I. A. Baksheev, Yu. V. Erokhin, I. A. Ekimenkova, A. V. Zakharov, V. V. Grigoriev, V. O. Yapaskurt, N. N. Koshlyakova
{"title":"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","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":"{\"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}","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}
Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia
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.
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.
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