Abstract：Maoling gold deposit occuring in aarly Proterozoic metamorphic rocks is near Maoling granite body, which is Mesozolc in age (K-Ar age:207.8Ma). The distance that the gold deposit is apart from granite body is only 0.2km. and but Maoling granite itself is altered and mineralized. The host rocks of Maoling gold deposit are sericite phyllite and quartz sericite phyllite. The si-lification and sericitization are the chief alteration of the host rock. The or-ebodies consist of the gold-bearing quartz veinlets and the phyllite which was silicified and sericitized. The ore boundary is defined by chemical analysis.
引用本文:
余昌涛, 贾斌, 刘斌. 辽宁省盖县猫岭金矿床地质特征及成因探讨[J]. 地质与资源, 1992, 1(1): 38-47.
Yu Changtao, Jia Bin, Liu Bin. GEOLOGICAL CHARACTERISTIC AND GENESIS OF MAOLING GOLD DEPOSIT SN LIAONING PROVINCE. GEOLOGY AND RESOURCES, 1992, 1(1): 38-47.
1992, Vol. 1 
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