中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mineral magnetic variation of the Jiaodao Chinese loess/paleosol sequence and its bearing on long-term climatic variability

文献类型:期刊论文

作者Deng, CL; Vidic, NJ; Verosub, KL; Singer, MJ; Liu, QS; Shaw, J; Zhu, RX
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2005-03-31
卷号110期号:B3
ISSN号2169-9313
DOI10.1029/2004JB003451
文献子类Review
英文摘要[ 1] To retrieve reliable long-term paleoclimatic signals from the Chinese loess/paleosol sequences deposited over the past 2.6 Myr, multiparameter mineral magnetic investigations have been conducted on the Jiaodao section on the Chinese central Loess Plateau. First, the lithogenic magnetic components and the pedogenic overprinting were chemically separated by the citrate-bicarbonate-dithionite (CBD) method. The magnetic properties of the least pedogenically altered loess units and post-CBD loess/paleosols are dominated by coarse-grained lithogenic magnetite. Increasing degree of pedogenesis increases both the concentration and grain size of pedogenic magnetite/maghemite. Longterm changes of the pre-CBD magnetic properties suggest a long-term decrease in summer monsoon intensity and a long-term increase in winter monsoon intensity from the late Pliocene to the late Pleistocene. Long-term variations of the post-CBD magnetic properties suggest an increase in both concentration and grain size of coarse-grained lithogenic PSD/MD magnetite grains, and hence indicate a long-term increase in winter monsoon intensity over that period. The coercivity decrease of the lithogenic component for the loess unit L15 may be related to the accelerated uplift of the Tibetan Plateau and its adjacent regions during the period of L15 deposition. From paleosol S5 to loess L1, higher values of coercivity of the lithogenic component occur in typical loess and paleosols, and lower values are found at the loess/paleosol transition. These coercivity variations are thought to be related to significant changes in the source region as well as dust deposition in the Loess Plateau caused by changes in ice/snow or vegetational cover. These new results lead to a better understanding of the relationships between the effects of tectonic, paleoclimatic, and paleoenvironmental processes in northwestern China.
WOS关键词ISOTHERMAL REMANENT MAGNETIZATION ; LOW-TEMPERATURE OXIDATION ; LOESS-PALEOSOL SEQUENCES ; NORTH-SOUTH TRANSECT ; BICARBONATE-DITHIONITE EXTRACTION ; FINE-GRAINED MAGNETITE ; NW-SE TRANSECT ; ACQUISITION CURVES ; PALEOCLIMATIC IMPLICATIONS ; DEPENDENT SUSCEPTIBILITY
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000228369500002
出版者AMER GEOPHYSICAL UNION
源URL[http://ir.iggcas.ac.cn/handle/132A11/65795]  
专题中国科学院地质与地球物理研究所
通讯作者Deng, CL
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Paleomagnetism Lab, Beijing 100029, Peoples R China
2.Univ Ljubljana, Dept Agron, Ljubljana 1111, Slovenia
3.Univ Calif Davis, Dept Geol, Davis, CA 95616 USA
4.Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA
5.Univ Calif Santa Cruz, Dept Earth Sci, Santa Cruz, CA 95064 USA
6.Univ Liverpool, Dept Earth & Ocean Sci, Geomagnetism Lab, Liverpool L69 7ZE, Merseyside, England
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Deng, CL,Vidic, NJ,Verosub, KL,et al. Mineral magnetic variation of the Jiaodao Chinese loess/paleosol sequence and its bearing on long-term climatic variability[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2005,110(B3).
APA Deng, CL.,Vidic, NJ.,Verosub, KL.,Singer, MJ.,Liu, QS.,...&Zhu, RX.(2005).Mineral magnetic variation of the Jiaodao Chinese loess/paleosol sequence and its bearing on long-term climatic variability.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,110(B3).
MLA Deng, CL,et al."Mineral magnetic variation of the Jiaodao Chinese loess/paleosol sequence and its bearing on long-term climatic variability".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 110.B3(2005).

入库方式: OAI收割

来源:地质与地球物理研究所

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