Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (1): 118-131.doi: 10.13278/j.cnki.jjuese.20170160

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Age and Provenance of Early Paleozoic Sedimentary Formation in Northern Jiamusi Massif: Evidence from U-Pb Ages and Hf Isotope Compositions of Detrital and Magmatic Zircons

Qiao Jian, Luan Jinpeng, Xu Wenliang, Wang Zhiwei, Zhao Shuo, Guo Peng   

  1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2017-02-07 Online:2018-01-26 Published:2018-01-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41330206,41672050)

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Abstract: In this paper, we present the LA-ICP-MS/SIMS U-Pb ages and Hf isotope compositions of detrital zircons from the metasedimentary rocks and intrusive rocks within the Jinyinku Formation in the northern Jiamusi massif to constrain the depositional ages and provenance of the strata. All the zircons separated from our three samples are euhedral-subhedral in shape,and display striped absorption and/or oscillatory growth zoning patterns in CL images, implying their magmatic origin. The dating results indicate that the 72 analytical spots of zircons from a sericite schist yield ages between 1 955 Ma and 457 Ma that can be subdivided into five age populations with peaks at 814, 757, 568, 491, and 463 Ma. Their εHf (t) values and two-stage model ages (TDM2) range from -13.9 to -0.1 and from 2 411 to 1 715 Ma, respectively. The zircons from aplite and diabase that intruded in the Jinyinku Formation yield weighted mean ages of 263 Ma and 267 Ma, respectively. Additionally, the former has the εHf (t) values of 0.9-2.0 and TDM2 ages of 1 110-1 047 Ma;whereas the latter has the εHf (t) values of -7.7-6.4 and TDM1 ages of 1 206-662 Ma. In consideration with the occurrence of the granitoids with the ages of~430 Ma within the Jiamusi massif, zircon age populations, and Hf isotopic compositions, we conclude that the Jinyinku Formation formed between 463 Ma and 430 Ma (i.e., Late Ordovician to Early Silurian) in a passive continental margin setting,and sourced mainly from Neoproterozoic and Early Paleozoic terrane in the Jiamusi massif and adjacent regions.

Key words: Jiamusi massif, Jinyinku Formation, depositional age, provenance, detrital zircon, Hf isotope

CLC Number: 

  • P597.3
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