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Magnetic reversal frequency in the Lower Cambrian Niutitang Formation, Hunan Province, South China

文献类型：期刊论文

作者Duan, Zongqi1,2,5; Liu, Qingsong2,3; Ren, Shoumai4; Li, Lihui1,5; Deng, Xiaolong1,5; Liu, Jianxing6
刊名GEOPHYSICAL JOURNAL INTERNATIONAL
出版日期2018-08-01
卷号214期号:2页码:1301-1312
关键词Palaeomagnetism Rock and mineral magnetism Reversals: process timescale magnetostratigraphy
ISSN号0956-540X
DOI10.1093/gji/ggy199
英文摘要The reversal frequency of the palaeomagnetic field bears great information of evolution of Earth's deep interior. However, there are still debates on the frequency pattern during the older periods of the Phanerozoic. This study investigated the Niutitang Formation (Lower Cambrian) of the Ciye 1 Hole from South China. Rock magnetic results indicate that the dominant magnetic carrier is magnetite. Characteristic remanence magnetizations have been successfully isolated for the weakly magnetized shale rocks through stepwise alternated field demagnetization using the 2G Enterprises Rapid System Magnetometer with a low-noise thin-walled quartz-glass sample holder. Constrained by radiometric ages, our palaeomagnetic results indicated frequent polarity reversals during the period of similar to 524-514 Ma, which backs up the speculation about the episode of the Ediacaran-Cambrian (similar to 550-500 Ma) with a character of reversal hyperactivity.
WOS关键词ISOTHERMAL REMANENT MAGNETIZATION ; KULUMBE RIVER SECTION ; PGE-AU MINERALIZATION ; POLARITY TIME-SCALE ; YANGTZE PLATFORM ; BLACK SHALES ; NORTHWESTERN SIBERIA ; ACQUISITION CURVES ; YUNNAN PROVINCE ; SHELLY FOSSILS
资助项目Chinese Academy of Sciences[XDB 10030101] ; National Key Research and Development Program of China[2016YFA0601903] ; National Science Foundation of China[41430962] ; National Science Foundation of China[41506075] ; Chinese Continental Shelf Deep Drilling Program[GZH201100202] ; China Postdoctoral Science Foundation[2014M561047]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000448238600034
出版者OXFORD UNIV PRESS
资助机构Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Science Foundation of China ; National Science Foundation of China ; Chinese Continental Shelf Deep Drilling Program ; Chinese Continental Shelf Deep Drilling Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Science Foundation of China ; National Science Foundation of China ; Chinese Continental Shelf Deep Drilling Program ; Chinese Continental Shelf Deep Drilling Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Science Foundation of China ; National Science Foundation of China ; Chinese Continental Shelf Deep Drilling Program ; Chinese Continental Shelf Deep Drilling Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Science Foundation of China ; National Science Foundation of China ; Chinese Continental Shelf Deep Drilling Program ; Chinese Continental Shelf Deep Drilling Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation
源URL[http://ir.iggcas.ac.cn/handle/132A11/89126]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Liu, Qingsong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Qingdao Natl Oceanog Lab Sci & Technol, Lab Marine Geol, Qingdao 266237, Peoples R China
3.Southern Univ Sci & Technol, Dept Marine Sci & Engn, Shenzhen 518055, Peoples R China
4.China Geol Survey, Beijing 100037, Peoples R China
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
6.SOA, Inst Oceanog 1, Qingdao 266061, Peoples R China
推荐引用方式
GB/T 7714		 Duan, Zongqi,Liu, Qingsong,Ren, Shoumai,et al. Magnetic reversal frequency in the Lower Cambrian Niutitang Formation, Hunan Province, South China[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2018,214(2):1301-1312.
APA Duan, Zongqi,Liu, Qingsong,Ren, Shoumai,Li, Lihui,Deng, Xiaolong,&Liu, Jianxing.(2018).Magnetic reversal frequency in the Lower Cambrian Niutitang Formation, Hunan Province, South China.GEOPHYSICAL JOURNAL INTERNATIONAL,214(2),1301-1312.
MLA Duan, Zongqi,et al."Magnetic reversal frequency in the Lower Cambrian Niutitang Formation, Hunan Province, South China".GEOPHYSICAL JOURNAL INTERNATIONAL 214.2(2018):1301-1312.

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来源：地质与地球物理研究所

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