Mantle-driven plate convergence due to slab detachment
文献类型：期刊论文
| 作者 | Wu, Yangming1; Faccenda, Manuele5; Liao, Jie3,4; Fan, Jianke2; Guo, Feng6; Lai, Zhongping1 |
| 刊名 | COMMUNICATIONS EARTH & ENVIRONMENT
 |
| 出版日期 | 2025-06-22 |
| 卷号 | 6期号:1页码:12 |
| DOI | 10.1038/s43247-025-02484-x |
| 通讯作者 | Wu, Yangming(yangmingwu@stu.edu.cn) |
| 英文摘要 | The coupling between the lithosphere and mantle dynamics is important for Earth's tectonic movement and deformation. Plate driving forces changing from subduction to viscous flow drag can potentially explain the continuous plate convergence where subducting slabs are detached. However, tectonic expressions in different slab detachment scenarios are inconsistent and the role of mantle flow in plate convergence remains enigmatic. Through numerical modeling, we demonstrate that plate convergence can be caused by mantle flow induced by slab detachment and regulated by lithospheric mantle-ridge interaction. Spreading ridge-trench collision has minimal effects on the deformation of overriding plates, whereas continent-trench collision can lead to substantial tectonic uplift at suture zones. Mid-ocean ridges bounding incoming plates accelerate plate motion in ridge-trench collision scenarios and induce considerable tectonic uplift in continent-trench collision scenarios, as evidenced by the acceleration of the Farallon-Pacific ridge spreading and the rapid uplift of the Himalayas after slab detachment episodes. |
| WOS关键词 | SUBDUCTION ; PACIFIC ; FLOW ; DYNAMICS ; LITHOSPHERE ; TECTONICS ; COLLISION ; TRACTION ; HIMALAYA ; MOTIONS |
| 资助项目 | National Natural Science Foundation of China (National Science Foundation of China)[2023A1515012090] ; Guangdong Basic and Applied Basic Research Foundation[42104093] ; National Natural Science Foundation of China[NTF23029T] ; STU Scientific Research Foundation for Talents |
| WOS研究方向 | Environmental Sciences & Ecology ; Geology ; Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:001512419000001 |
| 出版者 | SPRINGERNATURE |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/202381]  |
| 专题 | 海洋研究所_海洋环流与波动重点实验室 |
| 通讯作者 | Wu, Yangming |
| 作者单位 | 1.Shantou Univ, Inst Marine Sci, Guangdong Prov Key Lab Marine Disaster Predict & P, Shantou, Peoples R China 2.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Observat & Forecasting, Key Lab Marine Geol & Environm, Qingdao, Peoples R China 3.Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai, Peoples R China 4.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangzhou, Peoples R China 5.Univ Padua, Dipartimento Geosci, Via Gradenigo 6, Padua, Italy 6.Yangtze Univ, Coll Resources & Environm, Wuhan, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wu, Yangming,Faccenda, Manuele,Liao, Jie,et al. Mantle-driven plate convergence due to slab detachment[J]. COMMUNICATIONS EARTH & ENVIRONMENT,2025,6(1):12. |
| APA | Wu, Yangming,Faccenda, Manuele,Liao, Jie,Fan, Jianke,Guo, Feng,&Lai, Zhongping.(2025).Mantle-driven plate convergence due to slab detachment.COMMUNICATIONS EARTH & ENVIRONMENT,6(1),12. |
| MLA | Wu, Yangming,et al."Mantle-driven plate convergence due to slab detachment".COMMUNICATIONS EARTH & ENVIRONMENT 6.1(2025):12. |
入库方式： OAI收割
来源：海洋研究所
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