Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (5): 1433-1449.doi: 10.13278/j.cnki.jjuese.20200085

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Late Paleozoic Tectonic Evolution of Beishan Orogenic Belt: Chronology and Geochemistry Constraints of Early Permian Syenogranitic Porphyry Dyke in Liuyuan Area, Gansu Province

Sun Hairui1,2, Lü Zhicheng1,2, Yu Xiaofei1,2, Li Yongsheng1,2, Du Zezhong1,2, Lü Xin1,2, Gong Fanying1,2   

  1. 1. Development and Research Center, China Geological Survey, Beijing 100037, China;
    2. Mineral Exploration Technical Guidance Center, Ministry of Natural Resources, Beijing 100083, China
  • Received:2020-04-12 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by National Key R & D Program of China (2018YFC0603806,2018YFC0603704), Project of China Geological Survey (DD20160050) and Fundamental Research Funds for the Central Universities (310827171122)

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Abstract: Beishan orogenic belt is located in the middle part of Central Asia orogenic belt (CAOB), and it is crucial to discuss the accretionary evolution of the CAOB. Liuyuan area is in the southern part of Beishan orogenic belt, where granitoid rocks and different types of dykes are widely distributed. To study these rocks and dykes can provide us with more important clues about the reconstruction of the geological evolution of this area. The LA-ICP-MS zircon U-Pb dating of the syenogranitic porphyry dyke in northeast Liuyuan area yields the weighted 206Pb/238U ages of (288.5±1.4) Ma, the Early Permian. The geochemical results show that the contents of SiO2 and total alkali of the syenogranitic porphyry are high,while the contents of Fe, Mg, Ca, Al and P are low. In addition, the porphyry is characterized by rich in Rb, Th, U and Pb but poor in Ba, Nb, La, Ce, Sr and Ti, with obvious Eu negative anomaly. The value of Rb/Sr is high, the value of K/Rb is low, and the saturation temperature of zircon is lower (730-844 ℃, concentrating around 740 ℃). Based on the above geochemical results and the comprehensive discriminant analysis, we believe that the porphyry belongs to high-K calc-alkaline and high fractionated I-type granites. Also, the syenogranitic porphyry presents a narrow range of Zr/Hf (18.42 to 28.01, average 22.37) and Th/U values (3.82 to 7.99, average 5.34) respectively, which is similar to those of crust sourced rocks. The syenogranitic porphyry show positive εHf (t) values, varying from 2.94 to 9.66, with average of 5.72, and relatively young TDM2 ages, ranging from 955 to 611 Ma. Considering the occurrences of the coeval mafic igneous rocks in this region, we believe that the porphyry magma should be mainly derived from the partial melting of the crust-derived metamorphic igneous rocks with some contribution of mantle materials. The tectonic discriminant analysis shows that the Early Permian syenogranitic porphyry was formed in a subduction environment. Based on the previous studies on the regional tectonic deformation, basin sediment source, and the magma evolution from Permian to Triassic, it is concluded that the accretionary orogenic events in the southern part of Beishan orogenic belt lasted at least until the Early Permian, which provided important constraints on the reconstruction of the tectonic evolution of the Late Paleozoic Beishan orogenic belt.

Key words: syenogranitic porphyry dyke, high fractionated I-type granite, geochemistry, Early Permian, Beishan area, Central Asia orogenic belt

CLC Number: 

  • P588.1
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