Home > Archive>Volume 93, Issue 5, 2019 >1559-1579. DOI:10.1111/1755-6724.14351
PDF HTML XML Export Cite reminder
Detrital Zircon U-Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications
CSTR:
[cstr]
Author:
Fund Project:

We are grateful to Yang Yueheng and Ma Qian of the Institute of Geology and Geophysics, Chinese Academy of Sciences (Beijing), China, for their advice and assistance during Lu-Hf isotope analyses. We thank the Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources, Jilin University, Changchun, China for assistance in zircon U-Pb dating. The final version of this paper benefited from perceptive comments by Li Shan (Guest Editor) and two anonymous reviewers. This study is financially supported by National Natural Science Foundation of China (Grant No. 41474081) and the projects from China Geological Survey (Grant No. 1212011120973).

  • Article
    • | |
  • Metrics
    • |
  • Reference
    • |
  • Related
    • |
  • Cited by
    • | |
  • Comments
    Abstract:

    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 εHf(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.

    Reference
    Related
    Cited by
Get Citation

CUI Weilong, ZENG Zhen, ZHANG Xingzhou, LIU Zhenghong, WANG Shijie, PU Jianbin, FU Qiulin, GUO Ye.2019. Detrital Zircon U-Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications[J]. Acta Geologica Sinica(),93(5):1559-1579

Copy
Share
Article Metrics
  • Abstract:
  • PDF:
  • HTML:
  • Cited by:
History
  • Received:May 15,2019
  • Revised:August 14,2019
  • Online: October 29,2019
Article QR Code
You are the Visitors
Governing Body：China Association for Science and Technology
Organizer：Geological Society of China
Address：No. 26 Baiwanzhuang Street, Xicheng District, Beijing 100037, China
Phone：010-68999024

京公网安备 11000002000088号 | 京ICP备11041704号
® 2025 All Rights Reserved