Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (4): 1085-1104.doi: 10.13278/j.cnki.jjuese.20170179

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Detrital Zircon U-Pb Geochronology and Hf Isotope of Phyllite of Langyashan Formation in Hongshuihe Iron Ore District of Eastern Kunlun and Their Geological Significance

Zhang Qiang, Ding Qingfeng, Song Kai, Cheng Long   

  1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2017-12-20 Online:2018-07-26 Published:2018-07-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41572056)

Abstract: The Hongshuihe iron ore district is located in the north-middle part of the eastern Kunlun orogenic belt. On the basis of geological field work, the authors applied petrography, geochemistry, LA-ICP-MS detrital zircon U-Pb geochronology,and Hf isotope to the ore-hosting phyllite of the Langyashan Formation. The results of the main and trace elements showed that the original rocks of the phyllite of the Langyashan Formation were possibly composed of high-maturity sandstones from the crust source, showing the warm and humid paleo-climate and paleo-geographic features. The original rocks were experienced the medium-high degree chemical weathering, whose provenance was the felsic rocks with low content of alkaline feldspar. Their sedimentary tectonic environment might be on the edge of the passive continent. The detrital zircon geochronological results showed that the sedimentary age of the phyllite was between (788±9) Ma and (515.2±4.4) Ma, different from the age of Jixianian. The Hongshuihe iron deposit should be one of the examples of the global banded iron formations, which reflect the end of the Sturtian ice age. In addition, the εHf(t) values of these detrital zircons varies from -30.4 to 8.3, indicating that the composition of Hf isotope sources is highly heterogeneous, with a two-stage model age of 3 596-1 448 Ma, which indicates that the source rocks of these zircons include both newborn crust material and reconstructed ancient crust material. The newborn crust might be from Mesoproterozoic, and the reconstructed crust might be from Archean. Through discussing on the classification of zircon ages and comparing the ages of some old sedimentary strata and intrusive rocks of the adjacent areas, it is inferred that the basement of Archean, Baishahe Formation, Xiaomiao Group, Wanbaogou Group and the intermediate-acid rocks formed in the eastern Kunlun in the late period of Mesoproterozoic are the possible provenances.

Key words: Hf isotope, detrital zircons, geochemistry, phyllite, Hongshuihe iron deposit, eastern Kunlun orogenic belt

CLC Number: 

  • P597.3
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