Plume-ridge interaction induced migration of the Hawaiian-Emperor seamounts
文献类型：期刊论文
| 作者 | Sun, Weidong1,2,3 ; Langmuir, Charles H.4; Ribe, Neil M.5; Zhang, Lipeng1,2; Sun, Saijun1,2; Li, He1,2; Li, Congying1,2; Fan, Weiming3,6; Tackley, Paul J.7; Sanan, Patrick7
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| 刊名 | SCIENCE BULLETIN
 |
| 出版日期 | 2021-08-30 |
| 卷号 | 66期号:16页码:1691-1697 |
| 关键词 | Pacific plate Emperor-Hawaii chain Plume-ridge interaction Geochemistry Numerical modeling |
| ISSN号 | 2095-9273 |
| DOI | 10.1016/j.scib.2021.04.028 |
| 通讯作者 | Sun, Weidong(weidongsun@qdio.ac.cn) ; Langmuir, Charles H.(langmuir@eps.harvard.edu) |
| 英文摘要 | The history of the Hawaiian hotspot is of enduring interest in studies of plate motion and mantle flow, and has been investigated by many researchers using the detailed history of the Hawaiian-Emperor Seamount chain. One of the unexplained aspects of this history is the apparent offset of several Emperor seamounts from the Hawaii plume track. Here we show that the volcanic migration rates of the Emperor seamounts based on existing data are inconsistent with the drifting rate of the Pacific plate, and indicate northward and then southward "absolute movements" of the seamounts. Numerical modeling suggests that attraction and capture of the upper part of the plume by a moving spreading ridge led to variation in the location of the plume's magmatic output at the surface. Flow of the plume material towards the ridge led to apparent southward movement of Meiji. Then, the upper part of the plume was carried northward until 65 Ma ago. After the ridge and the plume became sufficiently separated, magmatic output moved back to be centered over the plume stem. These changes are apparent in variations in the volume of seamounts along the plume track. Chemical and isotopic compositions of basalt from the Emperor Seamount chain changed from depleted (strong mid-ocean ridge affinity) in Meiji and Detroit to enriched (ocean island type), supporting declining influence from the ridge. Although its surface expression was modified by mantle flow and by plume-ridge interactions, the stem of the Hawaiian plume may have been essentially stationary during the Emperor period. (c) 2021 Science China Press. Published by Elsevier B.V. and Science China Press. All rights reserved. |
| 资助项目 | National Key Research & Development Program of China[2016YFC0600408] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18020000] ; Programme National de Planetologie (PNP) of the Institut des Sciences de l'Univers (INSU) of the French National Centre for Scientific Research (CNRS) ; French Space Centre (CNES)[BFC 221950] |
| WOS研究方向 | Science & Technology - Other Topics |
| 语种 | 英语 |
| WOS记录号 | WOS:000686908500016 |
| 出版者 | ELSEVIER |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/176284]  |
| 专题 | 海洋研究所_深海极端环境与生命过程研究中心 |
| 通讯作者 | Sun, Weidong; Langmuir, Charles H. |
| 作者单位 | 1.Chinese Acad Sci, Ctr Deep Sea Res, Ctr Ocean Mega Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Pilot Natl Lab Marine Sci & Technol Qingdao, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China 3.Univ Chinese Acad Sci, Sch Marine Sci, Beijing 100049, Peoples R China 4.Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA 5.Univ Paris Saclay, CNRS, Lab Fast, F-91405 Orsay, France 6.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 7.Swiss Fed Inst Technol, Dept Earth Sci, Inst Geophys, CH-8092 Zurich, Switzerland |
| 推荐引用方式 GB/T 7714 | Sun, Weidong,Langmuir, Charles H.,Ribe, Neil M.,et al. Plume-ridge interaction induced migration of the Hawaiian-Emperor seamounts[J]. SCIENCE BULLETIN,2021,66(16):1691-1697. |
| APA | Sun, Weidong.,Langmuir, Charles H..,Ribe, Neil M..,Zhang, Lipeng.,Sun, Saijun.,...&Sanan, Patrick.(2021).Plume-ridge interaction induced migration of the Hawaiian-Emperor seamounts.SCIENCE BULLETIN,66(16),1691-1697. |
| MLA | Sun, Weidong,et al."Plume-ridge interaction induced migration of the Hawaiian-Emperor seamounts".SCIENCE BULLETIN 66.16(2021):1691-1697. |
入库方式： OAI收割
来源：海洋研究所
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