| 前河金矿田葚沟矿区构造特征及找矿方向 |
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| 引用本文： | 姚松明,韩光照,王中义,盛利涛,齐康.前河金矿田葚沟矿区构造特征及找矿方向[J].矿产与地质,2013(5):377-380. |
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| 作者姓名： | 姚松明 韩光照 王中义 盛利涛 齐康 |
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| 作者单位： | 嵩县前河矿业有限责任公司,河南 洛阳471433 |
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| 摘 要： | 葚沟矿区位于前河金矿田中心部位，是豫西地区近年发现的规模达大型的构造蚀变岩型金矿床。F4矿体为该矿床主要矿体，除 F4外矿区还有 F22、F18这两条断裂。近年地质人员对 F22与 F4关系提出了不同观点。本文通过对Ⅳ号矿带、F22构造特征研究，理清了它们之间的相互关系，总结出区内断裂的生成顺序为 F4-F22-F4。同时指出了矿区的探矿方向，对指导该区找矿及生产有一定意义。
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| 关 键 词： | 金矿床 F4 F22 断裂构造特征 找矿方向 豫西地区 葚沟 |
Tectonic characteristics of Shengou mining area of Qianhe Au ore field and its prospecting direction |
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| YAO Song-ming,HAN Guang-zhao,WANG Zhong-yi,SHENG Li-tao,QI Kang.Tectonic characteristics of Shengou mining area of Qianhe Au ore field and its prospecting direction[J].Mineral Resources and Geology,2013(5):377-380. |
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| Authors: | YAO Song-ming HAN Guang-zhao WANG Zhong-yi SHENG Li-tao QI Kang |
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| Institution: | (Songxian Qianhe Mining Co., Ltd., Luoyang 471433, Henan, China) |
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| Abstract: | Shengou mining area is located at the center of Qianhe Au ore field,and it is a large scaled structure altered rock type Au deposit which was found in recent years in west Henan.Ore-body F4 is the major ore-body in the deposit,and F22 and F18 are also the two faults in the mining area.Different viewpoints about the relationship between F22 and F4 are put forward by geologists.Through researching on tectonic characteris-tics of No.IV ore belt and F22 and sorting out the relationship between them,it is concluded that the occur-rence sequence of faults in the area is F4-F22-F4 .This paper also points out the prospecting direction,which has certain meaning in prospecting and production in this area. |
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| Keywords: | F4 F22 tectonic characteristics prospecting direction |
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