Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (2): 389-403.doi: 10.13278/j.cnki.jjuese.201502105

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Chronology,Geochemistry and Petrogenesis of the Volcanic Rocks in Manitu Formation in Chaihe Area, Central Great Xing'an Range

Si Qiuliang1,2, Cui Tianri2, Tang Zhen2,3, Li Wei2, Wu Xinwei2,3, Jiang Bin2,3, Li Linchuan2,3   

  1. 1. College of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China;
    2. Shenyang Institute of Geology and Mineral Resources/Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China;
    3. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2014-07-16 Published:2015-03-26

Abstract:

The zircon LA-ICP-MS U-Pb dating and geochemistry are reported for the volcanic rocks in Manitu Formation in Chaihe, central Great Xing'an Range in order to discover its formation time, petrogenesis and the regional tectonic setting Petrographically.The volcanic rocks in Manitu Formation are composed of andesite and dacite,but they are trachyte, trachydacite, and dacite based on its chemical composition. Zircon from these volcanic rocks are euhedral-subhedral in shape, with fine-scale oscillatory growing ring. The Th/U ratio of (0.33-2.08) indicates a magmatic origin. The dating results show that the volcanic rocks in Manitu Formation are formed in Late Jurassic from 139 to 148 Ma. The geochemical study shows that the SiO2 of the andesite is between 64.87%-68.65%,Al2O3 is between 15.53%-16.72%,Na2O+K2O is between 6.75%-9.22%,K2O/Na2O is between 0.63-1.57, falling in the series of high-potassium calc-alkaline. All samples have a similar REE pattern with a significant fractionation of LREE from HREE((La/Yb)N =11.50-14.88)and negative Eu anomalies(δEu=0.45-1.17). The total rare earth element is from 124.95×10-6 to 208.57×10-6. The trace element geochemistry is characterized evidently by enrichment of Rb, Ba, K, depletion of Nb, P, Ti. Its original magma is derived from the partial melting of the crust,during an extension after the closure of the Mongol-Okhotsk Ocean.

Key words: LA-ICP-MS zircon U-Pb dating, geochemistry, volcanic rocks, Manitu Formation, Chaihe area, Central Great Xing'an Range

CLC Number: 

  • P588.141

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