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小秦岭Q8号金矿床地质特征及深部资源潜力分析
引用本文:白和.小秦岭Q8号金矿床地质特征及深部资源潜力分析[J].陕西地质,2003,21(1):19-27.
作者姓名:白和
作者单位:中国地质大学资源学院,武汉,430074
摘    要:小秦岭金矿团田Q8号矿脉金矿床受地层、区域变质—混合岩化、岩浆活动及构造控制。矿区混合岩化强烈,岩浆活动频繁,构造复杂。矿脉规模大,赋存矿体数量多,是目前陕西小秦岭金矿田中延深深度最大、赋矿标高最低的金矿床。根据矿床地质特征分析,矿床仍有深延条件,其深部资源潜力较大。

关 键 词:金矿床  岩浆活动  矿床地质特征  构造控制  成矿作用  岩浆岩  断裂  褶皱
文章编号:1001-6996(2003)01-0019-09
修稿时间:2003年2月15日

GEOLOGY OF THE GOLD DEPOSIT Q8 AND THE DEEP-SEATED POTENTIAL MINERAL RESOURCES IN XIAOQINLING
Bai He.GEOLOGY OF THE GOLD DEPOSIT Q8 AND THE DEEP-SEATED POTENTIAL MINERAL RESOURCES IN XIAOQINLING[J].Geology of Shaanxi,2003,21(1):19-27.
Authors:Bai He
Abstract:The gold bearing veins in the gold deposit Q8 of the Xiaoqinling gold field are controlled by strata, regional metamorphism and migmatization, magmatic activities and structures. The mineralized area is characterized by extensive migmatization, frequently magmatic activities, complex structures, large scale gold bearing veins and a lot of occurrences of orebodies. The gold deposits in this area have the deepest extension and lowest elevation in the Xiaoqinling gold fields. According to the geological characteristics, the gold deposits are possible to extend deeper and have a great prospecting potential.
Keywords:Xiaoqinling  gold deposit  characteristics  resources potential
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