Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (6): 1724-1739.doi: 10.13278/j.cnki.jjuese.201606111

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Petrogenesis of Rhyolite from Hongshanzi Basin in Southern Greater Xing'an Range: Elements and Sr-Nd-Pb Isotope Constraints

Wu Jianhua1, Xie Kairui2, Zhu Hongtao3, Wu Rengui2, Liu Shuai1   

  1. 1. State Key Laboratory Breeding Base of Nuclear Resources and Environment, East China Institute of Technology, Nanchang 330013, China;
    2. Collage of Earth Science, East China Institute of Technology, Nanchang 330013, China;
    3. NO. 243 Geological Party, CNNC, Chifeng 024006, Inner Mongolia, China
  • Received:2016-02-07 Online:2016-11-26 Published:2016-11-26
  • Supported by:
    Supported by Project of National Natural Science Foundation of China (41372071) and Project of CNNC (2008-74)

Abstract: The Hongshanzi early Late Jurassic volcanic basin is located in Keshenketeng Banner, Inner Mongolia, the southern tip of the Greater Xing'an Range. Its tectonic position is within the Liaoyuan block between the Xilamulun-Changchun suture zone and the Kangbao-Weichang-Chifeng-Kaiyuan fault belt. The fresh red and grey rhyolites, in Hongshanzi basin, are the wall rocks of hydrothermal-type U-Mo deposits. Both have the features of rich in SiO2, K2O and high ratio of Fe2O3/FeO, with lack of Al2O3, CaO and MgO contents, the fresh red rhyolite is higher in(K2O+Na2O) contents and Fe2O3/FeO ratio, while lower in SiO2. Both fresh red and grey rhyolites, are relatively high the total amount of REE, showing rich LREE obviously and right REE patterns, with negative Eu anomalies. The high contents of HSFE(Nb, Ta, Zr, Hf, Ce, Y, Ga) and LIRE(Rb, Th, U), low contents of the LIRE Ba and Sr, show the trace elements feature of A1 type rhyolite, low Ba-Sr type rhyolite and the extensional tectonic setting. The rhyolites have smaller (87Sr/86Sr)i, higher εNd(t), younger TDM2,lower (206Pb/204Pb)i, (207Pb/204Pb)i, (208Pb/204Pb)i. Obviously, both fresh red and grey rhyolites were formed by the partial melting of Mid-Mesoproterozoic young lower crust materials originated from the EMⅠenriched mantle under the extensional tectonic setting within the plates, and had been accompanied by the fractional crystallization during the magmatic process. Their differences may be related to the different composition of young lower crustal materials.

Key words: rhyolite, Sr-Nd-Pb isotopes, early Late Jurassic, Hongshanzi basin, the southern tip of Greater Xing'an Range

CLC Number: 

  • P548.141
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