中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geomagnetic paleointensity dating of South China Sea sediments for the last 130 kyr

文献类型:期刊论文

作者Yang Xiaoqiang1; Friedrich Heller2; Wu Nengyou3; Yang Jie1; Su Zhihua1
刊名earth and planetary science letters
出版日期2009-06-30
卷号284期号:1-2页码:258-266
关键词South China Sea relative paleointensity chronology
ISSN号0012-821x
通讯作者eesyxq@mail.sysu.edu.cn
中文摘要relative paleointensity records from the northern south china sea, northwest pacific ocean were studied in two gravity piston cores. continuous mineral magnetic and paleomagnetic measurements were made using discrete sediment samples. detailed rock magnetic parameters, such as thermomagnetic and high-field hysteresis data, indicate that pseudo-single domain magnetite in a narrow range of grain-size and concentration is the main contributor to the remanent magnetization. the uniform magnetic mineralogy meets the commonly accepted criteria for establishing relative paleointensity records. the relative paleointensity (rpi) curves were constructed by normalizing the natural remanent magnetization (nrm) with isothermal remanent magnetization (irm), both in the 20-60 mt demagnetization state. dating constraints have been provided by radiocarbon ages in the upper 400 cm of both cores. furthermore, we have correlated our paleointensity records with napis-75, s.atlantic-1089, sint-200 and nopapis-250 to determine the chronological rpi framework for the south china sea (scs-pis). although some temporal offsets of paleointensity features between the different records have been recognized, their similar shape suggests that relative paleointensity on the 10(3)-10(4) year scale is globally coherent and can provide an age framework for sediments independent of delta o-18 ages.
英文摘要relative paleointensity records from the northern south china sea, northwest pacific ocean were studied in two gravity piston cores. continuous mineral magnetic and paleomagnetic measurements were made using discrete sediment samples. detailed rock magnetic parameters, such as thermomagnetic and high-field hysteresis data, indicate that pseudo-single domain magnetite in a narrow range of grain-size and concentration is the main contributor to the remanent magnetization. the uniform magnetic mineralogy meets the commonly accepted criteria for establishing relative paleointensity records. the relative paleointensity (rpi) curves were constructed by normalizing the natural remanent magnetization (nrm) with isothermal remanent magnetization (irm), both in the 20-60 mt demagnetization state. dating constraints have been provided by radiocarbon ages in the upper 400 cm of both cores. furthermore, we have correlated our paleointensity records with napis-75, s.atlantic-1089, sint-200 and nopapis-250 to determine the chronological rpi framework for the south china sea (scs-pis). although some temporal offsets of paleointensity features between the different records have been recognized, their similar shape suggests that relative paleointensity on the 10(3)-10(4) year scale is globally coherent and can provide an age framework for sediments independent of delta(18)o ages. (c) 2009 elsevier b.v. all rights reserved.
WOS标题词science & technology ; physical sciences
类目[WOS]geochemistry & geophysics
研究领域[WOS]geochemistry & geophysics
关键词[WOS]inter-hemispheric correlation ; relative paleointensity ; north-atlantic ; late pleistocene ; loess plateau ; labrador-sea ; sulu sea ; 300 ka ; record ; intensity
收录类别SCI
资助信息national natural science foundation of china [40674034]; natural science foundation of guangdong province, china [06023110]
原文出处http://www.sciencedirect.com/science/journal/0012821x
语种英语
WOS记录号WOS:000268438900028
公开日期2010-09-16
源URL[http://ir.giec.ac.cn/handle/344007/3310]  
专题中国科学院广州能源研究所
作者单位1.Sun Yat Sen Univ, Dept Earth Sci, Guangzhou 510275, Guangdong, Peoples R China
2.Swiss Fed Inst Technol, Inst Geophys, CH-8092 Zurich, Switzerland
3.Chinese Acad Sci, Guangzhou Inst Energy Convers, Guangzhou 510640, Guangdong, Peoples R China
推荐引用方式
GB/T 7714
Yang Xiaoqiang,Friedrich Heller,Wu Nengyou,et al. Geomagnetic paleointensity dating of South China Sea sediments for the last 130 kyr[J]. earth and planetary science letters,2009,284(1-2):258-266.
APA Yang Xiaoqiang,Friedrich Heller,Wu Nengyou,Yang Jie,&Su Zhihua.(2009).Geomagnetic paleointensity dating of South China Sea sediments for the last 130 kyr.earth and planetary science letters,284(1-2),258-266.
MLA Yang Xiaoqiang,et al."Geomagnetic paleointensity dating of South China Sea sediments for the last 130 kyr".earth and planetary science letters 284.1-2(2009):258-266.

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来源:广州能源研究所

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