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。
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.
出处
《地质找矿论丛》
CAS
CSCD
1991年第1期76-84,共9页
Contributions to Geology and Mineral Resources Research
