Rixiang,Li Guangxue. Rock magnetic properties of the fine~grained sediment on the outer shelf of the East China Sea: Implication for provenance. Marine Geology ,2003,193: 195~206
20 李萍,李培英,张晓龙等.冲绳海槽沉积物不同粒级的磁性特征及其与环境的关系.科学通报,2005,50(3) :262~268Li Ping,Li Peiying,Zhang Xiaolong et al. Okinawa Trough sediments magnetic characteristics with different grain size and their relationship between environment. Chinese Science Bulletin ,2005 ,50 (3) : 262~268
21 张玉芬,李长安,王秋良等.江汉平原沉积物磁学特征及对长江三峡贯通的指示.科学通报,2008,53(5) :577~582Zhang Yufen, Li Chang'an, Wang Qiuliang et al. Jianghan Plain magnetic characteristics of the sediments and the Three Gorges on the Yangtze River through the instructions. Chinese Science Bulletin,2008,53(5) : 577~582
22 (苏)金兹堡А И著,徐海江,王剑锋译.成因矿物学概论.北京:地质出版社,1982. 1~133Ginzburg A H, Translator by Xu Haijiang, Wang Jianfeng.OnepKHno feHeTHHecKoft MHHepa;iOTHH. Beijing: Geological Publishing House, 1982. 1-133
23 林师整.磁铁矿矿物化学、成因及演化的探讨.矿物学报,1982,(3) :166~174Lin Shizheng. A contribution to the chemistry, origin and evolution of magnetite. Acta Mineralogica Sinica, 1982,(3) : 166~174
24 王顺金.论磁铁矿的标型特征.矿物学岩石学论丛,1987,(3) :139~154 Wang Shunjin. The typical characteristics of magnetite. Collection of Mineralogy and Petrology,1987 ,(3) : 139~154
25 陈光远,孙岱生,殷辉安.成因矿物学与找矿矿物学.重庆:重庆出版社,1987. 234~235Chen Guangyuan, Sun Daisheng, Yin Hui'an. Genetic Mineralogy and Prospecting Mineralogy. Chongqing: Chongqing Press, 1987. 234~235
26 Nielsen R L, Forsythe L M, Gallahan W E et al. Major-and trace-element magnetite-melt equilibria. Chemical Geology, 1994 , 117 :167~191
27 王张华,张丹,李晓等.长江三角洲地区晚新生代沉积物磁性和磁性矿物分布特征及其对物源、古地理环境演变的指示意义.中国地质,2008,35(4) :670~682Wang Zhanghua, Zhang Dan , Li Xiao et al. Magnetic properties and relevant minerals of Late Cenozoic sediments in the Yangtze River delta and their implications. Geology in China ,2008 ,35(4) : 670~682
28 孙秀荣,戴纯俊,刘志高等.长江三角洲南翼晚更新世-全新世沉积物地球物理研究.物探与化探,2002,26(3) :175~178Sun Xiurong,Dai Chunjun,Liu Zhigao et al. Geophysical studies of Epipleistocene-Holocene sediments in the southern limb of the Yangtze Delta. Geophysical and Geochemical Exploration ,2002 ,26(3) : 175~178
29 魏子新.长江三角洲东部第四纪沉积环境演化新构造运动古气候与海平面变化的耦合作用.上海:华东师范大学资源与环境科学学院博士论文,2003. 1~116Wei Zixin. Quaternary Environmental Evolution in Eastern Yangtze Delta: Coupling of Neotectonic Movement, Paleoclimate and Sealevel Fluctuation. Shanghai: East China Normal University, Ph. D Dissertation, 2003. 1~116
30 王张峤,陈中原,魏子新等.长江口第四纪沉积物中构造与古气候耦合作用的探讨.科学通报,2005,50(14) :1503~1511Wang Zhangjiao,Chen Zhongyuan , Wei Zixin et al. Coupling controls of neotectonism and paleoclimate on the Quaternary sediments of the Yangtze ( Changjiang ) coast. Chinese Science Bulletin, 2005, 50 (14) : 1503~1511
