Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (6): 1746-1762.doi: 10.13278/j.cnki.jjuese.201706113

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Geochronology, Geochemistry and Formation of Xiaoyao Rock in Southern Anhui Province

Shi Ke1,2, Zhang Dayu1, Ding Ning2, Wang Deen3, Chen Xuefeng1   

  1. 1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China;
    2. Geological Survey of Anhui Province, Hefei 230001, China;
    3. No. 332 Geological Party, Bureau of Geology and Mineral Resources Exploration of Anhui Province, Huangshan 245000, Anhui, China
  • Received:2017-03-13 Online:2017-11-26 Published:2017-11-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41320104003) and Geological Survey Project of China Geological Survey (KJ2013-03) and Land and Resources Science and Technology Projects of Anhui Province (2015-K-5)

Abstract: The Xiaoyao granodiorite pluton intruded into Neoproterozoic Paleozoic marine sedimentary strata in Jixi County, south Anhui Province. The LA-ICP-MS zircon U-Pb isotopic data yield weighted mean ages of (149.3±2.3) and (148.6±1.9) Ma, indicating the magma was emplaced in Late Jurassic. After an electron microprobe (EPMA) analysis, the composition of representative silicate from Xiaoyao granodiorite intrusion shows that the biotite is Mg-biotite. The whole-rock chemical compositions suggest that Xiaoyao granodiorite intrusion is of I-type, belonging to high-kalium calcium alkaline series granitoid, and the characters of the trace elements show that the rocks are enriched in LREE, and depleted of HREE, indicating the lower crust sourced magma with some mantle materials added, which experienced strong fractional crystallization during its evolution. The Xiaoyao intrusion granodiorite pluton is characterized by that of volcanic-arc granite (VAG).

Key words: Geochronology, geochemistry, EMPA, Xiaoyao granodiorite pluton, south Anhui Province

CLC Number: 

  • P581
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