Barium content of Archaean continental crust reveals the onset of subduction was not global
文献类型:期刊论文
作者 | Huang, Guangyu1; Mitchell, Ross N.1,4; Palin, Richard M.2; Spencer, Christopher J.3; Guo, Jinghui1,4 |
刊名 | NATURE COMMUNICATIONS |
出版日期 | 2022-11-02 |
卷号 | 13期号:1页码:8 |
DOI | 10.1038/s41467-022-34343-0 |
英文摘要 | Earth's earliest continental crust is dominated by tonalite-trondhjemite-granodiorite (TTG) suites, making these rocks key to unlocking the global geodynamic regime operating during the Archaean (4.0-2.5 billion years ago [Ga]). The tectonic setting of TTG magmatism is controversial, with hypotheses arguing both for and against subduction. Here we conduct petrological modeling over a range of pressure-temperature conditions relevant to the Archaean geothermal gradient. Using an average enriched Archaean basaltic source composition, we predict Ba concentrations in TTG suites, which is difficult to increase after magma generated in the source. The results indicate only low geothermal gradients corresponding to hot subduction zones produce Ba-rich TTG, thus Ba represents a proxy for the onset of subduction. We then identify statistically significant increases in the Ba contents of TTG suites worldwide as recording the diachronous onset of subduction from regional at 4 Ga to globally complete sometime after 2.7 Ga. Only subduction zone can produce Ba-rich TTG, representing a proxy for the onset of subduction. Statistical increases in Ba contents of Archaean TTGs reveal the diachronous onset of subduction from regional at 4 Ga to globally complete after 2.7 Ga |
WOS关键词 | PLATE-TECTONICS ; AMPHIBOLITE ; EVOLUTION ; ZIRCON ; GROWTH ; MONAZITE ; BEHAVIOR ; GRANITE ; GENESIS ; APATITE |
资助项目 | National Natural Science Foundation of China[41890832] ; National Natural Science Foundation of China[42172217] ; National Natural Science Foundation of China[41902057] |
WOS研究方向 | Science & Technology - Other Topics |
语种 | 英语 |
出版者 | NATURE PORTFOLIO |
WOS记录号 | WOS:000879356300011 |
资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/107703] |
专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
通讯作者 | Huang, Guangyu; Mitchell, Ross N. |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Univ Oxford, Dept Earth Sci, Oxford OX1 3AN, England 3.Queens Univ, Dept Geol Sci & Geol Engn, Kingston, ON K7L 3N6, Canada 4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Huang, Guangyu,Mitchell, Ross N.,Palin, Richard M.,et al. Barium content of Archaean continental crust reveals the onset of subduction was not global[J]. NATURE COMMUNICATIONS,2022,13(1):8. |
APA | Huang, Guangyu,Mitchell, Ross N.,Palin, Richard M.,Spencer, Christopher J.,&Guo, Jinghui.(2022).Barium content of Archaean continental crust reveals the onset of subduction was not global.NATURE COMMUNICATIONS,13(1),8. |
MLA | Huang, Guangyu,et al."Barium content of Archaean continental crust reveals the onset of subduction was not global".NATURE COMMUNICATIONS 13.1(2022):8. |
入库方式: OAI收割
来源:地质与地球物理研究所
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