The new mineral novograblenovite, (NH4,K)MgCl3•6H2O from the Tolbachik volcano, Kamchatka, Russia: mineral description and crystal structure

被引:11
作者
Okrugin, Viktor M. [1 ]
Kudaeva, Sharapat S. [1 ]
Karimova, Oxana, V [2 ]
Yakubovich, Olga, V [2 ,3 ]
Belakovskiy, Dmitry, I [4 ]
Chukanov, Nikita, V [5 ]
Zolotarev, Andrey A. [6 ]
Gurzhiy, Vladislav V. [6 ]
Zinovieva, Nina G. [3 ]
Shiryaev, Andrey A. [2 ,7 ]
Kartashov, Pavel M. [2 ]
机构
[1] Inst Volcanol & Seismol FEB RAS, Piip Blvd 9, Petropavlovsk Kamchatski 683006, Russia
[2] RAS, Inst Geol Ore Deposits Geochem Mineral & Petrog I, Staromonetny 35, Moscow 119017, Russia
[3] Moscow MV Lomonosov State Univ, Fac Geol, Moscow 119899, Russia
[4] Fersman Mineral Museum RAS, Leninskiy Prospect 18-2, Moscow 119071, Russia
[5] Russian Acad Sci, Inst Problems Chem Phys, Chernogolovka 142432, Moscow Region, Russia
[6] St Petersburg State Univ, Inst Earth Sci, Univ Emb 7-9, St Petersburg 199034, Russia
[7] Frumkin Inst Phys Chem & Electrochem RAS, Leninsky Prospect 31,Korp 4, Moscow 119071, Russia
关键词
novograblenovite; new mineral; ammonium potassium magnesium chloride hydrate; crystal structure; Plosky Tolbachik volcano; Kamchatka; AMMONIUM-SULFATE CHLORIDE; BOND-VALENCE PARAMETERS; LA FOSSA CRATER; AEOLIAN ISLANDS; CARNALLITE; VULCANO;
D O I
10.1180/mgm.2018.88
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The new mineral novograblenovite, (NH4,K)MgCl3 center dot 6H(2)O, was found on basaltic lava from the 2012-2013 Tolbachik fissure eruption at the Plosky Tolbachik volcano, Kamchatka Peninsula, Russia. It occurs as prismatic, needle-like transparent crystals together with gypsum and halite. Novograblenovite was formed due to the exposure of the host rocks to eruptive gas exhalations enriched in HCl and NH3. Basalt was the source of potassium and magnesium for the mineral formation. Novograblenovite crystallises in the monoclinic space group C2/c, with unit-cell parameters a = 9.2734(3) angstrom, b = 9.5176(3) angstrom, c = 13.2439(4) angstrom, beta= 90.187(2)degrees, V = 1168.91(2) angstrom(3) and Z= 4. The five strongest reflections in the powder X-ray diffraction pattern [d(obs), angstrom (I, %) (h k l)] are: 3.330 (100) (2 2 0), 2.976 (45) ((1) over bar 1 4), 2.353 (29) ((2) over bar 2 4), 3.825 (26) (2 0 2), 1.997 (25) ((4 2) over bar 2). The density calculated from the empirical formula and the X-ray data is 1.504 g cm(-3). The mineral is biaxial (+) with alpha = 1.469(2), beta = 1.479(2) and gamma = 1.496(2) (lambda = 589 nm); 2V(meas.) = 80(10)degrees and 2Va(calc.) = 75.7 degrees. The crystal structure (solved and refined using single-crystal X-ray diffraction data, R-1 = 0.0423) is based on the perovskite-like network of (NH4,K)Cl-6-octahedra sharing chlorine vertices, and comprises [Mg(H2O)(6)](2+) groups in framework channels. The positions of all independent H atoms were obtained by difference-Fourier techniques and refined isotropically. All oxygen, nitrogen and chlorine atoms are involved in the system of hydrogen bonding, acting as donors or acceptors. The formula resulting from the structure refinement is [(NH4)(0.7)K-0.3]MgCl3 center dot 6H(2)O. The mineral is named after Prokopiy Trifonovich Novograblenov, one of the researchers of Kamchatka Peninsula, a teacher, naturalist, geographer and geologist.
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页码:223 / 231
页数:9
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