Short wavelength infrared (SWIR) of white micas as a vectoring exploration tool for the Jiaojia gold deposit, Jiaodong Peninsula: implications for district- to deposit-scale gold exploration

IF 3.2 2区 地球科学 Q1 GEOLOGY
Hao Wang , Junling Zhang , Zhengjiang Ding , Qibin Zhang , Junfeng Zhao
{"title":"Short wavelength infrared (SWIR) of white micas as a vectoring exploration tool for the Jiaojia gold deposit, Jiaodong Peninsula: implications for district- to deposit-scale gold exploration","authors":"Hao Wang ,&nbsp;Junling Zhang ,&nbsp;Zhengjiang Ding ,&nbsp;Qibin Zhang ,&nbsp;Junfeng Zhao","doi":"10.1016/j.oregeorev.2025.106626","DOIUrl":null,"url":null,"abstract":"<div><div>The disseminated-style gold deposit, as the primary mining deposit-type in the Jiaodong Peninsula, has the current exploration depth exceeding 4000 m. These deposits/orebodies are primarily hosted within the Mesozoic granitic intrusions adjacent to the regional faults. The Jiaojia gold deposit, as the most famous disseminated-style gold deposit in Jiaodong, presents widely white micas alteration assemblages comprising distal potassic zone, intermediate sericitization, and proximal pyrite-muscovite-quartz zone. The mineral chemistry of white micas from three alteration zones was analyzed using short-wave infrared spectroscopy (SWIR) and electron microprobe analysis, along with an evaluation of the physicochemical conditions governing their formation. From distal to the proximal alteration zone, the K/(K + Na + Ca) ratio of muscovite decreases, while the Fe + Mg content first decreases and then slightly increases. This variation indicates that, from the distal to the proximal alteration zones, the temperature of the hydrothermal fluid progressively decreased, while the oxygen fugacity evolved from oxidizing to reducing and then to weakly oxidizing conditions. In each alteration zone, there is no linear correlation between the Pos2200 (the Al-OH absorption feature at 2200 nm) and its composition (e.g., Si, Al<sub>tot</sub>, Fe + Mg). Our thermodynamic simulations reveal that during each alteration stage, muscovite of different end-members can form, leading to the formation of mixed peaks in the Pos2200 region of the spectrum. In contrast, Illite crystallinity values (IC values), reflecting the crystallinity of the white mica, is controlled by fluid/rock ratio and can be used as vectors towards potential mineralization. Based on 3D mapping of IC values, the southwest part of Jiaojia gold deposit could represent the most potential mineralization location for deeper drilling. Integrating geological mapping and spectrum data, 180 ∼ 350 m proximal to potential ore bodies can be outlined using the criteria of IC values (IC &gt; 1.3), which could be predicted to gold endowment of disseminated deposits over the entire Jiaodong gold province, East China.</div></div>","PeriodicalId":19644,"journal":{"name":"Ore Geology Reviews","volume":"181 ","pages":"Article 106626"},"PeriodicalIF":3.2000,"publicationDate":"2025-04-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ore Geology Reviews","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0169136825001866","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

The disseminated-style gold deposit, as the primary mining deposit-type in the Jiaodong Peninsula, has the current exploration depth exceeding 4000 m. These deposits/orebodies are primarily hosted within the Mesozoic granitic intrusions adjacent to the regional faults. The Jiaojia gold deposit, as the most famous disseminated-style gold deposit in Jiaodong, presents widely white micas alteration assemblages comprising distal potassic zone, intermediate sericitization, and proximal pyrite-muscovite-quartz zone. The mineral chemistry of white micas from three alteration zones was analyzed using short-wave infrared spectroscopy (SWIR) and electron microprobe analysis, along with an evaluation of the physicochemical conditions governing their formation. From distal to the proximal alteration zone, the K/(K + Na + Ca) ratio of muscovite decreases, while the Fe + Mg content first decreases and then slightly increases. This variation indicates that, from the distal to the proximal alteration zones, the temperature of the hydrothermal fluid progressively decreased, while the oxygen fugacity evolved from oxidizing to reducing and then to weakly oxidizing conditions. In each alteration zone, there is no linear correlation between the Pos2200 (the Al-OH absorption feature at 2200 nm) and its composition (e.g., Si, Altot, Fe + Mg). Our thermodynamic simulations reveal that during each alteration stage, muscovite of different end-members can form, leading to the formation of mixed peaks in the Pos2200 region of the spectrum. In contrast, Illite crystallinity values (IC values), reflecting the crystallinity of the white mica, is controlled by fluid/rock ratio and can be used as vectors towards potential mineralization. Based on 3D mapping of IC values, the southwest part of Jiaojia gold deposit could represent the most potential mineralization location for deeper drilling. Integrating geological mapping and spectrum data, 180 ∼ 350 m proximal to potential ore bodies can be outlined using the criteria of IC values (IC > 1.3), which could be predicted to gold endowment of disseminated deposits over the entire Jiaodong gold province, East China.

Abstract Image

胶东半岛焦家金矿白云母短波红外矢量找矿方法及其对地—矿级金矿找矿的启示
浸染型金矿床是胶东半岛主要的金矿类型,目前勘探深度超过4000 m。这些矿床/矿体主要赋存于邻近区域断裂的中生代花岗质侵入体内。焦家金矿床是胶东最著名的浸染型金矿床,发育广泛的白色云母蚀变组合,包括远端钾化带、中端绢云母化带和近端黄铁矿-白云母-石英带。利用短波红外光谱(SWIR)和电子探针分析方法对3个蚀变带的白色云母进行了矿物化学分析,并对其形成的理化条件进行了评价。从远端到近端蚀变带,白云母的K/(K + Na + Ca)比值降低,Fe + Mg含量先降低后略有升高。这种变化表明,从远端到近端蚀变带,热液温度逐渐降低,氧逸度由氧化→还原→弱氧化。在各蚀变带中,Pos2200 (2200 nm处Al-OH的吸收特征)与其组成(如Si、Altot、Fe + Mg)之间不存在线性相关关系。热力学模拟结果表明,在每一个蚀变阶段,会形成不同端元的白云母,导致在光谱的Pos2200区域形成混合峰。伊利石结晶度值(IC值)反映了白云母的结晶度,受液岩比控制,可作为潜在成矿的指示载体。根据IC值的三维填图,焦家金矿西南段是最具深部钻探潜力的成矿位置。综合地质填图和频谱数据,利用IC值标准(IC >;1.3),可对整个胶东金省浸染状矿床的金禀赋进行预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Ore Geology Reviews
Ore Geology Reviews 地学-地质学
CiteScore
6.50
自引率
27.30%
发文量
546
审稿时长
22.9 weeks
期刊介绍: Ore Geology Reviews aims to familiarize all earth scientists with recent advances in a number of interconnected disciplines related to the study of, and search for, ore deposits. The reviews range from brief to longer contributions, but the journal preferentially publishes manuscripts that fill the niche between the commonly shorter journal articles and the comprehensive book coverages, and thus has a special appeal to many authors and readers.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信