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Zircon U-Pb ages, geochemical characteristics and tectonic implications of volcanic rocks from Manitu Formation of Suolun area in central Great Xing'an Range
DU Yue-dan1, HE Zhong-hua1, SUI Zhen-min2, TAN Hao-yuan1, REN Zi-hui1
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. College of Resources and Environmental Science, Jilin Agricultural University, Changchun 130118, China
Abstract:

The volcanic rocks in Manitu Formation of Suolun area are composed of andesite, trachy-andesite and dacite petrographically,but they are mainly basaltic andesite or trachy-andesite with minor rhyolite based on chemical composition. Zircon U-Pb dating results show that they formed in Early Cretaceous from 130 to 132 Ma. These volcanic rocks belong to high-K calc-alkaline series. They are high in total rare earth elements (∑REE=95.19×10-6��198.38×10-6), with high LREE/HREE(6.38��10.59) and negative Eu anomalies (δEu=0.68��1.01). The volcanic rocks are enriched in LILE(K, Rb, Th)and LREE, but depleted in HFSE(Nb, Ta, P, Ti). Trace elements are characterized by high Sr (>499×10-6), low Yb (the maximum is 2.83×10-6, <3.6×10-6) and Y (majority <29.9×10-6), and high ratio of Sr/Y and low ratio of Rb/Sr, indicating the characteristic of arc volcanic rocks. The volcanic rocks have positive values of εHf(t) (7.3��13.7), and the initial 176Hf/177Hf ratios for magmatic zircons is 0.282 964, suggesting that the andesitic magma of Manitu Formation was derived from the lithosphere mantle and partial melting of newly accreted lower crust, and is affected by the subduction fluid. Volcanic rocks of Manitu Formation formed in the island arc tectonic environment caused by the subductions of the Paleo-Pacific Plate beneath the Eurasian continent.

Keywords: central Great Xingan Range   Inner Mongolia   Suolun   Manitu Formation   zircon U-Pb dating   geochronology   Hf isotope  
�ո����� 2016-11-02 �޻����� 2017-05-03 ����淢������  
DOI: 10.3969/j.issn.1004-5589.2017.02.003
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