Application of big data of rock geochemistry to plate tectonic evolution
文献类型：期刊论文
| 作者 | Liu, He1,2 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2025-12-01 |
| 卷号 | 41期号:12页码:4137-4148 |
| 关键词 | Plate tectonics Onset time Style change Big data Geochemistry |
| ISSN号 | 1000-0569 |
| DOI | 10.18654/1000-0569/2025.12.11 |
| 通讯作者 | Liu, He(liuhe@qdio.ac.en) |
| 英文摘要 | Plate tectonics drives the circulation of materials and heat between Earth's surface and deep interior, profoundly influencing the evolution of planetary habitability. Scientific debates on the timing of plate tectonics initiation and its evolutionary history have long polarized the Earth science community, with early 21" century scholars proposing contrasting extremes. Numerous studies once argued for an Archean to Paleoproterozoic onset of plate tectonics, with some even advocating a Hadean origin, while others persistently maintained a Neoproterozoic commencement. Recent years, however, a growing consensus has emerged, ie, most researchers now accept that modern-style plate tectonics emerged after the Neoproterozoic, while earlier tectonic regimes are recognized as distinct "early plate tectonics" or "proto-plate tectonics". Increasing evidence suggests that the localized and short-lived Archean subduction differed substantially from globally interconnected plate tectonic systems, potentially representing transitional phases between non-plate and plate-dominated geodynamics. This paper reviews the relevant arguments regarding the initiation time of plate tectonics, explains the origin of the contradictions, and describes the process of alleviation in recent debates. Meanwhile, the following aspects are also introduced in this paper, such as the progresses in using big data analysis of rock geochemistry to constrain the formation and evolution of plate tectonics, analyzing the era of the formation and style transitions of plate tectonics, and discussing the global impacts of the initiation of early and modern plate tectonics on magmatism, lithospheric structure, mantle temperature, and deep material cycling. |
| WOS关键词 | CONTINENTAL-CRUST ; ARCHEAN SUBDUCTION ; LITHOSPHERE ; GROWTH ; START ; EARTH ; GA ; SUPERCONTINENT ; CONSEQUENCES ; SPECULATIONS |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:001676360000011 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/204676]  |
| 专题 | 海洋研究所_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, Inst Oceanol, Key Lab Ocean Observat & Forecasting, Qingdao 266000, Peoples R China 2.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266000, Peoples R China |
| 推荐引用方式 GB/T 7714 | Liu, He. Application of big data of rock geochemistry to plate tectonic evolution[J]. ACTA PETROLOGICA SINICA,2025,41(12):4137-4148. |
| APA | Liu, He.(2025).Application of big data of rock geochemistry to plate tectonic evolution.ACTA PETROLOGICA SINICA,41(12),4137-4148. |
| MLA | Liu, He."Application of big data of rock geochemistry to plate tectonic evolution".ACTA PETROLOGICA SINICA 41.12(2025):4137-4148. |
入库方式： OAI收割
来源：海洋研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。