Basement nature and origin of the Junggar terrane: New zircon U-Pb-Hf isotope evidence from Paleozoic rocks and their enclaves
文献类型：期刊论文
| 作者 | Xu, Xing-Wang1,2; Li, Xian-Hua1; Jiang, Neng1; Li, Qiu-Li1; Qu, Xun3; Yang, Yue-Heng1; Zhou, Gang3; Dong, Lian-Hui3 |
| 刊名 | GONDWANA RESEARCH
 |
| 出版日期 | 2015-08-01 |
| 卷号 | 28期号:1页码:288-310 |
| 关键词 | Zircon U-Pb-Hf isotope evidence Basement nature Origin The Junggar terrane Southern Laurentia |
| DOI | 10.1016/j.gr.2014.03.011 |
| 文献子类 | Article |
| 英文摘要 | The question of whether the Junggar terrane in the central area of the Central Asian Orogenic Belt (CAOB) has a Precambrian basement is one of the hottest topics surrounding the tectonic evolution of the CAOB. Recent work shows that the Central Tianshan range has a Mesoproterozoic-Neoproterozoic basement Here, we reported the SIMS U-Pb age and Hf isotopes of zircons from newly discovered dioritic gneiss and magnetite quartzite enclaves and their host diorite dike in the Taheir area, deformed Ordovician conglomerate in the Dazigou area, and mica gneiss relicts and their host granite in the Shuangchagou area in the Junggar terrane. The results reveal the following evidence: 1) the dioritic gneiss was metamorphosed from 2.52 Ga diorite at approximately 1.88 Ga, the magnetite quartzite interlayered with hornblende-plagioclase gneiss layers has an age of approximately 1.92 Ga, and the inherited zircons from the diorite TH4-6 contain three zircon populations with upper intercept ages of approximately 3.06 Ga, 1.98 Ga and 1.89 Ga; 2) the sienna and colorless zircon populations from the conglomerate reveal two magmatic rocks with ages of approximately 1.86 Ga and 0.94 Ga; and 3) the magmatic zircons that form mica gneiss have T-DMC and T-DM2 ages ranging from 1.2 Ga to 2.08 Ga, and the inherited zircons from the mica gneiss and granite in the Shuangchagou area contain five zircon populations with upper intercept ages of approximately 2.48 Ga, 1.80 Ga, 1.47 Ga, 1.14 Ga and 0.96 Ga. |
| WOS关键词 | ASIAN OROGENIC BELT ; PHANEROZOIC CRUSTAL GROWTH ; DUCTILE COMPRESSIONAL ZONE ; EASTERN TIANSHAN MOUNTAINS ; CHINESE TIEN-SHAN ; A-TYPE GRANITES ; CONTINENTAL-CRUST ; NW CHINA ; TECTONIC EVOLUTION ; DETRITAL ZIRCONS |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000356743000018 |
| 资助机构 | National Natural Science Foundation of China(41390422 ; National Natural Science Foundation of China(41390422 ; CAS(kzcx-ew-ly03 ; CAS(kzcx-ew-ly03 ; National 305 project(2011BAB06B03-3 ; National 305 project(2011BAB06B03-3 ; 41072060) ; 41072060) ; kzcx2-yw-107) ; kzcx2-yw-107) ; 2006BAB07B01-03) ; 2006BAB07B01-03) ; National Natural Science Foundation of China(41390422 ; National Natural Science Foundation of China(41390422 ; CAS(kzcx-ew-ly03 ; CAS(kzcx-ew-ly03 ; National 305 project(2011BAB06B03-3 ; National 305 project(2011BAB06B03-3 ; 41072060) ; 41072060) ; kzcx2-yw-107) ; kzcx2-yw-107) ; 2006BAB07B01-03) ; 2006BAB07B01-03) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/62358]  |
| 专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Key Lab Mineral Resources, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Peoples R China 3.Xinjiang Bur Geol & Mineral Resources, Urumqi 830000, Xinjiang, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xu, Xing-Wang,Li, Xian-Hua,Jiang, Neng,et al. Basement nature and origin of the Junggar terrane: New zircon U-Pb-Hf isotope evidence from Paleozoic rocks and their enclaves[J]. GONDWANA RESEARCH,2015,28(1):288-310. |
| APA | Xu, Xing-Wang.,Li, Xian-Hua.,Jiang, Neng.,Li, Qiu-Li.,Qu, Xun.,...&Dong, Lian-Hui.(2015).Basement nature and origin of the Junggar terrane: New zircon U-Pb-Hf isotope evidence from Paleozoic rocks and their enclaves.GONDWANA RESEARCH,28(1),288-310. |
| MLA | Xu, Xing-Wang,et al."Basement nature and origin of the Junggar terrane: New zircon U-Pb-Hf isotope evidence from Paleozoic rocks and their enclaves".GONDWANA RESEARCH 28.1(2015):288-310. |
入库方式： OAI收割
来源：地质与地球物理研究所
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