刘沈衡.南京栖霞山铅锌多金属矿床重磁异常及矿床成因解释[J].地质找矿论丛,1991,(1):76-84
南京栖霞山铅锌多金属矿床重磁异常及矿床成因解释
INTERPRETATION OF GRAVITY AND MAGNETIC CHARACTERISTICS OF THE QIXIASHAN Pb—Zn POLY METAL DEPOSIT, NANJING AND DISCUSSION ON ITS GENESIS
  
DOI:10.6053/j.issn.1001-1412.1991.1. 008
中文关键词:  隐伏岩体  层控矿床  区域构造  成因过程立体模型
英文关键词:
基金项目:
作者单位
刘沈衡 华东有色地质勘查局814队 
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中文摘要:
      南京栖霞山铅锌多金属矿床重磁异常的性质,推断该矿床深部存在稳伏岩体。依据该结论并结合栖霞山铅锌多金属矿床的地质特征分析了栖霞山铅锌多金属矿床的成因机制,指出该矿床是以岩浆热液为主的复成层控矿床。给出了该矿床由莫霍面至地面范围的区域构造和成因过程立体模型。
英文摘要:
      This paper presents interpretation of gravity and magnetic anomaly and the geological characteristics of Qixiashan Pb-Zn ploymetal deposit on which metallogenic mechanism and the stereo-structural model from Moho interface to the surface of the deposit are proposed. It is a complex deposit dominated by magma hydroahermal fluid.
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