豫西申家窑—葫芦峪金银多金属矿深部成矿条件与成矿规律  

Deep Metallogenic Conditions and Metallogenic Regularity of Shenjiayao—Huluyu Au-Ag Polymetallic Deposit in Western Henan

作　　者：赵彦巧 王春永 郭凯旋 白英建 胡利芳 张进宇 ZHAO Yanqiao;WANG Chunyong;GUO Kaixuan;BAI Yingjian;HU Lifang;ZHANG Jinyu(No.1 Geological Brigade,Henan Bureau of Nonferrous Metals Geology and Mineral Resources,Zhengzhou 450016,Henan,China;Nonferrous Metal Mineral Exploration Engineering Technology Research Center of Henan Province,Zhengzhou 450016,Henan,China)

机构地区：[1]河南省有色金属地质矿产局第一地质大队,河南郑州450016 [2]河南省有色金属矿产探测工程技术研究中心,河南郑州450016

出　　处：《中国钼业》2022年第6期14-19,共6页China Molybdenum Industry

基　　金：河南省财政地质勘查项目(任务书编号:豫国土资发[2013]7号、豫国土资发〔2015〕97号、豫国土资发[2018]22号)。

摘　　要：根据近年来的地质勘查资料,通过对豫西申家窑—葫芦峪金银多金属矿床成矿地质条件与富集规律进行综合分析,认为金银多金属矿(化)体主要赋存在太古界太华岩群兰树沟岩组与NNW向、近SN向断裂破碎带复合部位,受地层、断裂破碎带控制;区内成矿地质条件有利,控岩、控矿条件明显,本区具备寻找大型构造破碎蚀变岩型矿床的远景和潜力。Based on the geological exploration data in recent years, through the comprehensive analysis of the metallogenic geological conditions and enrichment law of Shenjiayao-Huluyu Au-Ag polymetallic deposit in western Henan, it is considered that the Au-Ag polymetallic ore(mineralization) body is mainly located in the composite part of Lanshugou formation of Archean Taihua rock group and NNW direction and near SN direction fault fracture zone, which is controlled by stratum and fault fracture zone;The metallogenic geological conditions in the area are favorable, and the rock and ore control conditions are obvious.This area has the prospect and potential to find large-scale structural broken altered rock deposits.

关 键 词：成矿规律 成矿地质条件 金银多金属矿 申家窑—葫芦峪 

分 类 号：P618.51[天文地球—矿床学]