中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
  4. 岩石圈演化国家重点实验室
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
ISSN号1367-9120
DOI10.1016/j.jseaes.2017.01.006
文献子类Article
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.
WOS关键词ULTRAHIGH-PRESSURE METAMORPHISM ; FLUID-ROCK INTERACTION ; OCEAN ISLAND BASALTS ; WESTERN TIANSHAN ; NW CHINA ; TECTONIC IMPLICATIONS ; SOUTHWESTERN TIANSHAN ; BEARING ECLOGITE ; CARBON-DIOXIDE ; MANTLE
WOS研究方向Geology
语种英语
WOS记录号WOS:000394484600026
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China(41572047 ; Excellent Young Project of Institute of Oceanology, Chinese Academy of Sciences(Y52221101Q) ; Special Research Program of the State Oceanic Administration of China(GASI-GEOGE-02) ; 9101400 ; 41130314) ; National Natural Science Foundation of China(41572047 ; Excellent Young Project of Institute of Oceanology, Chinese Academy of Sciences(Y52221101Q) ; Special Research Program of the State Oceanic Administration of China(GASI-GEOGE-02) ; 9101400 ; 41130314) ; National Natural Science Foundation of China(41572047 ; Excellent Young Project of Institute of Oceanology, Chinese Academy of Sciences(Y52221101Q) ; Special Research Program of the State Oceanic Administration of China(GASI-GEOGE-02) ; 9101400 ; 41130314) ; National Natural Science Foundation of China(41572047 ; Excellent Young Project of Institute of Oceanology, Chinese Academy of Sciences(Y52221101Q) ; Special Research Program of the State Oceanic Administration of China(GASI-GEOGE-02) ; 9101400 ; 41130314)
源URL[http://ir.iggcas.ac.cn/handle/132A11/53019]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Xiao, Yuanyuan
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：地质与地球物理研究所

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。