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KANG Congxuan, YANG Xianzhong, CAI Yitao, HUANG Xianjue, KONG Guanglin, LI Chaowei. 2019. Geological and geochemical characteristics of the Paleoproterozoic intrusions in Bengbu uplift, southeast North China Craton[J]. Geology in China, 46(6): 1481-1495. doi: 10.12029/gc20190615
Citation: KANG Congxuan, YANG Xianzhong, CAI Yitao, HUANG Xianjue, KONG Guanglin, LI Chaowei. 2019. Geological and geochemical characteristics of the Paleoproterozoic intrusions in Bengbu uplift, southeast North China Craton[J]. Geology in China, 46(6): 1481-1495. doi: 10.12029/gc20190615
shu

Geological and geochemical characteristics of the Paleoproterozoic intrusions in Bengbu uplift, southeast North China Craton

  • 1.

    Nanjing Center of Geological Survey, CGS, Nanjing 210016, Jiangsu, China

  • 2.

    School of Earth Sciences and Engineering, Hohai University, Nanjing 210016, Jiangsu, China

  • 3.

    No. 312 Geological Party, Bureau of Geology and Mineral Resources Exploration of Anhui Province, Bengbu 233040, Anhui, China

    • Fund Project: Supported by Anhui Public Welfare Geological Survey Fund (No. 2014-K-5)
More Information
  • Author Bio: KANG Congxuan, male, born in 1985, doctor candidate, mainly engages in the study of minerals, rocks, deposit geology and engineering geology; E-mail: kangcongxuan@sina.com
Received Date:  26 April 2018
Revised Date:  04 April 2019
Publish Date:  25 December 2019
    Abstract

  • North China landmass is the oldest landmass and one of the largest craton massifs in the world. Bengbu uplift is a part of the North China landmass, and its initial formation of continental crust is late Archean in the time limit. With the collisions and stitching of the Yangtze platform and North China continental block, the Bengbu uplift experienced complex evolution processes. In order to further explore the Paleoproterozoic magmatic activity in the Bengbu uplift, the authors updated the data of geochronologic and geochemical analysis. Based on field observation, geochronology and geochemistry of Paleoproterozoic intrusions in this area, the authors obtained zircon U-Pb ages of (2089±44)Ma and (2133±27)Ma for Zhuangzili and Muopanshan granites. The geochemical data show that granites have high-Na and low-K significantly, and belong to the quasi-aluminum supersaturated type. They are characterized by relative enrichment of LREE with a strong Eu negative anomaly and insignificant Ce anomaly. The elements of K, Nb, Sr, P and Ti are characterized by measurable depletion, and there exists relative enrichment of Rb, Th, U, Nd, Zr and Sm. Intrusion projection points are distributed in A type granite area in the discrimination diagram of genetic type. Nd twophase age (2.37-2.84 Ga) is consistent with the age of North China Craton formed in Archean, with 2.40-2.50 Ga being the main stage. εHf(t) values vary between -9.77 and +9.59, with obvious differences, suggesting the complexity of the origin of the material, and the old two-phase Hf model age (2.27-2.96 Ga) suggests that the main material was derived during Neoarchean. The tectonic environment belongs to the granite category within the plate and non-orogenic tectonic environment, which implies its extensional tectonic setting.

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