Oksana V. Udoratina, Taras L. Panikorovskii, Nikita V. Chukanov, Mikhail V. Voronin, Vladimir P. Lutoev, Atali A. Agakhanov, Sergey I. Isaenko
{"title":"Dmitryvarlamovite，Ti2(Fe3+Nb)O8，一种与黑钨矿类有关的新铌铁矿超群矿物","authors":"Oksana V. Udoratina, Taras L. Panikorovskii, Nikita V. Chukanov, Mikhail V. Voronin, Vladimir P. Lutoev, Atali A. Agakhanov, Sergey I. Isaenko","doi":"10.1180/mgm.2023.95","DOIUrl":null,"url":null,"abstract":"<p>The new columbite-supergroup mineral dmitryvarlamovite, ideally Ti<span>2</span>(Fe<span>3+</span>Nb)O<span>8</span>, was discovered in weathered alkaline metasomatic assemblages formed after late Riphaean sedimentary carbonate rocks of the Verkhne-Shchugorskoe deposit, Middle Timan Mts., Russia. The associated minerals are columbite-(Fe), pyrochlore-group minerals, monazite-(Ce), xenotime-(Y), baryte, pyrite, drugmanite and plumbogummite. Dmitryvarlamovite occurs as isolated anhedral equant grains up to 0.5 mm across. The colour of dmitryvarlamovite is black, the streak is black and the lustre is submetallic. The new mineral is brittle, with the mean VHN hardness of 753 kg mm<span>–2</span> corresponding to the Mohs’ hardness of 6. No cleavage is observed. The fracture is conchoidal. The calculated density is 4.891 g⋅cm<span>–3</span>. In reflected light, dmitryvarlamovite is light grey; no pleochroism is observed. The reflectance values (<span>R</span><span>min</span>, % / <span>R</span><span>max</span>, % / λ, nm) are: 19.8/20.3/470, 18.3/18.9/546, 17.8/18.5/589 and 17.3/17.8/650. The chemical composition is (electron microprobe data, with iron divided into Fe<span>2</span>O<span>3</span> and FeO based on the charge balance, wt.%): MnO 0.11, FeO 1.51, V<span>2</span>O<span>3</span> 0.89, Cr<span>2</span>O<span>3</span> 0.28, Fe<span>2</span>O<span>3</span> 19.26, TiO<span>2</span> 37.72, Nb<span>2</span>O<span>5</span> 40.08, total 99.85. The IR and Raman spectra indicate the absence of H-, C- and N-bearing groups. The empirical formula is (Fe<span>2+</span><span>0.08</span>V<span>3+</span><span>0.05</span>Cr<span>3+</span><span>0.01</span>Fe<span>3+</span><span>0.92</span>Ti<span>1.79</span>Nb<span>1.15</span>)<span>Σ4.00</span>O<span>8</span>. The crystal structure was determined using single-crystal X-ray diffraction data and refined to <span>R</span> = 0.048. Dmitryvarlamovite is orthorhombic, space group <span>P</span>2<span>1</span>2<span>1</span>2, <span>a</span> = 4.9825(6), <span>b</span> = 4.6268(4), <span>c</span> = 5.5952(6) Å and <span>V</span> = 5.5952(6) Å<span>3</span> (<span>Z</span> = 1). The structure is related to those of wolframite-group minerals but differs in the scheme of cation ordering. The crystal-chemical formula derived based on the structural data is (Ti<span>0.57</span>Nb<span>0.21</span>Fe<span>3+</span><span>0.15</span>Fe<span>2+</span><span>0.04</span>V<span>0.02</span>Cr<span>0.01</span>)<span>2</span>(Nb<span>0.36</span>Ti<span>0.33</span>Fe<span>3+</span><span>0.31</span>)<span>2</span>O<span>8</span>. The strongest lines of the powder X-ray diffraction pattern [<span>d</span>, Å (<span>I</span>, %) (<span>hkl</span>)] are: 3.58 (40) (011), 2.911 (100) (111), 2.809 (40) (002), 2.497 (38) (020), 2.447 (29) (103), 1.7363 (32) (103) and 1.7047 (29) (220). Dmitryvarlamovite is named after Dmitry Anatol'evich Varlamov (b. 1965).