Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (3): 709-726.doi: 10.13278/j.cnki.jjuese.20180266

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Chronology and Geochemistry of Neoarchean Metamorphic Intrusive Rocks in Hongshanzi, Inner Mongolia

Wang Chunguang1, Dong Xiaojie1, Xu Zhongyuan1, Ren Yunwei2, Wang Wenlong2, Chen Yusong1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Tianjin Center, China Geological Survey, Tianjin 300170, China
  • Received:2018-10-19 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by National Nature Science Foundation of China(41872194) and Project of China Geological Survey(1212010510515)

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Abstract: A set of complicated granites are exposed in the Yinshan granite-greenstone belt of the western block of North China craton. The research on the types, genesis and relationship with greenstone belt is of great significance to discuss the formation and evolution of the granite-greenstone belt. The authors studied the granite greenstone belt in the red mountain area in the west side of the Sanheming iron deposit in Inner Mongolia. The greenstone belts contain not only a large amount of epi-crust rocks such as metamorphic Komatite, Komatite basalt, and tholeiite, but also a variety of metamorphic intrusive rocks. The study shows that there are mainly three types of intrusive rocks related to the greenstone belt in this area, namely metamorphic quartz diorite, metamorphic granite diorite, and metamorphic granite. The geochemistry and zircon dating of metamorphic quartz diorite and metamorphic granite were obtained in this study. Metamorphic quartz diorite is Archean high-alumina TTG rocks, with higher aluminum and potassium, lower magnesium, and strong differentiation of REEs. The SHRIMP zircon U-Pb age is 2534±7 Ma (MSWD=1.3), which is cotemporary with Sanukite and TTG in the southern part of the study area. The metamorphic granites belong chemically to a calcalkaline per-aluminous series, rich in silica and alkali, and low in iron, magnesium, titanium and manganese. The SHRIMP zircon U-Pb age is 2509±7 Ma (MSWD=1.5). The field geological phenomena show that metamorphic granite obviously intruded into greenstone strata and metamorphic quartz diorite. The study found that the metamorphic quartz-dolomite diorite was formed in TTG magmatic arc tectonic environment during plate subduction; while metamorphic granite genesis may be related to the melting of thick crust metasedimentary rocks.

Key words: Yinshan block, granite-greenstone belt, metamorphic intrusive rocks, zircon U-Pb chronology, geochemistry

CLC Number: 

  • P588.12
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