文章摘要
陈书中,李军亭,牛昱博.豫西小池沟金矿矿床地质特征研究[J].矿产勘查,2021,12(5):1168-1175
豫西小池沟金矿矿床地质特征研究
Geological characteristics of Xiaochigou gold deposit in western Henan
投稿时间:2020-09-03  
DOI:
中文关键词: 小池沟  金矿  矿床地质特征  矿床成因  控制因素
英文关键词: Xiaochigou  gold deposit  geological characteristics of the deposit  metallogeny  control factors
基金项目:
作者单位
陈书中 河南省有色金属矿产探测工程技术研究中心河南郑州 450016
河南省有色金属地质矿产局第六地质大队河南郑州 450016 
李军亭 河南省有色金属地质矿产局第六地质大队河南郑州 450016 
牛昱博 河南省有色金属地质矿产局第六地质大队河南郑州 450016 
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中文摘要:
      豫西洛宁县小池沟金矿资源丰富。本文在研究区前人区域地质、矿产地质工作的基础上,开展野外地质调查并采集样品测试分析,进行矿体特征、矿石质量、矿石结构与构造、金矿化特征、围岩蚀变和成矿阶段等研究,分析矿床主控因素和找矿标志,探讨矿床成因。研究结果表明:金矿区圈定 6个矿体,各构造蚀变带控制的金矿体沿矿体走向呈串珠状产出,矿石中金的含量和黄铁矿与方铅矿均具正相关关系,矿石矿物共生组合主要有 4种类型。小池沟金矿区脉状金矿体主要以构造蚀变岩型为主,围岩主要蚀变类型有硅化、钾化、黄铁矿化、绿泥石化、绿帘石化。成矿过程大致分为 3个阶段:南北向挤压下的Ⅰ期矿化、张(扭)性背景下的Ⅱ期矿化和地壳持续抬升背景下大气降水循环作用的Ⅲ期矿化蚀变。控矿主要因素为构造、基底岩系和燕山期花岗岩,矿床成因类型为中低温热液型金矿床。
英文摘要:
      Xiaochigou deposit is rich of gold resources in Luoning County,west of Henan Province Based on the previous regional geological and mineral geological work, eld geological survey and samples test and analysis were carried out in this paper,the orebody characteristics,ore quality and ore structure and texture,gold mineralization features,wall-rock alteration and mineralization stages were also studied,in order to analyze the main controlling factors and prospecting marks of the deposits The results show that there are six ore bodies delineated in this area The gold ore bodies controlled by various structural alteration zones occur as beads along the strike There is a positive correlation between gold and pyrite and galena in the ore There are four types of ore mineral association The vein-like gold ore bodies in Xiaochigou gold deposit are mainly tectonic alteration rock type The main alteration type of surrounding rock is silicification,potassium,pyritization, chloritization and epidotization The mineralization process can be divided into three stages,the rst stage of mineralization happened under north-south compression,the second stage mineralization took place in the background of tension (torsion),and the third stage mineralization alteration caused by atmospheric precipitation cycle under the background of continuous crustal uplift The main ore controlling factors are structures,basement rock series and Yanshanian granites The genetic type of the deposit is medium-low temperature hydrothermal gold deposit
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