| Continental collision zones are primary sites for net continental crust growth - A testable hypothesis | |
| Niu, Yaoling1,2,3,4; Zhao, Zhidan3,4; Zhu, Di-Cheng3,4; Mo, Xuanxue3,4; Niu, YL | |
| 2013-12-01 | |
| 发表期刊 | EARTH-SCIENCE REVIEWS
 |
| ISSN | 0012-8252 |
| 卷号 | 127页码:96-110 |
| 文章类型 | Article |
| 摘要 | The significance of the continental crust (CC) on which we live is self-evident. However, our knowledge remains limited on its origin, its way and rate of growth, and how it has acquired the "andesitic" composition from mantle derived magmas. Compared to rocks formed from mantle derived magmas in all geological environments, volcanic arc rocks associated with seafloor subduction share some common features with the CC; both are relatively depleted in "fluid-insoluble" elements (e.g., Nb, Ta and Ti), but enriched in "fluid-soluble" elements (e.g., U, K and Pb). These chemical characteristics are referred to as the "arc-like signature", and point to a possible link between subduction-zone magmatism and CC formation, thus leading to the "island arc" model widely accepted for the origin of the CC over the past 45 years. However, this "island arc" model has many difficulties: e.g., (1) the bulk arc crust (AC) is basaltic whereas the bulk CC is andesitic; (2) the AC has variably large Sr excess whereas the CC is weakly Sr deficient; and (3) AC production is mass-balanced by subduction erosion and sediment recycling, thus contributing no net mass to the CC growth, at least in the Phanerozoic. Our recent and ongoing studies on granitoid rocks (both volcanic and intrusive) formed in response to the India Asia continental collision (similar to 55 +/- 10 Ma) show remarkable compositional similarity to the bulk CC with the typical "arc-like signature". Also, these syncollisional granitoid rocks exhibit strong mantle isotopic signatures, meaning that they were recently derived from a mantle source. The petrology and geochemistry of these syncollisional granitoid rocks are most consistent with an origin via partial melting of the upper ocean crust (i.e., last fragments of underthrusting ocean crust upon collision) under amphibolite facies conditions, adding net mantle-derived materials to form juvenile CC mass. This leads to the logical and testable hypothesis that continental collision produces and preserves the juvenile crust, and hence maintains net CC growth.; The significance of the continental crust (CC) on which we live is self-evident. However, our knowledge remains limited on its origin, its way and rate of growth, and how it has acquired the "andesitic" composition from mantle derived magmas. Compared to rocks formed from mantle derived magmas in all geological environments, volcanic arc rocks associated with seafloor subduction share some common features with the CC; both are relatively depleted in "fluid-insoluble" elements (e.g., Nb, Ta and Ti), but enriched in "fluid-soluble" elements (e.g., U, K and Pb). These chemical characteristics are referred to as the "arc-like signature", and point to a possible link between subduction-zone magmatism and CC formation, thus leading to the "island arc" model widely accepted for the origin of the CC over the past 45 years. However, this "island arc" model has many difficulties: e.g., (1) the bulk arc crust (AC) is basaltic whereas the bulk CC is andesitic; (2) the AC has variably large Sr excess whereas the CC is weakly Sr deficient; and (3) AC production is mass-balanced by subduction erosion and sediment recycling, thus contributing no net mass to the CC growth, at least in the Phanerozoic. Our recent and ongoing studies on granitoid rocks (both volcanic and intrusive) formed in response to the India Asia continental collision (similar to 55 +/- 10 Ma) show remarkable compositional similarity to the bulk CC with the typical "arc-like signature". Also, these syncollisional granitoid rocks exhibit strong mantle isotopic signatures, meaning that they were recently derived from a mantle source. The petrology and geochemistry of these syncollisional granitoid rocks are most consistent with an origin via partial melting of the upper ocean crust (i.e., last fragments of underthrusting ocean crust upon collision) under amphibolite facies conditions, adding net mantle-derived materials to form juvenile CC mass. This leads to the logical and testable hypothesis that continental collision produces and preserves the juvenile crust, and hence maintains net CC growth. Importantly, the history of the Greater Tibetan Plateau from the Early Paleozoic to present manifests the history of "super" continent amalgamation through a series of continental collision events with production and preservation of abundant syncollisional granitoids. Plate tectonics in terms of seafloor spreading and subduction is a continuous process on a global scale since its inception (in the early Archean?), whereas continental collision on regional scales and super-continental formation on a global scale are episodic (vs. continuous). Hence, continental collision with juvenile crust formation/preservation and super-continent amalgamation explains the episodic growth of the CC. We are continuing testing and refining this hypothesis by detailed petrological, geochemical and geochronological studies of syncollisional granitoids along older collision zones in central-west China, especially on the northern Tibetan Plateau in a global context. (C) 2013 Published by Elsevier B.V. |
| 关键词 | Continental Collision Ocean Crust Melting Syncollisional Granitoid Magmatism Juvenile Crust Formation Episodic Continental Crust Growth Super-continental Amalgamation Daly Gap |
| 学科领域 | Geology |
| DOI | 10.1016/j.earscirev2013.09.004 |
| URL | 查看原文 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS研究方向 | Geology |
| WOS类目 | Geosciences, Multidisciplinary |
| WOS记录号 | WOS:000328871100005 |
| WOS关键词 | BASALT-TRACHYTE ASSOCIATION ; SOUTHERN TIBET ; ARC MAGMAS ; SUBDUCTION ZONES ; MANTLE DIFFERENTIATION ; GEOCHEMICAL EVOLUTION ; MELTING EXPERIMENTS ; GANGDESE BATHOLITH ; CHEMICAL-STRUCTURE ; ISOTOPIC EVIDENCE |
| WOS标题词 | Science & Technology ; Physical Sciences |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/16296 |
| 专题 | 海洋地质与环境重点实验室 |
| 通讯作者 | Niu, YL |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England 3.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China 4.China Univ Geosci, Sch Earth Sci & Mineral Resources, Beijing 100083, Peoples R China |
| 第一作者单位 | 中国科学院海洋研究所 |
| 推荐引用方式 GB/T 7714 | Niu, Yaoling,Zhao, Zhidan,Zhu, Di-Cheng,et al. Continental collision zones are primary sites for net continental crust growth - A testable hypothesis[J]. EARTH-SCIENCE REVIEWS,2013,127:96-110. |
| APA | Niu, Yaoling,Zhao, Zhidan,Zhu, Di-Cheng,Mo, Xuanxue,&Niu, YL.(2013).Continental collision zones are primary sites for net continental crust growth - A testable hypothesis.EARTH-SCIENCE REVIEWS,127,96-110. |
| MLA | Niu, Yaoling,et al."Continental collision zones are primary sites for net continental crust growth - A testable hypothesis".EARTH-SCIENCE REVIEWS 127(2013):96-110. |
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