31 丁元陶.长江三角洲东部沉积物粒度特征及其环境意义.资源调查与环境,2006,27(4) :261~267Ding Yuantao. Grain-size characteristics of the eastern Yangtze delta sediments and its environmental implication. Resources Survey & Environment ,2006 ,27(4) : 261~267
32 王建华,周洋,郑卓等.杭州湾晚第四纪沉积与古环境演变.古地理学报,2006,8(4) :551~558Wang Jianhua, Zhou Yang, Zhen Zhuo et al. Late Quaternary sediments and paleoenvironmental evolution in Hangzhou Bay. Journal of Palaeogeography, 2006,8(4) : 551~558
33 郭玉贵,李延成,许东禹等.黄东海大陆架及邻域大地构造演化史.海洋地质与第四纪地质,1997,17(1) :1~11Guo Yugui, Li Yanchen, Xu Dongyu et al. Tectonic evolution of Yellow Sea, East China Sea and continental shelf and adjacent areas. Marine Geology & Quaternary Geology, 1997 ,17( 1) : 1~11
34 程三友.中国东北地区区域构造特征与中新生代盆地演化.北京:中国地质大学(北京)博士论文,2006. 1~121Cheng Sanyou. Regional Tectonic Characters and Meso-Cenozoic Basin Evolution in North Eastern China. Beijing: China University of Geosciences, Ph. D Dissertation ,2006. 1~121
35 李延栋,莫杰.中国滨太平洋构造域构造格架和东海地质演化.海洋地质与第四纪地质,2002,22(4) :1~6Li Yangdong, Mo Jie. Tectionic framework of the West Circumpacific tectonic tract and the geological evolution of the East China Sea. Marine Geology & Quaternary Geology ,2002 ,22(4) : 1~6
36 Chen Zhongyuan, Stanley D J. Quaternary subsidence and river channel migration in the Yangtze Delta Plain, Eastern China. Journal of Coastal Research, 1995 ,11: 927~945
37 陈中原.长江三角洲之沉降.火山地质与矿产,2001,22(2) :95~101Chen Zhongyuan. Yangtze delta subsidence. Volcanology & Mineral Resources,2001,22(2) : 95~101
38 秦大正.上海覆盖区活断层.地震地质,1994,16(2) :160~166
Qin Dazhen. The active fault in Shanghai overburden area. Seismology and Geology,1994 ,16(2) : 160~166
39 章震铨,刘昌森.上海两条隐伏第四纪断裂的研究.地震地质,2001,23(4) :545~555Zhang Zhenshuan, Liu Changsen. Research on two buried Quaternary faults in Shanghai. Seismology and Geology, 2001 , 23 (4) : 545~555
40 Oldfield F. Environmental magnetism--A personal perspective. Quaternary Science Reviews, 1991 ,10: 73~85
41 董瑞斌,张卫国,卢升高等.土壤和沉积物的磁参数及其在环境科学中的应用.科技通报,2000,16(6) :479~483Dong Ruibin,Zhang Weiguo,Lu Shenggao et al. The magnetic indexes for soil and sediment and their applications on environmental studies. Bulletin of Science and Technology, 2000,16(6) : 479-483
42 王润华,郭坤一,于振江等.长江三角洲地区第四纪磁性地层学研究.地层学杂志,2005,29(增刊):612~617Wang Runhua,Guo Kunyi,Yu Zhenjiang et al. Quaternary magneto-stratigraphy of the Yangtze delta area. Journal of Stratigraphy,2005,29 (Suppl. ): 612~617
43 汪品先.亚洲形变与全球变冷--探索气候与构造的关系.第四纪研究,1998,(3) :213~221Wang Pingxian. Deformation of Asia and global cooling: Searching links between climate and tectonics. Quaternary Sciences, 1998,(3) : 213~221
44 施雅风,李吉均,李炳元等.晚新生代青藏高原的隆升与东亚环境变化.地理学报,1999,54(1) :10~20Shi Yafeng,Li Jijun,Li Bingyuan et al. Uplift of the Qinghai-Xizang ( Tibetan) Plateau and East Asia environmental change during Late Cenozoic. Acta Geographica Sinica, 1999,54 (1) : 10-20
目录