Mineralization Ages of Some Epithermal Gold-Silver Vein-type Deposits in the Central Kitami Mining District of the Kitami Metallogenic Province, Hokkaido, Japan

H. Maeda
{"title":"Mineralization Ages of Some Epithermal Gold-Silver Vein-type Deposits in the Central Kitami Mining District of the Kitami Metallogenic Province, Hokkaido, Japan","authors":"H. Maeda","doi":"10.11456/SHIGENCHISHITSU1951.40.17","DOIUrl":null,"url":null,"abstract":"The mineralization ages of some epithermal gold-silver vein-type deposits in the Kitami metallogenic province, Hokkaido, Japan have been studied based on the K-Ar dating on the vein adularia and quartz mixtures. The Kohnomai mineralization took place in Middle Miocene time (12.9•}0.4 Ma). On the other hand, the gold-silver mineralization in the Ikutahara-Rubeshibe area occurred in Late Miocene to Early Pliocene time (Ryuo mine: 7.7•}0.2 Ma; Shakinzawa mine: 7.4•}0.2 Ma; Muka mine: 6.6•}0.2 Ma; Saroma mine: 5.3•}0.5 Ma).","PeriodicalId":383641,"journal":{"name":"Mining geology","volume":"38 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1990-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"16","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mining geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.11456/SHIGENCHISHITSU1951.40.17","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 16

Abstract

The mineralization ages of some epithermal gold-silver vein-type deposits in the Kitami metallogenic province, Hokkaido, Japan have been studied based on the K-Ar dating on the vein adularia and quartz mixtures. The Kohnomai mineralization took place in Middle Miocene time (12.9•}0.4 Ma). On the other hand, the gold-silver mineralization in the Ikutahara-Rubeshibe area occurred in Late Miocene to Early Pliocene time (Ryuo mine: 7.7•}0.2 Ma; Shakinzawa mine: 7.4•}0.2 Ma; Muka mine: 6.6•}0.2 Ma; Saroma mine: 5.3•}0.5 Ma).
日本北海道北上成矿省北上矿区中部一些浅成热液型金银脉型矿床的成矿时代
利用岩脉与石英混合物的K-Ar测年方法,研究了日本北海道北上成矿省部分浅成热液型金银脉型矿床的成矿年龄。Kohnomai矿化发生在中中新世(12.9•}0.4 Ma)。另一方面,Ikutahara-Rubeshibe地区的金银成矿发生在晚中新世至上新世早期(Ryuo矿:7.7•}0.2 Ma;上津泽矿:7.4•}0.2 Ma;木卡矿:6.6•0.2 Ma;Saroma矿:5.3•0.5 Ma)。
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
自引率
0.00%
发文量
0
×
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