Knowledge Management System Of Institute of Oceanology, Chinese Academy of Sciences
Mantle plume - mid ocean ridge interactions revealed from hotspot melt production rate along the Walvis Ridge-Rio Grande Rise | |
Bai, Yongliang1; Cheng, Kunpeng1; Dong, Dongdong2; Song, Xinjian1; Li, Sanzhong3,4; Wu, Shiguo5; Wang, Zhenjie1 | |
2024-12-15 | |
发表期刊 | EARTH AND PLANETARY SCIENCE LETTERS
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ISSN | 0012-821X |
卷号 | 648页码:12 |
通讯作者 | Bai, Yongliang([email protected]) |
摘要 | Mantle plume and mid-ocean ridge (MOR) interactions have a profound impact on geological processes, such as large igneous province eruptions, mid-ocean ridge jumps and plume flow towards the MOR. The Walvis Ridge and Rio Grande Rise provide an excellent opportunity to study these interactions, as they have a record of duringand post-interaction stages. We have estimated the hotspot melt production rate along the Walvis Ridge - Rio Grande Rise. Our findings are as follows: (1) The hotspot melt production rate during plume-MOR interaction is seven times higher than that after the interaction, primarily because a thinner lithospheric coverage over the plume allows for greater decompression melting and facilitates the ascent of melt through the lithospheric mantle to accrete to the crust. (2) The waning of the Tristan-Gough plume is indicated by a decreasing melt production rate and an increase in inter-volcano spacing. (3) The linear ridges on the western side of the Guyot Province likely result from mantle plume flow beneath the lithosphere from the hotspot to the Mid-Atlantic Ridge. (4) Fracture zones enhance hotspot melt production rates. |
关键词 | Plume-ridge interaction Hotspot melt production rate Walvis Ridge Plume waning MOR-ward plume flow |
DOI | 10.1016/j.epsl.2024.119102 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | National Natural Science Foundation of China[42176068]; National Natural Science Foundation of China[42476063]; National Natural Science Foundation of China[92058213]; National Natural Science Foundation of China[42376081]; National Natural Science Foundation of China[42121005]; Nat-ural Science Foundation of Shandong, China[ZR2020MD065] |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:001354431800001 |
出版者 | ELSEVIER |
WOS关键词 | REGIONAL-RESIDUAL SEPARATION ; SOUTH ATLANTIC ; VOLCANISM ; LITHOSPHERE ; THICKNESS ; ORIGIN ; CRUST ; BATHYMETRY ; DYNAMICS ; DEPTH |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/199436 |
专题 | 深海极端环境与生命过程研究中心 |
通讯作者 | Bai, Yongliang |
作者单位 | 1.China Univ Petr, Coll Oceanog & Space Informat, Qingdao 266580, Peoples R China 2.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 3.Ocean Univ China, Key Lab Submarine Geosci & Prospecting Tech, Minist Educ, Qingdao 266100, Peoples R China 4.Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Peoples R China 5.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China |
推荐引用方式 GB/T 7714 | Bai, Yongliang,Cheng, Kunpeng,Dong, Dongdong,et al. Mantle plume - mid ocean ridge interactions revealed from hotspot melt production rate along the Walvis Ridge-Rio Grande Rise[J]. EARTH AND PLANETARY SCIENCE LETTERS,2024,648:12. |
APA | Bai, Yongliang.,Cheng, Kunpeng.,Dong, Dongdong.,Song, Xinjian.,Li, Sanzhong.,...&Wang, Zhenjie.(2024).Mantle plume - mid ocean ridge interactions revealed from hotspot melt production rate along the Walvis Ridge-Rio Grande Rise.EARTH AND PLANETARY SCIENCE LETTERS,648,12. |
MLA | Bai, Yongliang,et al."Mantle plume - mid ocean ridge interactions revealed from hotspot melt production rate along the Walvis Ridge-Rio Grande Rise".EARTH AND PLANETARY SCIENCE LETTERS 648(2024):12. |
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