Knowledge Management System Of Institute of Oceanology, Chinese Academy of Sciences
Modern-style arc magmatism since ca. 2.2 billion years ago revealed by Nb/ Ta-Dy/Yb systematics in igneous rocks | |
Liu, He1,2,3,5; Wang, Yiran3,4; Deng, Jianghong1,3,5; Zhang, Yu3,4; Chen, Qian3,4; Liao, Renqiang3; Sun, Wei-dong3,4,5 | |
2023-11-05 | |
发表期刊 | CHEMICAL GEOLOGY |
ISSN | 0009-2541 |
卷号 | 638页码:7 |
通讯作者 | Liu, He(liuhe@qdio.ac.cn) ; Deng, Jianghong(jhdeng0507@163.com) |
摘要 | The subduction of oceanic lithosphere is a significant mechanism in plate tectonics, which regulates volcanic activity along convergent plate boundaries on the modern Earth. However, while there is evidence for at least episodic, hot subduction in the Archaean, modern-style subduction might have not occurred on the early Earth under a different tectonic regime, potentially due to the high mantle temperature. It remains uncertain when modern-style subduction and its corresponding arc magmatism started operating on a global scale. Here we show that the modern arc intermediate-felsic rocks exhibit a distinct Nb/Ta-Dy/Yb correlation compared to their Archean counterparts due to the contrasting petrogenesis. Our statistical analysis of a worldwide igneous rock database, spanning geological history, indicates the widespread occurrence of intermediate-felsic rocks with modern arc signatures since ca. 2.2 Ga, which coincides with the onset of the supercontinent cycle. Continuous subduction of the cold oceanic lithosphere not only gave rise to arc magmatism along active margins but also accelerated the cooling rate of the mantle, which largely terminated the widespread formations of intermediate-felsic rocks derived from crustal delamination and slab melting. |
关键词 | Modern arc magmatism Archean igneous rocks Plate tectonics Continuous subduction Mantle cooling |
DOI | 10.1016/j.chemgeo.2023.121710 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | National Natural Science Foundation of China ; Taishan Scholar Program ; Laoshan Laboratory[tsqn202103126] ; [LSKJ202204100] ; [42073011] |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:001080104900001 |
出版者 | ELSEVIER |
WOS关键词 | EARLY CONTINENTAL-CRUST ; PLATE-TECTONICS ; PARTITION-COEFFICIENTS ; ARCHEAN CRUST ; VOLCANIC ARC ; GROWTH ; EVOLUTION ; EARTH ; GEOCHEMISTRY ; SUPERCONTINENT |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/181647 |
专题 | 深海极端环境与生命过程研究中心 |
通讯作者 | Liu, He; Deng, Jianghong |
作者单位 | 1.Chinese Acad Sci, Ctr Ocean Mega Sci, Haijun Rd, Qingdao 266400, Peoples R China 2.Univ Chinese Acad Sci, Sch Marine Sci, Haijun Rd, Qingdao 266400, Peoples R China 3.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, 7 Nanhai Rd, Qingdao 266071, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100094, Peoples R China 5.Laoshan Lab, Qingdao 266237, Peoples R China |
第一作者单位 | 深海极端环境与生命过程研究中心 |
通讯作者单位 | 深海极端环境与生命过程研究中心 |
推荐引用方式 GB/T 7714 | Liu, He,Wang, Yiran,Deng, Jianghong,et al. Modern-style arc magmatism since ca. 2.2 billion years ago revealed by Nb/ Ta-Dy/Yb systematics in igneous rocks[J]. CHEMICAL GEOLOGY,2023,638:7. |
APA | Liu, He.,Wang, Yiran.,Deng, Jianghong.,Zhang, Yu.,Chen, Qian.,...&Sun, Wei-dong.(2023).Modern-style arc magmatism since ca. 2.2 billion years ago revealed by Nb/ Ta-Dy/Yb systematics in igneous rocks.CHEMICAL GEOLOGY,638,7. |
MLA | Liu, He,et al."Modern-style arc magmatism since ca. 2.2 billion years ago revealed by Nb/ Ta-Dy/Yb systematics in igneous rocks".CHEMICAL GEOLOGY 638(2023):7. |
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