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Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia
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),...
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| Published in: | Moscow University geology bulletin 2023-08, Vol.78 (4), p.504-519 |
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| Main Authors: | , , , , , , |
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| container_end_page | 519 |
| container_issue | 4 |
| container_start_page | 504 |
| container_title | Moscow University geology bulletin |
| container_volume | 78 |
| creator | Baksheev, I. A. Erokhin, Yu. V. Ekimenkova, I. A. Zakharov, A. V. Grigoriev, V. V. Yapaskurt, V. O. Koshlyakova, N. N. |
| description | 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
3+
in tourmaline. Rutile associated with tourmaline contains, wt %: Sb
2
O
5
4.68–11.69, Cr
2
O
3
2.00–8.02, and WO
3
0.88–1.14. It is suggested that tourmaline and associated minerals were formed under oxidizing conditions. |
| doi_str_mv | 10.3103/S0145875223040038 |
| format | article |
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3+
in tourmaline. Rutile associated with tourmaline contains, wt %: Sb
2
O
5
4.68–11.69, Cr
2
O
3
2.00–8.02, and WO
3
0.88–1.14. It is suggested that tourmaline and associated minerals were formed under oxidizing conditions.</description><identifier>ISSN: 0145-8752</identifier><identifier>EISSN: 1934-8436</identifier><identifier>DOI: 10.3103/S0145875223040038</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Analytical methods ; Earth and Environmental Science ; Earth Sciences ; Geology ; Minerals ; Oxidation ; Rutile ; Tourmaline</subject><ispartof>Moscow University geology bulletin, 2023-08, Vol.78 (4), p.504-519</ispartof><rights>Allerton Press, Inc. 2023. ISSN 0145-8752, Moscow University Geology Bulletin, 2023, Vol. 78, No. 4, pp. 504–519. © Allerton Press, Inc., 2023. Russian Text © The Author(s), 2023, published in Vestnik Moskovskogo Universiteta, Seriya 4: Geologiya, 2023, No. 3, pp. 63–76.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c268t-8e9c2a01fa2ede5c86df42fd0db80a110f153de55f4a2016e7eae81fda80af13</cites><orcidid>0000-0003-4277-7216 ; 0000-0001-8790-7892 ; 0000-0002-0577-5898</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Baksheev, I. A.</creatorcontrib><creatorcontrib>Erokhin, Yu. V.</creatorcontrib><creatorcontrib>Ekimenkova, I. A.</creatorcontrib><creatorcontrib>Zakharov, A. V.</creatorcontrib><creatorcontrib>Grigoriev, V. V.</creatorcontrib><creatorcontrib>Yapaskurt, V. O.</creatorcontrib><creatorcontrib>Koshlyakova, N. N.</creatorcontrib><title>Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia</title><title>Moscow University geology bulletin</title><addtitle>Moscow Univ. Geol. Bull</addtitle><description>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
3+
in tourmaline. Rutile associated with tourmaline contains, wt %: Sb
2
O
5
4.68–11.69, Cr
2
O
3
2.00–8.02, and WO
3
0.88–1.14. It is suggested that tourmaline and associated minerals were formed under oxidizing conditions.</description><subject>Analytical methods</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Minerals</subject><subject>Oxidation</subject><subject>Rutile</subject><subject>Tourmaline</subject><issn>0145-8752</issn><issn>1934-8436</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp1UM1Kw0AQXkTBWn0AbwteG53dTdLNUYN_WCjYisewTWZtartbdxNBT76Db-iTuCGCB_HyDcP3M8xHyDGDU8FAnM2AxYkcJ5wLiAGE3CEDlok4krFId8mgo6OO3ycH3q8AkiSLYUBe86Wzm1oZOret26h1bZAqU9HcfX18zhYBHqMLVK42T_S-beo1Uqtps0R6pzZojLXv6PyzRdonNXWDdFqWrXNoShzRHE3j1Jo-BPCjkOF9rQ7Jng4rHv3MIZlfXc7zm2gyvb7NzydRyVPZRBKzkitgWnGsMCllWumY6wqqhQTFGGiWiEAkOlYcWIpjVCiZrlSgNRNDctLHbp19adE3xSp8acLFgssMJM_SWAYV61Wls9471MXW1Rvl3goGRddu8afd4OG9x2-7atD9Jv9v-gaAin8p</recordid><startdate>20230801</startdate><enddate>20230801</enddate><creator>Baksheev, I. A.</creator><creator>Erokhin, Yu. V.</creator><creator>Ekimenkova, I. A.</creator><creator>Zakharov, A. V.</creator><creator>Grigoriev, V. V.</creator><creator>Yapaskurt, V. O.</creator><creator>Koshlyakova, N. N.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0003-4277-7216</orcidid><orcidid>https://orcid.org/0000-0001-8790-7892</orcidid><orcidid>https://orcid.org/0000-0002-0577-5898</orcidid></search><sort><creationdate>20230801</creationdate><title>Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia</title><author>Baksheev, I. A. ; Erokhin, Yu. V. ; Ekimenkova, I. A. ; Zakharov, A. V. ; Grigoriev, V. V. ; Yapaskurt, V. O. ; Koshlyakova, N. N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c268t-8e9c2a01fa2ede5c86df42fd0db80a110f153de55f4a2016e7eae81fda80af13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Analytical methods</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Minerals</topic><topic>Oxidation</topic><topic>Rutile</topic><topic>Tourmaline</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Baksheev, I. A.</creatorcontrib><creatorcontrib>Erokhin, Yu. V.</creatorcontrib><creatorcontrib>Ekimenkova, I. A.</creatorcontrib><creatorcontrib>Zakharov, A. V.</creatorcontrib><creatorcontrib>Grigoriev, V. V.</creatorcontrib><creatorcontrib>Yapaskurt, V. O.</creatorcontrib><creatorcontrib>Koshlyakova, N. N.</creatorcontrib><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Moscow University geology bulletin</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Baksheev, I. A.</au><au>Erokhin, Yu. V.</au><au>Ekimenkova, I. A.</au><au>Zakharov, A. V.</au><au>Grigoriev, V. V.</au><au>Yapaskurt, V. O.</au><au>Koshlyakova, N. N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia</atitle><jtitle>Moscow University geology bulletin</jtitle><stitle>Moscow Univ. Geol. Bull</stitle><date>2023-08-01</date><risdate>2023</risdate><volume>78</volume><issue>4</issue><spage>504</spage><epage>519</epage><pages>504-519</pages><issn>0145-8752</issn><eissn>1934-8436</eissn><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 Fe
3+
in tourmaline. Rutile associated with tourmaline contains, wt %: Sb
2
O
5
4.68–11.69, Cr
2
O
3
2.00–8.02, and WO
3
0.88–1.14. It is suggested that tourmaline and associated minerals were formed under oxidizing conditions.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.3103/S0145875223040038</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0003-4277-7216</orcidid><orcidid>https://orcid.org/0000-0001-8790-7892</orcidid><orcidid>https://orcid.org/0000-0002-0577-5898</orcidid></addata></record> |
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| issn | 0145-8752 1934-8436 |
| language | eng |
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| subjects | Analytical methods Earth and Environmental Science Earth Sciences Geology Minerals Oxidation Rutile Tourmaline |
| title | Chromian Tourmaline and Cr–Sb–W-Bearing Rutile of the Kamennoozerskoe Chromitite Occurrence, Central Urals, Russia |
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