Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (4): 1159-1171.doi: 10.13278/j.cnki.jjuese.201704114

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Geochemistry and Geological Significance of Granite Porphyry in Wudaoling, Heilongjiang Province

Xi Aihua1,2, Wang Mingzhi2, Ge Yuhui1, Li Bile2, Wang Quan3, Zhu Qian1   

  1. 1. School of Geoscience & Technology, Southwest Petroleum University, Chengdu 610500, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China;
    3. No.703 Team of Heilongjiang Geological Prospecting Bureau for Non-Ferrous Metals, Harbin 150300, China
  • Received:2016-10-15 Online:2017-07-26 Published:2017-07-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41272095)

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Abstract: Located in the southern end of Yichun-Yanshou metallogenic belt, Wudaoling molybdenum deposit is a typical skarn type deposit. Through researching on the granite porphyry on the edge of the host rocks, we found that the granite porphyry and ore-bearing syenogranite have not only the same formation age, but also the similar geochemical characteristics: the zircon U-Pb ages of the granite porphyry are 194.1±2.0 Ma, and the ore-bearing syenogranite ages are 193.9+1.3 Ma; the type of granite porphyry is transitional from I-type to A-type granites, and is more closer to A-type granites. The syenogranite typically belongs to A-type granites. Besides, both of the granites are high potassium calc-alkaline-weak-alkaline and metaluminous-peraluminous granites with enrichment in Si, K-Na and Al. The granites are enriched in LILE (Rb, K) and light rare earth elements, depleted of HFSE (Nb, Ta, P, Ti). The microelements follow the same trends as that of the rare earth elements, showing that they might be comagmatic products. The initial Sr isotope ratio 87Sr/86Sr of granite porphyry is 0.723 123. Combining with the regional geological evolution characteristics, the authors suggest that the formation of Wudaoling granitic complex was related to the extended environment after the subduction of the Ancient Pacific plate;and the mineralization of skarn type molybdenum deposit may closely relate to the granite porphyry intrusion. Regionally, it implies a mineralization possibility of the granite porphyry in this phase.

Key words: Wudaoling granite, zircon U-Pb dating, A-type granites, geochemistry, Yichun-Yanshou metallogenic belt, Heilongjiang Province

CLC Number: 

  • P588.12
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