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Intraplate continental basalts over the past billion years track cooling of the mantle and the onset of modern plate tectonics | |
Chen, Qian1,2,3; Liu, He1,2,3; Johnson, Tim4; Hartnady, Michael4; Kirkland, Christopher L.4; Lu, Yongjun5,6,7; Sun, Wei-dong1,2,3 | |
2022-11-01 | |
发表期刊 | EARTH AND PLANETARY SCIENCE LETTERS |
ISSN | 0012-821X |
卷号 | 597页码:6 |
通讯作者 | Liu, He([email protected]) |
摘要 | The temperature of the convecting mantle exerts a first-order control on the rheology, composition, and consequently, tectonic behavior of Earth's lithosphere. Although the mantle has likely been cooling since the Archaean eon, how mantle temperature has evolved thereafter is poorly understood. Here, we apply a statistical analysis to secular changes in the alkali index [AI = whole-rock (Na2O + K2O)2/(SiO2 - 35) as weight%] of global sodic intracontinental basalts, a proxy for the degree of mantle melting, to constrain the evolution of mantle potential temperature (TP) over the past billion years. Our results show that, during the early Neoproterozoic, TP remained relatively constant until the beginning of the Cryogenian (720 Ma), when mantle temperature dropped rapidly over the following similar to 180 Ma. This remarkable episode of cooling records the onset of modern-style plate tectonics characterized by continuous deep subduction of the oceanic lithosphere, consistent with the widespread appearance of blueschists in the metamorphic rock record.(c) 2022 Elsevier B.V. All rights reserved. |
关键词 | mantle cooling modern plate tectonics snowball Earth intracontinental basalts |
DOI | 10.1016/j.epsl.2022.117804 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan[GPMR201903]; National Natural Science Foundation of China[42073011] |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000869031400003 |
出版者 | ELSEVIER |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/180654 |
专题 | 深海极端环境与生命过程研究中心 |
通讯作者 | Liu, He |
作者单位 | 1.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, 7 Nanhai Rd, Qingdao 266071, Peoples R China 2.Deep Sea Multidisciplinary Res Ctr, Qingdao Pilot Natl Lab Marine Sci & Technol, Qingdao 266237, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100094, Peoples R China 4.Curtin Univ, Sch Earth & Planetary Sci, GPO Box U1987, Perth, WA 6845, Australia 5.Geol Survey Western Australia, Dept Mines Ind Regulat & Safety, 100 Plain St, East Perth, WA 6004, Australia 6.Univ Western Australia, Ctr Excellence Core Crust Fluid Syst CCFS, Ctr Explorat Targeting, Perth, WA 6009, Australia 7.Univ Western Australia, Ctr Excellence Core Crust Fluid Syst CCFS, Australian Res Council, Perth, WA 6009, Australia |
第一作者单位 | 中国科学院海洋研究所 |
通讯作者单位 | 中国科学院海洋研究所 |
推荐引用方式 GB/T 7714 | Chen, Qian,Liu, He,Johnson, Tim,et al. Intraplate continental basalts over the past billion years track cooling of the mantle and the onset of modern plate tectonics[J]. EARTH AND PLANETARY SCIENCE LETTERS,2022,597:6. |
APA | Chen, Qian.,Liu, He.,Johnson, Tim.,Hartnady, Michael.,Kirkland, Christopher L..,...&Sun, Wei-dong.(2022).Intraplate continental basalts over the past billion years track cooling of the mantle and the onset of modern plate tectonics.EARTH AND PLANETARY SCIENCE LETTERS,597,6. |
MLA | Chen, Qian,et al."Intraplate continental basalts over the past billion years track cooling of the mantle and the onset of modern plate tectonics".EARTH AND PLANETARY SCIENCE LETTERS 597(2022):6. |
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文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
1-s2.0-S0012821X2200(520KB) | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 |
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