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
Detrital Zircon U-Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications

文献类型：期刊论文

作者Cui Weilong2,3; Zeng Zhen1,4; Zhang Xingzhou1; Liu Zhenghong1; Wang Shijie1; Pu Jianbin1; Fu Qiulin1; Guo Ye1
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
出版日期2019-10-01
卷号93期号:5页码:1559-1579
关键词Jiamusi massif Nanshuangyashan Formation Late Triassic detrital zircon NE China
ISSN号1000-9515
DOI10.1111/1755-6724.14351
英文摘要A suite of the fossil-rich marine-land interbedded strata (Nanshuangyashan Formation) is distributed at the eastern margin of the Jiamusi massif in the eastern Heilongjiang Province, NE China. The authors had recently discovered a suite of arkose beneath the marine-land interbedded strata, which overlays unconformably on the Permain granite in the eastern margin of the Jiamusi massif. The LA-ICP-MS zircon U-Pb dating indicate that all detrital zircons from the analysed four arkose samples show the four population ages of >800 Ma, 538-481 Ma, 269-250 Ma and 223-215 Ma. The former three population ages are widely recorded in the Jiamusi-Khanka massif and the Songnen massif. The later group is the minimal age population in the analyzed samples, limiting the sedimentation time of the arkoses occurred after the Late Triassic. At present, the minimal age population is not recorded in the Jiamusi massif, but the granites with the ages of 228-210 Ma are widely distributed in the Songnen-Zhangguangcai Range massif and the Khanka massif. The predominantly Permian zircons are characterized by oscillatory zoning and euhedral shapes, with variable zircon epsilon(Hf)(t) values (-5.5 to +11.2), indicating that they were derived from mixture sources, possibly mixed with components of the Songnen-Zhangguangcai Range massif and the Jiamusi-Khanka massif. These results, combined with regional analyses, indicate that the closing of Mudanjiang ocean and Panthalassa ocean possibly existed from Early Permian to Late Triassic.
WOS关键词HF ISOTOPIC COMPOSITIONS ; A-TYPE GRANITES ; NORTHEASTERN CHINA ; KHANKA MASSIF ; TRACE-ELEMENT ; HEILONGJIANG PROVINCE ; ACCRETIONARY COMPLEX ; STANDARD ZIRCONS ; METAMORPHIC BELT ; LU-HF
资助项目National Natural Science Foundation of China[41474081] ; China Geological Survey[1212011120973]
WOS研究方向Geology
语种英语
WOS记录号WOS:000493023200023
出版者WILEY
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Geological Survey ; China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Geological Survey ; China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Geological Survey ; China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Geological Survey ; China Geological Survey ; China Geological Survey ; China Geological Survey
源URL[http://ir.iggcas.ac.cn/handle/132A11/95770]  
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Zeng Zhen
作者单位1.Jilin Univ, Coll Earth Sci, Changchun 130061, Jilin, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.China Aerosp Acad Architectural Design & Res Co L, Beijing 100162, Peoples R China
推荐引用方式
GB/T 7714		 Cui Weilong,Zeng Zhen,Zhang Xingzhou,et al. Detrital Zircon U-Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2019,93(5):1559-1579.
APA Cui Weilong.,Zeng Zhen.,Zhang Xingzhou.,Liu Zhenghong.,Wang Shijie.,...&Guo Ye.(2019).Detrital Zircon U-Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications.ACTA GEOLOGICA SINICA-ENGLISH EDITION,93(5),1559-1579.
MLA Cui Weilong,et al."Detrital Zircon U-Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications".ACTA GEOLOGICA SINICA-ENGLISH EDITION 93.5(2019):1559-1579.

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。