Links between bulk sediment particle size and magnetic grain-size: general observations and implications for Chinese loess studies
文献类型:期刊论文
作者 | Oldfield, Frank1; Hao, Qingzhen1,2; Bloemendal, Jan1; Gibbs-Eggar, Zoe1,3; Patil, Shiva1,4; Guo, Zhengtang2 |
刊名 | SEDIMENTOLOGY
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出版日期 | 2009-12-01 |
卷号 | 56期号:7页码:2091-2106 |
关键词 | Environmental magnetism granulometry loess magnetic grain-size pedogenesis weathering |
ISSN号 | 0037-0746 |
DOI | 10.1111/j.1365-3091.2009.01071.x |
文献子类 | Article |
英文摘要 | Using a combination of particle size analysis, magnetic measurements, scanning electron microscopy and transmission electron microscopy imaging, this study shows that in a wide range of depositional environments, there is a strong link between particle size classes and magnetic response, especially below the upper limit of stable single domain magnetic behaviour. Ferrimagnetic grain assemblages dominated by stable single domain magnetosomes regularly have peak susceptibility and remanence values in coarser grades than do those containing finer-grained, viscous and superparamagnetic secondary magnetic minerals formed during pedogenesis. This effect is despite the fact that there is a one to two orders of magnitude size difference between the particle size boundaries (at 1 or 2 mu m) and key domain state transitions (mostly below 0 center dot 05 mu m). The implications of these results are explored using samples spanning 22 Myr of loess accumulation on the Chinese Loess Plateau. The results from the loess sections, complemented by data from low-temperature magnetic experiments, show that there are subtle distinctions in mean ferrimagnetic grain-size between the Pleistocene and Miocene parts of the record, thus allowing more refined rock magnetic interpretations of the fine-grained ferrimagnetic mineral assemblages arising from the effects of weathering, pedogenesis and possibly diagenesis in the sections studied. |
WOS关键词 | PLATEAU ; SAMPLES ; PEDOGENESIS ; MIOCENE ; RECORD ; SOILS ; EARTH ; LAKE ; SEA |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000272132000009 |
出版者 | WILEY-BLACKWELL PUBLISHING, INC |
资助机构 | National Science Foundation of China(40730104 ; National Science Foundation of China(40730104 ; Chinese Academy of Sciences(KZCX-YW-117) ; Chinese Academy of Sciences(KZCX-YW-117) ; 40672115) ; 40672115) ; National Science Foundation of China(40730104 ; National Science Foundation of China(40730104 ; Chinese Academy of Sciences(KZCX-YW-117) ; Chinese Academy of Sciences(KZCX-YW-117) ; 40672115) ; 40672115) ; National Science Foundation of China(40730104 ; National Science Foundation of China(40730104 ; Chinese Academy of Sciences(KZCX-YW-117) ; Chinese Academy of Sciences(KZCX-YW-117) ; 40672115) ; 40672115) ; National Science Foundation of China(40730104 ; National Science Foundation of China(40730104 ; Chinese Academy of Sciences(KZCX-YW-117) ; Chinese Academy of Sciences(KZCX-YW-117) ; 40672115) ; 40672115) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/71858] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Oldfield, Frank |
作者单位 | 1.Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 3.Cedars, Hereford HR1 1TS, England 4.KS Krishnan Geomagnet Res Lab IIG, Allahabad 221505, Uttar Pradesh, India |
推荐引用方式 GB/T 7714 | Oldfield, Frank,Hao, Qingzhen,Bloemendal, Jan,et al. Links between bulk sediment particle size and magnetic grain-size: general observations and implications for Chinese loess studies[J]. SEDIMENTOLOGY,2009,56(7):2091-2106. |
APA | Oldfield, Frank,Hao, Qingzhen,Bloemendal, Jan,Gibbs-Eggar, Zoe,Patil, Shiva,&Guo, Zhengtang.(2009).Links between bulk sediment particle size and magnetic grain-size: general observations and implications for Chinese loess studies.SEDIMENTOLOGY,56(7),2091-2106. |
MLA | Oldfield, Frank,et al."Links between bulk sediment particle size and magnetic grain-size: general observations and implications for Chinese loess studies".SEDIMENTOLOGY 56.7(2009):2091-2106. |
入库方式: OAI收割
来源:地质与地球物理研究所
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