Ryabchikovite, CuMg(Si2O6), a new pyroxene group mineral, and some genetic features of natural anhydrous copper silicates
-
Nadezhda V. Shchipalkina
, Igor V. Pekov
Abstract
Ryabchikovite, ideally CuMg(Si2O6), a new pyroxene-group mineral (IMA No. 2021-011) was discovered in exhalations of the active Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. The associated minerals are diopside, hematite, cuprospinel, fluorophlogopite, anhydrite, johillerite, tilasite, and aphthitalite-group sulfates. Ryabchikovite forms thin (up to 25 μm), light brown to reddish-brown epitactic crusts on short-prismatic brownish-gray crystals of diopside (up to 0.5 mm). The new mineral is optically biaxial (+), α = 1.685(5), β = 1.690(5), γ = 1.703(4), and 2V (meas) = 60(15)°. The average chemical composition (wt%, electron microprobe data) is: MgO 18.05, CaO 0.77, CuO 26.46, ZnO 2.23, Al2O3 0.93, Fe2O3 1.89, SiO2 50.10, total 100.43. The empirical formula calculated based on 6 O atoms per formulas unit is
Funding statement: This work was supported by the Russian Science Foundation, grant no. 1917-00050. The authors thank the Resource Center of X-ray diffraction studies and Geomodel Resource Centre of Saint-Petersburg State University for providing instrumental and computational resources. Raman measurements were partly performed at SPbSU Research park Center for optical and laser materials research with financial support from St. Petersburg State University (project no. 93021679).
Acknowledgments
We are grateful to Mario Tribaudino, Frank C. Hawthorne, and an anonymous reviewer for valuable comments and suggestions for improving the paper, and Fabrizio Nestola for his editorial work.
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