内蒙古达来庙地区晚石炭世花岗岩成因及其对兴蒙造山带北部构造体制转变的指示

杨泽黎; 王树庆; 胡晓佳; 辛后田; 李承东

doi:10.3799/dqkx.2018.260

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

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

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, ε_Nd(t)=0.08-2.77, and positive ε_Hf(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.
- granites,
- Late Paleozoic,
- Xing-Meng orogenic belt,
- petrogenesis,
- transformation of tectonic setting,
- geochemistry

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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

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