内蒙古锡林浩特地区中元古代锡林浩特岩群的厘定及其意义

周文孝; 葛梦春

doi:10.3799/dqkx.2013.070

Volume 38 Issue 4

Jul. 2013

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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

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

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.
- Xilinhot Group,
- metamorphic basement,
- Xilin Gol complex,
- Xilin Gol micro block,
- petrology

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References(39)

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Redefinition and Significance of Metamorphism Xilinhot Group in Xilinhot Area, Inner Mongolia, China

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