Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia

IF 0.3 Q4 GEOLOGY
I. A. Baksheev, Yu. V. Erokhin, I. A. Ekimenkova, A. V. Zakharov, V. V. Grigoriev, V. O. Yapaskurt, N. N. Koshlyakova
{"title":"Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia","authors":"I. A. Baksheev, Yu. V. Erokhin, I. A. Ekimenkova, A. V. Zakharov, V. V. Grigoriev, V. O. Yapaskurt, N. N. Koshlyakova","doi":"10.3103/s0145875223040038","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>Tourmaline, rutile, and associated minerals from veinlets cutting chromitites are characteristic of the Kamennoozerskoe occurrence belonging to the Shabrovskii district in the Central Urals. Tourmaline belongs to the dravite–oxy-dravite series and contains Cr (0.52–2.06 apfu), Ni (up to 0.03 apfu), and V (up to 0.02 apfu). Raman spectroscopy indicates Fe<sup>3+</sup> in tourmaline. Rutile associated with tourmaline contains, wt %: Sb<sub>2</sub>O<sub>5</sub> 4.68–11.69, Cr<sub>2</sub>O<sub>3</sub> 2.00–8.02, and WO<sub>3</sub> 0.88–1.14. It is suggested that tourmaline and associated minerals were formed under oxidizing conditions.</p>","PeriodicalId":44391,"journal":{"name":"Moscow University Geology Bulletin","volume":"24 1","pages":""},"PeriodicalIF":0.3000,"publicationDate":"2023-11-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Moscow University Geology Bulletin","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3103/s0145875223040038","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

Tourmaline, rutile, and associated minerals from veinlets cutting chromitites are characteristic of the Kamennoozerskoe occurrence belonging to the Shabrovskii district in the Central Urals. Tourmaline belongs to the dravite–oxy-dravite series and contains Cr (0.52–2.06 apfu), Ni (up to 0.03 apfu), and V (up to 0.02 apfu). Raman spectroscopy indicates Fe3+ in tourmaline. Rutile associated with tourmaline contains, wt %: Sb2O5 4.68–11.69, Cr2O3 2.00–8.02, and WO3 0.88–1.14. It is suggested that tourmaline and associated minerals were formed under oxidizing conditions.

Abstract Image

俄罗斯中乌拉尔地区Kamennoozerskoe铬铁矿产状的铬碧玺和含cr - sb - w金红石
摘要:乌拉尔中部沙布罗夫斯基地区的卡门努泽尔斯科产状脉状切割铬铁矿中的ourmaline、金红石及其伴生矿物具有一定的特征。电气石属钛氧钛钛系列,含Cr (0.52 ~ 2.06 apfu)、Ni (0.03 apfu)和V (0.02 apfu)。拉曼光谱分析表明电气石中含有Fe3+。金红石与电气石伴生物的wt %分别为:Sb2O5 4.68 ~ 11.69, Cr2O3 2.00 ~ 8.02, WO3 0.88 ~ 1.14。认为电气石及其伴生矿物是在氧化条件下形成的。
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
CiteScore
0.60
自引率
25.00%
发文量
43
期刊介绍: Moscow University Geology Bulletin  is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.
×
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