ZHANG Jiong-fei, QUAN Heng, ZHU Hong-chen. GEOLOGICAL CHARACTERISTICS OF XIAOYINUOGAIGOU GOLD DEPOSIT IN INNER MONGOLIA[J]. Geology and Resources, 1999, 8(3): 129-135. DOI: 10.13686/j.cnki.dzyzy.1999.03.001
    Citation: ZHANG Jiong-fei, QUAN Heng, ZHU Hong-chen. GEOLOGICAL CHARACTERISTICS OF XIAOYINUOGAIGOU GOLD DEPOSIT IN INNER MONGOLIA[J]. Geology and Resources, 1999, 8(3): 129-135. DOI: 10.13686/j.cnki.dzyzy.1999.03.001

    GEOLOGICAL CHARACTERISTICS OF XIAOYINUOGAIGOU GOLD DEPOSIT IN INNER MONGOLIA

    • The authors discovered the Xiaoyinuogaigou granite-porphyry in the southern margin of the Ergun block,where the Xiaoyinuogaigou gold deposit is located. The research confirms that:1)the Xiaoyinuogaigou granite-porphyry was formed in middle Jurassic;2)the ore-bearing rock and the host rock of the Xiaoyinuogaigou gold deposit are the Xiaoyinuogaigou granite-porphyry;3)the Xiaoyinuogaigou gold deposit is a mesothermal deposit;and 4)the Ergun ductile shear zone is the passageway for the Xiaoyinuogaigou granite-porphyry,and the secondary fracture of the Ergun ductile shear zone is the host structure of the Xiaoyinuogaigou gold deposit.
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