Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (1): 105-117.doi: 10.13278/j.cnki.jjuese.20170125

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Genesis and Material Source of Scheelite of Yangbishan Iron-Tungsten Deposit in Heilongjiang, NE China

Ma Yupeng1, Ren Yunsheng1,2, HaoYujie1,2, Lai Ke1, Zhao Hualei3, Liu Jun4   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources of China, Changchun 130061, China;
    3. Tianjin Center, China Geological Survey, Tianjin 300170, China;
    4. Heilongjiang Jianlong Iron and Steel Co., Ltd, Shuangyashan 155126, Heilongjiang, China
  • Received:2017-05-28 Online:2018-01-26 Published:2018-01-26
  • Supported by:
    Supported by National Key Research and Development Program of China (2017YFC0601304), National Basic Research Program ("973"Program) of China (2013CB429802) and National Natural Science Foundation of China (41272094)

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Abstract: The Yangbishan iron-tungsten deposit is located in Shuangyashan area of Heilongjiang Province, tectonically in the central of Jiamusi massif, the eastern Central Asian Orogenic Belt. The major ore-hosting strata in this area are the metamorphic rock series of Dapandao Formation in Xingdong Group. The layered iron orebodies are mainly hosted in the lowest rock section of Dapandao Formation. The lenticular and vein scheelite orebodies occur in the footwall of iron orebodies, and are controlled by the contact zone between the gneiss granite and the marble of Dapandao Formation. The ore-bearing rocks of tungsten mineralization in the Yangbishan deposit include garnet skarn and diopside skarn. The metallic minerals in the tungsten ore are mainly of scheelite and pyrrhotite, with a small amount of magnetite, pyrite, chalcopyrite, sphalerite, cassiterite, arsenopyrite and molybdenite. The δ18Oquartz value of scheelite-quartz veins in the Yangbishan deposit is 10.9 ‰-14.8 ‰, the δ18Owater value is 3.6 ‰-7.5 ‰, and the δD value is -120.9 ‰—-66.2 ‰, which show that the ore forming fluid of the scheelite mineralization is dominated by magmatic water. The δ34S value of metal sulfides in the skarn changes from 16.1 ‰ to 18.1 ‰, 206Pb/204Pb value from 17.879 to 18.863, 207Pb/204Pb value from 15.537 to 15.603, and 208Pb/204Pb value from 38.202 to 38.544. The data presented in this paper indicate that S and Pb in the metal sulfides mainly came from the ore-hosting strata and re-melted granitic magma. The geological characteristics of the tungsten mineralization in the Yangbishan deposit are similar to those of the skarn-type tungsten deposits. It can be concluded that the scheelite mineralization in the Yangbishan iron-tungsten deposit belongs to skarn-type deposits.

Key words: S-Pb isotope, fluid sources, genesis of the tungsten mineralization, Yangbishan iron-tungsten deposit, Jiamusi massif

CLC Number: 

  • P618.67
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