Effects of decarbonation on elemental behaviors during subduction-zone metamorphism: Evidence from a titanite-rich contact between eclogitefacies marble and omphacitite
文献类型：期刊论文
| 作者 | Xiao, Yuanyuan1,2,3; Niu, Yaoling1,2,4; Zhang, Hong-Fu5,6; Wang, Kuo-Lung3; Iizuka, Yoshiyuki3; Lin, Jinyan5; Tan, Yulong5; Xu, Yongjiang5 |
| 刊名 | JOURNAL OF ASIAN EARTH SCIENCES
 |
| 出版日期 | 2017-03-01 |
| 卷号 | 135页码:338-346 |
| 关键词 | Marine carbonate subduction Behaviors of chemical elements Subduction-zone metamorphism Subduction-zone magmatism Mantle isotopic heterogeneity |
| 英文摘要 | In this paper, we show the effects of subducted carbonates on geochemical processes during subduction-zone metamorphism (SZM) through the study of an eclogite-facies marble coexisting with metabasite from the ultrahigh pressure metamorphic belt of the Chinese Western Tianshan orogen. Between the marble and metabasite is a titanite-rich contact resulting from fluid-facilitated metamorphic reactions between the two lithologies, and recording elemental changes of geodynamic significance. Because this titanite-rich contact is dominated by titanite (an important host for high field strength elements, HFSEs) without white micas (an important host for large ion lithophile elements, LILEs), HFSEs are largely conserved in titanite whereas LILEs are moved away. This observation emphasizes the potential signifitance of subducting carbonate in retaining HFSEs in the slab through the formation and stabilization of titanite, contributing to the characteristic "arc signature" unique to subduction-zone magmatism (i.e., high LILEs, low HFSEs). The implicit assumption in this interpretation is that the observed lithological assemblage represents residues of subducting oceanic crust that has undergone major episodes of dehydration. Subducted carbonates also have significant implications for the origin of mantle isotopic heterogeneity as revealed from oceanic basalts. (C) 2017 Elsevier Ltd. All rights reserved. |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000394484600026 |
| 版本 | 出版稿 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/136768]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China 3.Acad Sinica, Inst Earth Sci, Taipei 11529, Taiwan 4.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England 5.Northwest Univ Xian, Dept Geol, Xian 710069, Peoples R China 6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xiao, Yuanyuan,Niu, Yaoling,Zhang, Hong-Fu,et al. Effects of decarbonation on elemental behaviors during subduction-zone metamorphism: Evidence from a titanite-rich contact between eclogitefacies marble and omphacitite[J]. JOURNAL OF ASIAN EARTH SCIENCES,2017,135:338-346. |
| APA | Xiao, Yuanyuan.,Niu, Yaoling.,Zhang, Hong-Fu.,Wang, Kuo-Lung.,Iizuka, Yoshiyuki.,...&Xu, Yongjiang.(2017).Effects of decarbonation on elemental behaviors during subduction-zone metamorphism: Evidence from a titanite-rich contact between eclogitefacies marble and omphacitite.JOURNAL OF ASIAN EARTH SCIENCES,135,338-346. |
| MLA | Xiao, Yuanyuan,et al."Effects of decarbonation on elemental behaviors during subduction-zone metamorphism: Evidence from a titanite-rich contact between eclogitefacies marble and omphacitite".JOURNAL OF ASIAN EARTH SCIENCES 135(2017):338-346. |
入库方式： OAI收割
来源：海洋研究所
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