Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China
文献类型:期刊论文
作者 | Hou, Xingao3; Yu, Zhiqiang3; Chen, Shefa3; Liu, Lei2,3; Xiao, Yilin1 |
刊名 | JOURNAL OF EARTH SCIENCE
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出版日期 | 2024-02-01 |
卷号 | 35期号:1页码:1-15 |
关键词 | UHP metamorphism eclogite marble element migration fluid actions geochemistry |
ISSN号 | 1674-487X |
DOI | 10.1007/s12583-022-1692 |
英文摘要 | In order to decipher element mobility in UHP meta-sedimentary rocks in the continental subduction zone, major and trace element compositions are investigated for a continuous profile from a representative UHP region in the Dabie Mountains. Among the lithologic contact zone, contents of K, Ca, LREE, and LILE exhibit varying degrees of downward trends in both marble and eclogite toward the contact zone, indicating that marble and their associated eclogite can release a large amount of K, Ca, and a small number of LILEs and LREEs. Titanite is the main Ti phase in both marble and eclogite. Titanite rims around rutile can occasionally be seen in eclogite. Contents of Ti and HFSE exhibit a well-coupled relation among marble and eclogite, indicating that substantial Ti and HFSEs were migrated from eclogite to marble, in accord with the capacity of a melt medium. Rutiles and titanites in marble exhibit a relatively limited variation in Nb/Ta ratios (12.9-16.2), similar to those of titanites in eclogite (14.2-16.7), which demonstrates that rutiles and titanites in marble were sourced from eclogite because of short-distance migrations of Ti and HFSEs. According to the P-T path and the temperature and pressure conditions of the peak metamorphism reported by previous studies, the eclogite associated with marble may not form supercritical fluids in the subduction zone because of the addition of carbonate minerals. |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:001162401600017 |
源URL | [http://ir.gig.ac.cn/handle/344008/77370] ![]() |
专题 | 中国科学院矿物学与成矿学重点实验室 |
通讯作者 | Liu, Lei |
作者单位 | 1.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China 3.Cent South Univ, Sch Geosci & Infophys, Key Lab Metallogen Predict Nonferrous Met & Geol, Minist Educ, Changsha 410083, Peoples R China |
推荐引用方式 GB/T 7714 | Hou, Xingao,Yu, Zhiqiang,Chen, Shefa,et al. Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China[J]. JOURNAL OF EARTH SCIENCE,2024,35(1):1-15. |
APA | Hou, Xingao,Yu, Zhiqiang,Chen, Shefa,Liu, Lei,&Xiao, Yilin.(2024).Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China.JOURNAL OF EARTH SCIENCE,35(1),1-15. |
MLA | Hou, Xingao,et al."Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China".JOURNAL OF EARTH SCIENCE 35.1(2024):1-15. |
入库方式: OAI收割
来源:广州地球化学研究所
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