IGGCAS OpenIR  > 岩石圈演化国家重点实验室
Barium content of Archaean continental crust reveals the onset of subduction was not global
Huang, Guangyu1; Mitchell, Ross N.1,2; Palin, Richard M.3; Spencer, Christopher J.4; Guo, Jinghui1,2
2022-11-02
Source PublicationNATURE COMMUNICATIONS
Volume13Issue:1Pages:8
AbstractEarth'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
DOI10.1038/s41467-022-34343-0
Funding OrganizationNational 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
WOS KeywordPLATE-TECTONICS ; AMPHIBOLITE ; EVOLUTION ; ZIRCON ; GROWTH ; MONAZITE ; BEHAVIOR ; GRANITE ; GENESIS ; APATITE
Language英语
Funding ProjectNational Natural Science Foundation of China[41890832] ; National Natural Science Foundation of China[42172217] ; National Natural Science Foundation of China[41902057]
Funding OrganizationNational 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
WOS Research AreaScience & Technology - Other Topics
WOS SubjectMultidisciplinary Sciences
WOS IDWOS:000879356300011
PublisherNATURE PORTFOLIO
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/107703
Collection岩石圈演化国家重点实验室
Corresponding AuthorHuang, Guangyu; Mitchell, Ross N.
Affiliation1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
3.Univ Oxford, Dept Earth Sci, Oxford OX1 3AN, England
4.Queens Univ, Dept Geol Sci & Geol Engn, Kingston, ON K7L 3N6, Canada
First Author AffilicationState Key Laboratory of Lithospheric Evolution
Corresponding Author AffilicationState Key Laboratory of Lithospheric Evolution
Recommended Citation
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.
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