Volume 38 Issue 4
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ZHOU Wen-xiao, GE Meng-chun, 2013. Redefinition and Significance of Metamorphism Xilinhot Group in Xilinhot Area, Inner Mongolia, China. Earth Science, 38(4): 715-724. doi: 10.3799/dqkx.2013.070
Citation: ZHOU Wen-xiao, GE Meng-chun, 2013. Redefinition and Significance of Metamorphism Xilinhot Group in Xilinhot Area, Inner Mongolia, China. Earth Science, 38(4): 715-724. doi: 10.3799/dqkx.2013.070
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Redefinition and Significance of Metamorphism Xilinhot Group in Xilinhot Area, Inner Mongolia, China

doi: 10.3799/dqkx.2013.070

  • Geological Survey, China University of Geosciences, Wuhan 430074, China

  • Received Date: 2013-12-01
  • Publish Date: 2013-07-01
    Abstract
  • Based on large scale geologic mapping and measuring section, the Xilin Gol complex is divided into three parts: supracrustal rock, Late Proterozoic basic-ultrabasic rock and Early Paleozoic acid intrusive rocks. According to lithologic association and characteristics of deformation and metamorphism, biotite (garnet) plagioclase gneiss intercalated with several layers barred amphibolite, with thin layer magnetite quartzite on its top; medium-coarse biotite plagioclase gneiss and fine-grained felsic gneiss; lithologic association of migmatization banding biotite (hornblende) plagioclase gneiss and garnet monzonitic gneiss intercalated with barred amphibolite; sillimanite biotite plagioclase gneiss, barred biotite plagioclase gneiss, intercalated with garnet bearing biotite quartz schist. Comparison study on the different lithologic association, metamorphic characteristics and depositional environment of Baoyintu Group, Ailegemiao Formatio, Bainaimiao Group and others. This paper proposes to redefine these supercrustal rocks named "Xilinhot Group", which compose the Precambrian metamorphic basement of Xilin Gol micro block. It's important to study the formation and development of Xilin Gol micro block and the evolution of structural relationship between Siberia plate and North China plate.

     

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