大兴安岭南端红山子盆地流纹岩的成因:元素和Sr-Nd-Pb同位素制约

doi:10.13278/j.cnki.jjuese.201606111

Abstract

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 ε_Nd(t), younger T_DM2,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

Wu Jianhua, Xie Kairui, Zhu Hongtao, Wu Rengui, Liu Shuai. Petrogenesis of Rhyolite from Hongshanzi Basin in Southern Greater Xing'an Range: Elements and Sr-Nd-Pb Isotope Constraints[J].Journal of Jilin University(Earth Science Edition), 2016, 46(6): 1724-1739.

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

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