Marinaite, Cu <sub>2</sub> Fe <sup>3+</sup> O <sub>2</sub> (BO <sub>3</sub> ), a new ludwigite-group mineral from Tolbachik volcano, Kamchatka, Russia.

Marinaite, ideally Cu 2 Fe 3+ O 2 (BO 3 ), a new mineral, was found in a high-temperature (400-600C) crack on the cooling lava field of the 2012-2013 fissure eruption at Tolbachik volcano, Kamchatka, Russia.The associated minerals are belomarinaite, tenorite, hematite, anglesite and gold.Marinaite forms prismatic, tabular, lamellar or acicular crystals up to 0.06 x 0.06 x 0.3 mm or aggregates of these forms up to 3 mm across.The mineral has a brown to black colour and submetallic lustre.Under the microscope in reflected light marinaite is grey with reddish-brown internal reflections.D calc .=5.026 g/cm 3 .Electron microprobe analyses yielded (wt.%) 62.15 CuO, 16.71 Fe 2 O 3 , 5.11 Al 2 O 3 , 3.14 TiO 2 , 0.16 SiO 2 , 12.84 B 2 O 3 , total 100.11wt.%.The empirical formula calculated based on 5 O apfu is Cu 2.07 Fe 0.56 Al 0.27 Ti 0.10 Si 0.01 B 0.98 O 5 .Marinaite is monoclinic, space group P2 1 /c, unit-cell parameters are: a = 3.12750(18), b = 11.9690(8),c = 9.4657(5) , = 97.568(6),V = 351.24(4) 3 and Z=4.The strongest lines of the powder XRD pattern [d in (I)(hkl)] are: 5.

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Publication Details

Journal
Mineralogical Magazine
Published
2025-11-24
DOI
https://doi.org/10.1180/mgm.2025.10179
Primary Topic
Crystal Structures and Properties
Type
article
Field-Weighted Citation Impact
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article

Marinaite, Cu 2 Fe 3+ O 2 (BO 3 ), a new ludwigite-group mineral from Tolbachik volcano, Kamchatka, Russia.

Ilya Chaplygin, Natalia V. Zubkova, И. Г. Грибоедова, Marina A. Yudovskaya et al.
Mineralogical Magazine
Crystal Structures and Properties
article

Marinaite, Cu 2 Fe 3+ O 2 (BO 3 ), a new ludwigite-group mineral from Tolbachik volcano, Kamchatka, Russia.

Ilya Chaplygin, Natalia V. Zubkova, И. Г. Грибоедова, Marina A. Yudovskaya, Dmitry I. Belakovskiy, Sergey N. Britvin, Д. А. Ксенофонтов, М. Ф. Вигасина, В. А. Рассулов, Н. Н. Кононкова, Dmitry Yu. Pushcharovsky, Igor V. Pekov
article en

Abstract

Marinaite, ideally Cu 2 Fe 3+ O 2 (BO 3 ), a new mineral, was found in a high-temperature (400-600C) crack on the cooling lava field of the 2012-2013 fissure eruption at Tolbachik volcano, Kamchatka, Russia.The associated minerals are belomarinaite, tenorite, hematite, anglesite and gold.Marinaite forms prismatic, tabular, lamellar or acicular crystals up to 0.06 x 0.06 x 0.3 mm or aggregates of these forms up to 3 mm across.The mineral has a brown to black colour and submetallic lustre.Under the microscope in reflected light marinaite is grey with reddish-brown internal reflections.D calc .=5.026 g/cm 3 .Electron microprobe analyses yielded (wt.%) 62.15 CuO, 16.71 Fe 2 O 3 , 5.11 Al 2 O 3 , 3.14 TiO 2 , 0.16 SiO 2 , 12.84 B 2 O 3 , total 100.11wt.%.The empirical formula calculated based on 5 O apfu is Cu 2.07 Fe 0.56 Al 0.27 Ti 0.10 Si 0.01 B 0.98 O 5 .Marinaite is monoclinic, space group P2 1 /c, unit-cell parameters are: a = 3.12750(18), b = 11.9690(8),c = 9.4657(5) , = 97.568(6),V = 351.24(4) 3 and Z=4.The strongest lines of the powder XRD pattern [d in (I)(hkl)] are: 5.

Mineralogical Magazine
St Petersburg University (RU), Lomonosov Moscow State University (RU), Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry (RU), All-Russian Scientific-Research Institute Of Mineral Resources named after N.M. Fedorovsky (RU), V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry (RU), Russian Academy of Natural Sciences (RU)
Far East Branch, Russian Academy of Sciences
Openalex Percentile: Top 74%
Crystal Structures and Properties
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