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CHEN Peijia, DAI Chaocheng, HUANG Cheng, WANG Xinliang. 2017. Geochemical characteristics and zircon U-Pb age of the Paleoproterozic S-type granite in Wulashan region and its geological significance[J]. Geology in China, 44(5): 959-973. doi: 10.12029/gc20170509
Citation: CHEN Peijia, DAI Chaocheng, HUANG Cheng, WANG Xinliang. 2017. Geochemical characteristics and zircon U-Pb age of the Paleoproterozic S-type granite in Wulashan region and its geological significance[J]. Geology in China, 44(5): 959-973. doi: 10.12029/gc20170509
shu

Geochemical characteristics and zircon U-Pb age of the Paleoproterozic S-type granite in Wulashan region and its geological significance

  • 1.

    College of Geosciences, East China Institute of Technology, Nanchang, 330013, Jiangxi, China

  • 2.

    Geology and Mineral Exploration Institute of Inner Mongolia, Hohhot 010000, Inner Mongolia, China

    • Fund Project: Supported by East China University of Technology Postgraduate Innovation Fund (No.YC2017-S277), National Youth Science Foundation Project (No.41402085) and the Ministry of Land and Resources, Geological and Mineral Survey Project for Southern Section of Da Hinggan Mountains Metallogenic Belt (No.1212011120718)
More Information
  • Author Bio: CHEN Peijia, male, born in 1993, master candidate, engages in the study of petrology; E-mail:a5733327@live.com
  • Corresponding author: DAI Chaocheng, male, born in 1980, lecturer, doctor, engages in the study of stratigraphy; E-mail:daichaocheng@qq.com 
Received Date:  09 October 2016
Revised Date:  19 October 2017
Publish Date:  25 October 2017
    Abstract

  • Wulashan area, located in the north part of the North China craton, has well-developed Paleoproterozoic granites, with the Nuoeryin S-type granites as the typical one. The investigation of Nuoeryin granites shows that the granites have high SiO2 (w(SiO2)=70.03%~75.43%), high Al2O3 (w(Al2O3)=13.04%~14.87%), and high K2O values (w(K2O)=5.36%~6.58%), low Mg# (< 10) and high A/CNK values, indicating that they belong to peraluminous S-type granites. They are enriched in LREE with significant differentiation between LREE and HREE (LaN/YbN=22.3-300.5), and REE patterns of the samples are of right-oblique type, with strong negative Eu anomalies(δEu=0.16-0.55). The primitive mantle-normalized trace element diagrams show enrichment of K, Rb, Th, Pb and depletion of Sr, Ba, Nb, Ta, P, Ti. The Nuoeryin granites have similar geochemical characteristics to the Paleoproterozic knondalites in Wulashan area and, and the reason is probably that Nuoeryin granites were generated by the knondalites anatexis while the Yinshan blocks and Ordos blocks experienced collision in Paleoproterzoic. The LA-ICP-MS zircon U-Pb ages of Nuoeryin granites are 1891±14 Ma and 1863±17 Ma, which represent the crystallization age of the Nuoeryin S-type granites, and the age is also contemporaneous with magmatic-metamorphic events in Khondalite belt.

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