Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (6): 1741-1755.doi: 10.13278/j.cnki.jjuese.20170299

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Formation Age, Geochemical Characteristics and Genesis of Granites in Northeastern Jiagedaqi of Daxing'anling

Yin Zhigang1, Li Haina1, Zhang Hai2, Hao Ke1, Pang Xuechang1, Gong Zhaomin1, Li Min1, Zhang Shengting1   

  1. 1. College of Mining Engineering, Liaoning Technical University, Fuxin 123000, Liaoning, China;
    2. Qiqihar Branch, Heilongjiang Institute of Geological Survey, Qiqihar 161005, Heilongjiang, China
  • Received:2018-09-07 Published:2018-11-26
  • Supported by:
    Supported by Project of China Geological Survey (1212011120671)

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Abstract: The study area is located in the northeastern part of the Xing'an block in DaXing'anling. The main types of rocks focused on are alkali feldspar granite and granite porphyry, and their formation age, geochemical characteristics, genesis and tectonic setting were studied in depth. The results show that SiO2 has a high mass fraction, with high A12O3, TFeO/MgO, poor MgO, TiO2, P2O5, etc.. A/NK-A/CNK and w(K2O)-w(SiO2) diagrams show that the samples are mainly of peraluminous, high potassium calc alkaline granites. All the (Na2O+K2O)/CaO-w(Zr+Nb+Ce+Y), TFeO/MgO-w(Zr+Nb+Ce+Y) and zircon saturation temperatures show that the rocks are of highly fractionated I-type granites. The emplacement age of the rock mass obtained from zircon LA-ICP-MS U-Pb dating is 128-124 Ma. It is concluded that the tectonic setting of the geotectonic background was the crustal extension in the late stage of continental collision orogeny after the extinction of the Mongolia-Okhotsk Ocean. The magma was originated from the partial melting of igneous source rocks.

Key words: zircon U-Pb chronology, rock geochemistry, tectonic setting, granite rock, Daxing'anling

CLC Number: 

  • P588.1
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