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胶东三山岛断裂带金矿床蚀变矿物勘查标识

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三山岛断裂带蚀变岩型金矿床控矿断裂产状变化部位含矿性存在差异,使得矿体不连续,勘查标识不明确.通过对三山岛北部海域金矿床30号勘探线的多个钻孔和三山岛井下坑道进行系统编录和样品采集,研究矿物共生组合与矿脉之间的穿切关系.研究表明:北部海域金矿床可划分为4个成矿阶段,即石英—黄铁矿—钾长石阶段(Ⅰ)、石英—黄铁矿—黄铜矿—自然金阶段(Ⅱ)、石英—黄铁矿—方铅矿—闪锌矿—自然金阶段(Ⅲ)和贫矿菱铁矿—方解石阶段(Ⅳ),其中Ⅱ和Ⅲ阶段是金的主要成矿阶段.利用短波红外光谱对控矿断裂含矿和贫矿部位样品进行分析,发现蚀变矿物组成、Al-OH吸收峰位和结晶度(IC)等存在明显差异,高的Pos2200和IC值与金矿体之间存在明确的正相关关系.对各钻孔的品位数据进行统计分析后,引入机器学习算法进行分析,强调IC值具有更高的权重影响.黄铁矿微量元素研究显示:As、Pb、Bi、Te和Sb等元素与Au元素含量之间具有显著正相关性.由此,基于断裂产状、短波红外光谱指标和黄铁矿元素含量等变化情况,建立了全新的勘查标识,对实际找矿勘查工作具有指导意义.
Exploration Indicators of Altered Minerals of Gold Deposits in the Sanshandao Fault Zone,Jiaodong Peninsula
The Jiaodong Peninsula represents the largest gold orefield in China and ranks as the third largest globally,with orebodies predominantly controlled by fault structures.The mineralization of gold deposits within the Sanshandao fault zone exhibits variability attributable to alterations in the controlling fault structures,leading to disparities in ore body continuity and ambiguous exploration indicators.This study systematically cataloged and sampled multiple drill holes and underground tunnels along exploration line 30 in the Beibuhaiyu and Sanshandao gold deposits.Based on the paragenetic associations of minerals and the cross-cutting relationships among ore veins,the gold deposits in the northern sea area can be categorized into four distinct metallogenic stages:quartz-pyrite-potassium feldspar(stage Ⅰ),quartz-pyrite-chalcopyrite-native gold(stage Ⅱ),quartz-pyrite-galena-sphalerite-native gold(stage Ⅲ),and barren siderite-calcite(stage Ⅳ).Notably,stage Ⅱand stage Ⅲ represent the primary metallogenic phases for native gold.The analysis of ore-bearing and barren sections of controlling faults through shortwave infrared spectroscopy has demonstrated substantial differences in alteration mineral composition,Al-OH absorption peak positions,and crystallinity index(IC).Notably,elevated Pos2200 and IC values exhibit a strong positive correlation with gold mineralization.Furthermore,statistical evaluation of grade data from multiple drill holes,augmented by machine learning algorithms,underscores the significant influence of IC values.The analysis of trace elements in pyrite revealed substantial positive correlations among elements including arsenic(As),lead(Pb),bismuth(Bi),tellurium(Te),antimony(Sb),and,gold(Au).Consequently,this study has established a novel exploration indicator grounded in variations in fault attitude,shortwave infrared spectroscopy markers,and pyrite elemental,commposition.This indicator holds considerable significance for informing practical prospecting efforts.

shortwave infrared spectroscopy analysisexploration identificationfault-controlled mineralization modelSanshandao faultJiaodong Peninsula

李健、宋明春、王昌伟、王润生、雷鸣、崔庆意、李杰、李世勇

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山东理工大学资源与环境工程学院,山东 淄博 255000

河北省战略性关键矿产资源重点实验室,河北地质大学地球科学学院,河北 石家庄 050031

山东省正元地质资源勘查有限责任公司,山东 淄博 255000

山东省物化探勘查院,山东 济南 250013

山东省核工业二七三地质大队,山东 烟台 264000

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短波红外光谱分析 勘查标识 断裂控矿模式 三山岛断裂 胶东半岛

国家自然科学基金NSFC-山东省联合基金项目山东省自然科学基金项目河北省人才项目

U2006201ZR2021QD056HBQZYCXY0010

2024

黄金科学技术
中国科学院资源环境科学信息中心

黄金科学技术

CSTPCD北大核心
影响因子:0.651
ISSN:1005-2518
年,卷(期):2024.32(5)