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河南省淅川县金家垭锑矿床地质特征及找矿前景
引用本文:吉恒召,陈金铎,张恺,李娇艳,李玉辉,闫贺龙.河南省淅川县金家垭锑矿床地质特征及找矿前景[J].金属矿山,2018,47(12):127-133.
作者姓名:吉恒召  陈金铎  张恺  李娇艳  李玉辉  闫贺龙
作者单位:1.河南省地质矿产勘查开发局第一地质勘查院,河南 郑州 450001;2.河南省地质矿产勘查开发局第二地质勘查院,河南 郑州 450000
基金项目:基金项目:中国地质调查局地质调查项目(编号:0499141055)。
摘    要:金家垭锑矿床位于豫陕交界的南秦岭造山带东段淅川断裂多金属成矿带上,成矿条件较好。为深入探讨矿区找矿潜力,分别采用1∶50 000水系沉积物测量、1∶10 000地质草测、1∶2 000岩石剖面测量和槽探工程控制等方法在矿区开展了地质勘查及研究工作,并对矿区地质特征、控矿因素、找矿标志及找矿前景进行了详细探讨。研究表明:①矿体主要赋存于寒武系水沟口组底部一套黑色硅质岩及土黄色黏土岩部位;②韧性-韧脆性构造是控矿和储矿的有利空间,使地层中的成矿元素发生活化迁移,随着物理化学条件改变,锑及其他有用元素在有利部位发生沉积富集,从而形成锑矿床;③采用1∶50 000 水系沉积物测量→1:10 000 地质草测→1∶2 000 岩石测量→槽探揭露方法的找矿效果明显。在上述分析的基础上,圈定了2处找矿靶区,并在靶区内发现了锑矿体,表明靶区内找矿前景较好,值得进一步开展工作。

关 键 词:锑矿  淅川断裂  地质特征  控矿因素  找矿前景  

Geological Characteristics and Prospecting Prospective of Jinjiaya Antimony Deposit in Xichuan County, Henan Province
Ji Hengzhao,Chen Jinduo,Zhang Kai,Li Jiaoyan,Li Yuhui,Yan Helong.Geological Characteristics and Prospecting Prospective of Jinjiaya Antimony Deposit in Xichuan County, Henan Province[J].Metal Mine,2018,47(12):127-133.
Authors:Ji Hengzhao  Chen Jinduo  Zhang Kai  Li Jiaoyan  Li Yuhui  Yan Helong
Affiliation:1. The First Geological Exploration Institute of Henan Geology and Mineral Exploration and Development Bureau, Zhengzhou 450001,China; 2.The Second Geological Exploration Institute of Henan Geological and Mineral Exploration and Development Bureau,Zhengzhou 450000,China
Abstract:Jinjiaya Antimony Deposit is located at Xichuan fault polymetallic metallogenic belt in the eastern part of the Southern Qinling Mountains Orogenic Belt at the junction of Henan Province and Shaanxi Province,the metallogenic conditions of the mining area is good.In order to study the prospecting potential of the area,geological prospecting and study have been carried out in the mining area by means of 1∶50 000 stream sediment survey, 1∶10 000 geological sketch survey,1∶2 000 rock profile survey and trench prospecting engineering control,besides that,geological characteristics,ore-controlling factors,prospecting indicators and prospecting prospective of the mining area are discussed in detail.The study results show that:①the orebodies are mainly hosted in a set of black siliceous rocks and yellowish clay rocks at the bottom of Shuigoukou Formation of Cambrian System;②the ductile-brittle structure is a favorable space for ore-controlling and storage,which activates and migrates the ore-forming elements in the stratum,with the change of physical and chemical conditions,antimony and other useful elements are deposited and enriched at favorable areas,therefore,the antimony deposit is formed;③the method of 1∶50 000 stream sediment survey,1∶10 000 geological survey,1∶2 000 rock survey and trench exploration and exposure has obvious prospecting effect.Based on the above discussion results,two prospecting targets areas are delineated and antimony orebodies are found in the target areas,which indicates that the prospecting prospective of the target areas is good and they are worth conducting further prospecting work.
Keywords:Antimony deposit  Xichuan fault  Geological characteristics  Ore-controlling  Prospecting prospective
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