Paleomagnetic Recording Efficiency of Sedimentary Magnetic Mineral Inclusions: Implications for Relative Paleointensity Determinations
文献类型：期刊论文
| 作者 | Hong, Hoabin1; Chang, Liao1,2; Hayashida, Akira3; Roberts, Andrew P.4; Heslop, David4; Paterson, Greig A.5,6; Kodama, Kazuto7; Tauxe, Lisa8 |
| 刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
 |
| 出版日期 | 2019-07-01 |
| 卷号 | 124期号:7页码:6267-6279 |
| 关键词 | magnetic mineral inclusions relative paleointensity detrital remanent magnetization |
| ISSN号 | 2169-9313 |
| DOI | 10.1029/2018JB016859 |
| 英文摘要 | Sedimentary relative paleointensity (RPI) records are often carried by complex magnetic mineral mixtures, including detrital and biogenic magnetic minerals. Recent studies have demonstrated that magnetic inclusions within larger detrital silicate particles can make significant contributions to sedimentary paleomagnetic records. However, little is known about the role such inclusions play in sedimentary paleomagnetic signal recording. We analyzed paleomagnetic and mineral magnetic data for marine sediment core MD01-2421 from the North Pacific Ocean, offshore of central Japan, to assess how magnetic inclusions and other detrital magnetic minerals record sedimentary paleomagnetic signals. Stratigraphic intervals in which abundant magnetic inclusions dominate the magnetic signal are compared with other intervals to assess quantitatively their contribution to sedimentary RPI signals. The normalized remanence record from core MD01-2421 does not correlate clearly with global RPI stacks, which we attribute to a demonstrated lower paleomagnetic recording efficiency of magnetic inclusions compared to other detrital magnetic minerals. We also carried out the first laboratory redeposition experiments under controlled Earth-like magnetic fields for particles with magnetic inclusions using material from core MD01-2421. Our results confirm that such particles can be aligned by ambient magnetic fields but with a lower magnetic recording efficiency compared to other detrital magnetic minerals, which is consistent with normalized remanence data from core MD01-2421. Our demonstration of the role of sedimentary magnetic inclusions should have wide applicability for understanding sedimentary paleomagnetic recording. |
| WOS关键词 | DEPOSITIONAL REMANENT MAGNETIZATION ; ACQUISITION EFFICIENCY ; EXSOLVED MAGNETITE ; MARINE-SEDIMENTS ; INTENSITY ; FIELD ; FLOCCULATION ; REACTIVITY ; ANISOTROPY ; SALINITY |
| 资助项目 | National Natural Science Foundation of China[41574060] ; National Natural Science Foundation of China[41574063] ; National Natural Science Foundation of China[41722402] ; Australian Research Council[DP120103952] ; Australian Research Council[DP160100805] ; NERC[NE/P017266/1] ; NSF[EAR1547263] ; Japan Society for the Promotion of Science |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000481819500004 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; NERC ; NERC ; NSF ; NSF ; Japan Society for the Promotion of Science ; Japan Society for the Promotion of Science ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; NERC ; NERC ; NSF ; NSF ; Japan Society for the Promotion of Science ; Japan Society for the Promotion of Science ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; NERC ; NERC ; NSF ; NSF ; Japan Society for the Promotion of Science ; Japan Society for the Promotion of Science ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Australian Research Council ; Australian Research Council ; NERC ; NERC ; NSF ; NSF ; Japan Society for the Promotion of Science ; Japan Society for the Promotion of Science |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/93362]  |
| 专题 | 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 | Chang, Liao |
| 作者单位 | 1.Peking Univ, Sch Earth & Space Sci, Lab Orogen Belts & Crustal Evolut, Beijing, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Shandong, Peoples R China 3.Doshisha Univ, Dept Environm Syst Sci, Kyoto, Japan 4.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia 5.Univ Liverpool, Dept Earth Ocean & Ecol Sci, Liverpool, Merseyside, England 6.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China 7.Doshisha Univ, Res Ctr Knowledge Sci Cultural Heritage, Kyoto, Japan 8.Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA |
| 推荐引用方式 GB/T 7714 | Hong, Hoabin,Chang, Liao,Hayashida, Akira,et al. Paleomagnetic Recording Efficiency of Sedimentary Magnetic Mineral Inclusions: Implications for Relative Paleointensity Determinations[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2019,124(7):6267-6279. |
| APA | Hong, Hoabin.,Chang, Liao.,Hayashida, Akira.,Roberts, Andrew P..,Heslop, David.,...&Tauxe, Lisa.(2019).Paleomagnetic Recording Efficiency of Sedimentary Magnetic Mineral Inclusions: Implications for Relative Paleointensity Determinations.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,124(7),6267-6279. |
| MLA | Hong, Hoabin,et al."Paleomagnetic Recording Efficiency of Sedimentary Magnetic Mineral Inclusions: Implications for Relative Paleointensity Determinations".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 124.7(2019):6267-6279. |
入库方式： OAI收割
来源：地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。