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J4 ›› 2011, Vol. 19 ›› Issue (6): 36-39.
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QIU Cong,LI Chunzhi,WANG Shunde,YANG Jinsheng
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Abstract:
We describe the geology in the Bieluagaxi gold deposit,through analyzing the formation,structure,characteristics of igneous rocks and the space-time relations of dykes and veins,we discuss the causes of Bieluagaxi gold deposit,and think that it’s belongs to high-temperature multi-source hydrothermal quartz vein and altered rock broken genetic types.Characteristics of inclusions and sulfur isotopes show that Bieluagaxi gold deposit was formed in the late Variscan and closely related to magmatic activities.Metallogenic material mainly come from post-magmatic hydrothermal ore,and sulfur in the ore may be from magmatic-hydrothermal and sedimentary strata.Because of the closely space-time relationship between the veins and diorite,we suggest that the mineralization regularity of Bieluagaxi gold deposits is“construction diorite dyke”,and a large-scale ore body in deep is existent or not still need to be check by the exploration and research in the further.
Key words: Metallogenic regularity, Dikes, Veins, Bieluagaxi gold deposit, Xinjiang Province
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QIU Cong,LI Chunzhi,WANG Shunde,YANG Jinsheng. Temporal-spatial Relations between Gangue Rock and Vein of Bieluagaxi Gold Deposit,Xinjiang Province[J].J4, 2011, 19(6): 36-39.
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URL: http://www.goldsci.ac.cn/EN/
http://www.goldsci.ac.cn/EN/Y2011/V19/I6/36
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