Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (4): 1059-1074.doi: 10.13278/j.cnki.jjuese.20180228

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LA-ICP-MS Zicon U-Pb Geochronology, Geochemistry and Geological Significance of Granodiorites in Lancai Area, Tongren, Qinghai

Ren Wenkai1,2, Wang Shengyun3, Chen Libiao1,2, Wu Shaofeng1,2, Zhang Haiqing1,2   

  1. 1. The Fourth Geological Exploration Institute of Qinghai Province, Xining 810029, China;
    2. Key Laboratory of Shale Gas Resources in Qinghai Province, Xining 810029, China;
    3. Beijing Research Institute of Uranium Geology, Beijing 100029, China
  • Received:2018-08-28 Published:2020-07-29
  • Supported by:
    Supported by Project of Centre for Hydrogeology and Environmental Geology Survey, China Geological Survey ([2016] 0703) and Project of China Geological Bureau of Nuclear Industry (201654)

Abstract: The geochemical characteristics and the LA-ICP-MS zircon U-Pb ages of the granodiorites in Lancai area, Tongren, Qinghai were studied,and the petrogenesis and tectonic significance were discussed. The results show that the crystallization age of Lancai granodiorite is (231.4±2.9) Ma (MSWD = 0.024). The ∑REE of the granitoide is 138.76×10-6-197.19×10-6. The REE patterns is rightward inclined with negative Eu anomaly. The trace element geochemistry is characterized evidently by the negative anomalies of Nb, Ta, Ti, Sr, Ba, P, etc. and positive anomalies of Rb, K, Th, U, etc. The granodiorites show the characteristics of metaluminous and belong to high-K calc-alkaline series. Lancai granodiorite is I-type granitoids. Based on the existing research results, Lancai granodiorite may be formed through partial melting of basic rocks in the crustal thickening geodynamic environment characterized mainly by compression on the whole and local shear extension,and the mantle-derived magmas may play an important role in the formation of the granodiorite.

Key words: granodiorites, geochemistry, zicon U-Pb dating, Lancai area, Qinghai

CLC Number: 

  • P588.12
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