中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Petrogenesis and tectonic setting of Late Devonian high-Mg andesites in the Beishan orogen, NW China

文献类型:期刊论文

作者Wang, Guo-Qiang2,3,4; Li, Xiang-Min2,3,4; Yu, Ji-Yuan2,3,4; Bu, Tao3,4; Huang, Bo-Tao4; Liu, Yu-Jie1
刊名GEOLOGICAL MAGAZINE
出版日期2021-12-06
页码16
关键词high-Mg andesites geochemistry petrogenesis tectonic setting Late Devonian Beishan Central Asian Orogenic Belt
ISSN号0016-7568
DOI10.1017/S0016756821001151
通讯作者Wang, Guo-Qiang(gqwangmint@gmail.com)
英文摘要High-Mg andesites (HMAs) are crucial for the reconstruction of plate tectonics, continental margin formation and lithospheric evolution. In this study, we present new fossil age, whole-rock geochemical and Sr-Nd isotope data on the newly discovered Dundunshan Group HMAs in the Dundunshan area of the Beishan orogen (central-southern Central Asian Orogenic Belt). The Dundunshan HMA samples are characterized by high MgO (6.47-7.02 wt%) contents and high Mg-# values (67.27-68.77), with SiO2 (58.57-62.13 wt%), Al2O3 (14.49-16.07 wt%) and CaO (5.05-6.24 wt%) resembling typical HMAs. The Dundunshan HMA samples are calc-alkaline and strongly enriched in light rare earth elements (LREEs) and large-ion lithophile elements (LILEs), with slightly negative Eu anomaly and high-field-strength element (HFSE) depletions. Their (Sr-87/Sr-86)(i) ratios (0.7041-0.7057) and epsilon(Nd(t)) (3.73-5.59) indicate that the Dundunshan HMAs were mainly formed by the interactions between subducted oceanic sediment-derived melts and mantle peridotites. Fossil evidence and published radiometric age data constrain the formation of the Dundunshan HMAs to early Late Devonian time. Sedimentological features of the Middle Devonian Sangejing Formation and regional tectonic correlation suggest that the Hongliuhe-Niujuanzi-Xichangjing Ocean in the Dundunshan area was likely closed during late Middle Devonian time, and that the Dundunshan HMAs were formed in a post-collision extensional setting.
WOS关键词SETOUCHI VOLCANIC BELT ; ZIRCON U-PB ; NIUJUANZI OPHIOLITIC MELANGE ; PHANEROZOIC CRUSTAL GROWTH ; SOUTHERN TIEN-SHAN ; SLAB-DERIVED MELTS ; A-TYPE GRANITES ; CENTRAL-ASIA ; POSTCOLLISIONAL MAGMATISM ; GEOCHEMICAL EVIDENCE
资助项目National Natural Science Foundation for Youth of China[41703038] ; Natural Science Foundation of Shaanxi Province[2015JM4144] ; China Geological Survey Project[DD20190812]
WOS研究方向Geology
语种英语
WOS记录号WOS:000727554400001
出版者CAMBRIDGE UNIV PRESS
资助机构National Natural Science Foundation for Youth of China ; Natural Science Foundation of Shaanxi Province ; China Geological Survey Project
源URL[http://ir.ieecas.cn/handle/361006/17281]  
专题地球环境研究所_科技外事处
通讯作者Wang, Guo-Qiang
作者单位1.Chinese Acad Sci, Inst Earth Environm, Xian 710061, Shaanxi, Peoples R China
2.Northwest China Ctr Geosci Innovat, Xian 710054, Shaanxi, Peoples R China
3.China Geol Survey, Ctr Orogen Belt Geol, Xian 710054, Shaanxi, Peoples R China
4.China Geol Survey, Xian Ctr, Xian 710054, Shaanxi, Peoples R China
推荐引用方式
GB/T 7714
Wang, Guo-Qiang,Li, Xiang-Min,Yu, Ji-Yuan,et al. Petrogenesis and tectonic setting of Late Devonian high-Mg andesites in the Beishan orogen, NW China[J]. GEOLOGICAL MAGAZINE,2021:16.
APA Wang, Guo-Qiang,Li, Xiang-Min,Yu, Ji-Yuan,Bu, Tao,Huang, Bo-Tao,&Liu, Yu-Jie.(2021).Petrogenesis and tectonic setting of Late Devonian high-Mg andesites in the Beishan orogen, NW China.GEOLOGICAL MAGAZINE,16.
MLA Wang, Guo-Qiang,et al."Petrogenesis and tectonic setting of Late Devonian high-Mg andesites in the Beishan orogen, NW China".GEOLOGICAL MAGAZINE (2021):16.

入库方式: OAI收割

来源:地球环境研究所

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