Volume 44 Issue 1
Jan.  2019
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Article Navigation >  Earth Science  > 2019  >  44(1): 268-283
Yang Zeli, Wang Shuqing, Hu Xiaojia, Xin Houtian, Li Chengdong, 2019. Petrogenesis of the Late-Carboniferous Granites of Dalaimiao, Inner Mongolia and Its Implications for the Tectonic Transformation of Northern Margin of Xing'an-Mongolian Orogenic Belt. Earth Science, 44(1): 268-283. doi: 10.3799/dqkx.2018.260
Citation: Yang Zeli, Wang Shuqing, Hu Xiaojia, Xin Houtian, Li Chengdong, 2019. Petrogenesis of the Late-Carboniferous Granites of Dalaimiao, Inner Mongolia and Its Implications for the Tectonic Transformation of Northern Margin of Xing'an-Mongolian Orogenic Belt. Earth Science, 44(1): 268-283. doi: 10.3799/dqkx.2018.260
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Petrogenesis of the Late-Carboniferous Granites of Dalaimiao, Inner Mongolia and Its Implications for the Tectonic Transformation of Northern Margin of Xing'an-Mongolian Orogenic Belt

doi: 10.3799/dqkx.2018.260

  • Tianjin Center of China Geological Survey, Tianjin 300170, China

  • Received Date: 2018-04-12
  • Publish Date: 2019-01-15
    Abstract
  • The Dalaimiao pluton crops out in the northern of Suzuoqi, near the border areas between China and Mongolia, which is referred as an important component of the Erenhot-East Ujimqin Late Paleozoic arc magmatic belt and its petrogenesis can provide insights into the tectonic evolution of the northern margins of Xing'an-Mongolian orogenic belt. Based on field investigation, geochronology and geochemistry, it is found that the pluton lithologically consists of medium-fine grained biotite granites in the center and medium-grained granites on the margin. Zircon U-Pb dating yields a weighted mean age of 301.2±2.1 Ma (MSWD=1.2, 2σ), indicating these granites were generated during a Late Carboniferous magmatic event. All of these granites are highly siliceous, Fe-poor, slightly peraluminous, and show enrichments in Rb, Th, U, Pb and depletions in Ba, Sr, P, Nb and Ta. The medium-fine grained biotite granites are Na-rich, and have high concentrations of heavy rare earth elements (REE), whereas the medium-grained granites show higher K2O contents, more significant elemental differentiation and negative europium anomalies. Dalaimiao pluton shows depleted isotopic compositions with (87Sr/86Sr)i=0.703 6-0.707 5, εNd(t)=0.08-2.77, and positive εHf(t) values of 4.70-11.50. Integrated geochronology and geochemical data suggest the Dalaimiao pluton is genetically classified as I-type granites, with some geochemical features of A-type granites. The Dalaimiao granites derived from partial melting of juvenile crust which were generated by the underplating of mantle material, and were formed in a tectonic transitional stage from compression uplift to intracontinental extension. Emplacement of Dalaimiao pluton provides more detailed constraints on the specific timing of tectonic variation in the northern margins of Xing'an-Mongolian orogenic belt during the Late Carboniferous.

     

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