Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (1): 97-111.doi: 10.13278/j.cnki.jjuese.20180284

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Petrogenesis of Late Carboniferous Granitic Plutons in Xinlin Area, Northern Great Xing'an Range and Their Geological Significance

Zhou Chuanfang, Yang Huaben, Li Xiangwen, Liu Yu, Liu Tao, Chen Zhuo, Cai Yanlong, Liu Ningbo, Wang Bochao, Wang Dake   

  1. Harbin Center for Integrated Natural Resources Survey, China Geological Survey, Harbin 150086, China
  • Received:2018-11-06 Published:2020-02-11
  • Supported by:
    Supported by Project of China Geological Survey (1212011220666,DD20191014)

Abstract: The Late Carboniferous granites, including Dawusu and Fuxili plutons, consist of monzogranie and granodiorite. The LA-ICP-MS zircon U-Pb date indicates that the emplaced ages of these two plutons are (303.7±2.2)Ma and(300.5±0.5)Ma, formed by the Late carboniferous magmatism. The plutons are characterized by high silica (w(SiO2)=66.77%-75.85%), alkali (w(Na2O+K2O)=7.41%-8.69%) and alumina (w(Al2O3)=12.90%-16.22%),with low MgO, CaO,and TiO2. They are of calcalkaline series and peraluminous as indicated by A/CNK ratio of 1.06-1.44. Different from the aluminum-rich S type granite, no aluminum-rich minerals such as native muscovite, cordierite, and garnet were seen under the microscope. Conversely, the plutons show I type granite characteristics with negative correlation between P2O5 and SiO2. The rocks are enriched in LREE, Ba, Rb and K with negative Nb, Ta and Ti anomalies, which is similar to that of the post-orogenic I type granitoids, indicating the plutons formed in an extensional tectonic environment. The w(87Sr/86Sr)ratio of the monzogranie is 0.712 938, and w(143Nd/144Nd) is 0.512 386 with the initial w(87Sr/86Sr)i and εNd(t)value of 0.704 4 and-1.09 respectively, indicating the source material is mainly the crust material from the depleted mantle. This is supported by the young Nd model age (TDM2=1 172 Ma). Combined with the previous studies in the regional tectonics, the Dawusu and Fuxili plutons are related to the lithosphere extension after the orogenic collision between the Erguna-Xing'an block and the Songnen block.

Key words: Northern Great Xing'an Range, Late Carboniferous, Xinlin, granite, U-Pb dating, petrogenesis

CLC Number: 

  • P588.1
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