中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
High-Fidelity Archeointensity Results for the Late Neolithic Period From Central China

文献类型:期刊论文

作者Cai, Shuhui4; Tauxe, Lisa5; Wang, Weilin6; Deng, Chenglong1,4; Pan, Yongxin1,2; Yang, Liping3; Qin, Huafeng4
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2020-05-28
卷号47期号:10页码:11
关键词Archeointensity late Neolithic age central China archeomagnetic jerk Chinese archeointensity reference curve
ISSN号0094-8276
DOI10.1029/2020GL087625
英文摘要Archeomagnetism focuses on exploring high-resolution variations of the geomagnetic field over hundreds to thousands of years. In this study, we carried out a comprehensive study of chronology, absolute and relative paleointensity on a late Neolithic site in central China. Ages of the samples are constrained to be similar to 3,500-3,000 BCE, a period when available paleointensity data are sparse. We present a total of 64 high-fidelity absolute paleointensities, demonstrating the field varied quickly from similar to 55 to similar to 90 ZAm(2) between similar to 3,500-3,000 BCE. Our results record a new archeomagnetic jerk around 3,300 BCE, which is probably non-dipolar origin. The new results provide robust constraints on global geomagnetic models. We calculated a revised Chinese archeointensity reference curve for future application. The variations of absolute and relative paleointensity versus depth show good consistency, reinforcing the reliability of our results. This new attempt of combining absolute and relative paleointenstiy provides a useful tool for future archeomagnetic research. Plain Language Summary The geomagnetic field is generated in the Earth's liquid outer core; its behavior can provide us information on the Earth's interior and help us understand processes deep in the planet we live on. The magnetic field surrounds the Earth and acts like an umbrella protecting the planet from strong solar winds, and thus the geomagnetic behavior can affect life on the Earth. Understanding the evolution of the geomagnetic field allows us to learn about the Earth in the past and can help us predict what will happen in the future. The geomagnetic field includes both dipolar and non-dipolar components, with the former related to global and the latter to regional features. Studying regional geomagnetic variations from different areas is essential for outlining regional features and global distributions of the field. In this study, we carried out archeomagnetic research on a late Neolithic archeological site in central China. The high-fidelity results fill a gap of the present data set in both space and time, and thus refine both the regional and global geomagnetic models significantly. The newly released Chinese archeointensity reference curve in this study can be used for regional geomagnetic comparison as well as for archeological dating in this region.
WOS关键词GEOMAGNETIC-FIELD ; SECULAR VARIATION ; WESTERN-EUROPE ; RELATIVE PALEOINTENSITY ; INTENSITY VARIATIONS ; BC ; CALIBRATION ; CURVES
资助项目NSFC[41974077] ; NSFC[41621004] ; NSFC[41888101] ; NSF[EAR1520674] ; NSF[EAR1547263] ; CAS Pioneer Hundred Talents Program
WOS研究方向Geology
语种英语
WOS记录号WOS:000560371700038
出版者AMER GEOPHYSICAL UNION
资助机构NSFC ; NSFC ; NSFC ; NSFC ; NSF ; NSF ; NSF ; NSF ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; NSFC ; NSFC ; NSFC ; NSFC ; NSF ; NSF ; NSF ; NSF ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; NSFC ; NSFC ; NSFC ; NSFC ; NSF ; NSF ; NSF ; NSF ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; NSFC ; NSFC ; NSFC ; NSFC ; NSF ; NSF ; NSF ; NSF ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program ; CAS Pioneer Hundred Talents Program
源URL[http://ir.iggcas.ac.cn/handle/132A11/97639]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者Cai, Shuhui
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China
3.Shaanxi Prov Inst Archeol, Xian, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
5.Univ Calif San Diego, Scripps Inst Oceanog, San Diego, CA 92103 USA
6.Shanxi Univ, Coll Hist & Culture, Taiyuan, Peoples R China
推荐引用方式
GB/T 7714
Cai, Shuhui,Tauxe, Lisa,Wang, Weilin,et al. High-Fidelity Archeointensity Results for the Late Neolithic Period From Central China[J]. GEOPHYSICAL RESEARCH LETTERS,2020,47(10):11.
APA Cai, Shuhui.,Tauxe, Lisa.,Wang, Weilin.,Deng, Chenglong.,Pan, Yongxin.,...&Qin, Huafeng.(2020).High-Fidelity Archeointensity Results for the Late Neolithic Period From Central China.GEOPHYSICAL RESEARCH LETTERS,47(10),11.
MLA Cai, Shuhui,et al."High-Fidelity Archeointensity Results for the Late Neolithic Period From Central China".GEOPHYSICAL RESEARCH LETTERS 47.10(2020):11.

入库方式: OAI收割

来源:地质与地球物理研究所

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