</p>","PeriodicalId":18618,"journal":{"name":"Mineralogical Magazine","volume":"97 1","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2024-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Dmitryvarlamovite, Ti2(Fe3+Nb)O8, a new columbite-supergroup mineral related to the wolframite group\",\"authors\":\"Oksana V. Udoratina, Taras L. Panikorovskii, Nikita V. Chukanov, Mikhail V. Voronin, Vladimir P. Lutoev, Atali A. Agakhanov, Sergey I. Isaenko\",\"doi\":\"10.1180/mgm.2023.95\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>The new columbite-supergroup mineral dmitryvarlamovite, ideally Ti<span>2</span>(Fe<span>3+</span>Nb)O<span>8</span>, was discovered in weathered alkaline metasomatic assemblages formed after late Riphaean sedimentary carbonate rocks of the Verkhne-Shchugorskoe deposit, Middle Timan Mts., Russia. The associated minerals are columbite-(Fe), pyrochlore-group minerals, monazite-(Ce), xenotime-(Y), baryte, pyrite, drugmanite and plumbogummite. Dmitryvarlamovite occurs as isolated anhedral equant grains up to 0.5 mm across. The colour of dmitryvarlamovite is black, the streak is black and the lustre is submetallic. The new mineral is brittle, with the mean VHN hardness of 753 kg mm<span>–2</span> corresponding to the Mohs’ hardness of 6. No cleavage is observed. The fracture is conchoidal. The calculated density is 4.891 g⋅cm<span>–3</span>. In reflected light, dmitryvarlamovite is light grey; no pleochroism is observed. The reflectance values (<span>R</span><span>min</span>, % / <span>R</span><span>max</span>, % / λ, nm) are: 19.8/20.3/470, 18.3/18.9/546, 17.8/18.5/589 and 17.3/17.8/650. The chemical composition is (electron microprobe data, with iron divided into Fe<span>2</span>O<span>3</span> and FeO based on the charge balance, wt.%): MnO 0.11, FeO 1.51, V<span>2</span>O<span>3</span> 0.89, Cr<span>2</span>O<span>3</span> 0.28, Fe<span>2</span>O<span>3</span> 19.26, TiO<span>2</span> 37.72, Nb<span>2</span>O<span>5</span> 40.08, total 99.85. The IR and Raman spectra indicate the absence of H-, C- and N-bearing groups. The empirical formula is (Fe<span>2+</span><span>0.08</span>V<span>3+</span><span>0.05</span>Cr<span>3+</span><span>0.01</span>Fe<span>3+</span><span>0.92</span>Ti<span>1.79</span>Nb<span>1.15</span>)<span>Σ4.00</span>O<span>8</span>. The crystal structure was determined using single-crystal X-ray diffraction data and refined to <span>R</span> = 0.048. Dmitryvarlamovite is orthorhombic, space group <span>P</span>2<span>1</span>2<span>1</span>2, <span>a</span> = 4.9825(6), <span>b</span> = 4.6268(4), <span>c</span> = 5.5952(6) Å and <span>V</span> = 5.5952(6) Å<span>3</span> (<span>Z</span> = 1). The structure is related to those of wolframite-group minerals but differs in the scheme of cation ordering. The crystal-chemical formula derived based on the structural data is (Ti<span>0.57</span>Nb<span>0.21</span>Fe<span>3+</span><span>0.15</span>Fe<span>2+</span><span>0.04</span>V<span>0.02</span>Cr<span>0.01</span>)<span>2</span>(Nb<span>0.36</span>Ti<span>0.33</span>Fe<span>3+</span><span>0.31</span>)<span>2</span>O<span>8</span>. The strongest lines of the powder X-ray diffraction pattern [<span>d</span>, Å (<span>I</span>, %) (<span>hkl</span>)] are: 3.58 (40) (011), 2.911 (100) (111), 2.809 (40) (002), 2.497 (38) (020), 2.447 (29) (103), 1.7363 (32) (103) and 1.7047 (29) (220). Dmitryvarlamovite is named after Dmitry Anatol'evich Varlamov (b. 1965).