Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (6): 1740-1753.doi: 10.13278/j.cnki.jjuese.201606112

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Chronology and Geochemical Characteristics of Zhuanshanzi Granite in Chifeng and Its Diagenetic Dynamics Background

Sun Zhenjun1, Sun Guosheng2, Yu Henan1, Xiang Zhu1, Tian Yi3, Liu Tong4, Chen Xu4, Li Yang4   

  1. 1. Department of Earthquake Science, Institute of Disaster Prevention Science and Technology, Beijing 101601, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China;
    3. Liaoning Survey Academy of Geology and Mineral Resources, shenyang 110031, China;
    4. 243 Team of Nuclear Industry, Chifeng 024006, Inner Mongolia, China
  • Received:2016-04-25 Online:2016-11-26 Published:2016-11-26
  • Supported by:
    Supported by Higher School Science and Technology Research Key Project in Hebei Province(ZD2015203) and Central University Basic Scientific Research Business Expenses Funded Project(ZD2015203)

Abstract: The Zhuanshanzi hornblende monzogranite is located in the the Mesozoic tectonic magmatic active belt which between the North China craton and the Xingmeng orogeny belt. Testing of major elements, rare-earth elements (REEs), trace elements and LA-ICP-MS zircon U-Pb dating of the hornblende monzogranite have be carried out to accurately determined the forming age and study the dynamics background of the granite,rock. Results show that the LA-ICP-MS zircon U-Pb age of the hornblende monzogranite is (245.8±3.1) Ma. (MSWD=3.7,n=17), and belongs to the Early Triassic. Geochemically, the granite is characterized by high concentrations of silica (w(SiO2)=71.68%-72.85%), alkali (w(Na2O+K2O)=8.98%-9.20%), and alumina (w (Al2O3)=13.45%-13.77%); low concentrations of calcium (w(CaO)=0.81%-0.99%); and with low values of TFeO/MgO (average is 6.55), indicating the hornblende monzogranite belongs to high-K, calc-alkaline high differentiation Ⅰ type, weak aluminum granite. The granite is enriched in LREE and relatively depleted in HREE(LaN/YbN=21.94-24.33), and obvious Eu anomaly (δEu=0.66-0.68), which indicates that a large number of the plagioclase fractionation occured during the magmatic processes. In addition, the granite is enriched in Th, U, La and P, and depleted in Ba, Nb, Ti, Sr and Ta, and so on. In summary, the Zhuanshanzi granite is mainly formed by partial melting of crust material, with a few new mantle source composition. It is formed under the extensional tectonic setting in post-collision or post-orogenic stage after the North China plate and Siberia plate's eventual collision.

Key words: granite, geochemistry, LA-ICP-MS zircon U-Pb dating, tectonic setting, Zhuanshanzi

CLC Number: 

  • P588.12
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