</p>\",\"PeriodicalId\":18618,\"journal\":{\"name\":\"Mineralogical Magazine\",\"volume\":\"97 1\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2024-02-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mineralogical Magazine\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1180/mgm.2023.95\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"MINERALOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mineralogical Magazine","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1180/mgm.2023.95","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"MINERALOGY","Score":null,"Total":0}
Dmitryvarlamovite, Ti2(Fe3+Nb)O8, a new columbite-supergroup mineral related to the wolframite group
The new columbite-supergroup mineral dmitryvarlamovite, ideally Ti2(Fe3+Nb)O8, was discovered in weathered alkaline metasomatic assemblages formed after late Riphaean sedimentary carbonate rocks of the Verkhne-Shchugorskoe deposit, Middle Timan Mts., Russia. The associated minerals are columbite-(Fe), pyrochlore-group minerals, monazite-(Ce), xenotime-(Y), baryte, pyrite, drugmanite and plumbogummite. Dmitryvarlamovite occurs as isolated anhedral equant grains up to 0.5 mm across. The colour of dmitryvarlamovite is black, the streak is black and the lustre is submetallic. The new mineral is brittle, with the mean VHN hardness of 753 kg mm–2 corresponding to the Mohs’ hardness of 6. No cleavage is observed. The fracture is conchoidal. The calculated density is 4.891 g⋅cm–3. In reflected light, dmitryvarlamovite is light grey; no pleochroism is observed. The reflectance values (Rmin, % / Rmax, % / λ, nm) are: 19.8/20.3/470, 18.3/18.9/546, 17.8/18.5/589 and 17.3/17.8/650. The chemical composition is (electron microprobe data, with iron divided into Fe2O3 and FeO based on the charge balance, wt.%): MnO 0.11, FeO 1.51, V2O3 0.89, Cr2O3 0.28, Fe2O3 19.26, TiO2 37.72, Nb2O5 40.08, total 99.85. The IR and Raman spectra indicate the absence of H-, C- and N-bearing groups. The empirical formula is (Fe2+0.08V3+0.05Cr3+0.01Fe3+0.92Ti1.79Nb1.15)Σ4.00O8. The crystal structure was determined using single-crystal X-ray diffraction data and refined to R = 0.048. Dmitryvarlamovite is orthorhombic, space group P21212, a = 4.9825(6), b = 4.6268(4), c = 5.5952(6) Å and V = 5.5952(6) Å3 (Z = 1). The structure is related to those of wolframite-group minerals but differs in the scheme of cation ordering. The crystal-chemical formula derived based on the structural data is (Ti0.57Nb0.21Fe3+0.15Fe2+0.04V0.02Cr0.01)2(Nb0.36Ti0.33Fe3+0.31)2O8. The strongest lines of the powder X-ray diffraction pattern [d, Å (I, %) (hkl)] are: 3.58 (40) (011), 2.911 (100) (111), 2.809 (40) (002), 2.497 (38) (020), 2.447 (29) (103), 1.7363 (32) (103) and 1.7047 (29) (220). Dmitryvarlamovite is named after Dmitry Anatol'evich Varlamov (b. 1965).
期刊介绍：
Mineralogical Magazine is an international journal of mineral sciences which covers the fields of mineralogy, crystallography, geochemistry, petrology, environmental geology and economic geology. The journal has been published continuously since the founding of the Mineralogical Society of Great Britain and Ireland in 1876 and is a leading journal in its field.
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