A new mineral sanguite, KCuCl3, is found in the Glavnaya Tenoritovaya fumarole at the Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Associated minerals are belloite, avdoninite, eriochalcite, sylvite, halite, carnallite, mitscherlichite, chrysothallite, romanorlovite, mellizinkalite, gypsum, chlorothionite, kainite, sellaite, and earlier hematite, tenorite, and chalcocyanite. Sanguite forms prismatic crystals up to 1 mm long and up to 0.2 mm thick, typically combined in groups, dense clusters, or crusts up to several dozens of cm2 in area. The major crystal forms are {011}, {100}, and {010}. The mineral is transparent, with vitreous luster. Its color is bright red, and slightly altered samples are dark red to brownish red. Sanguite is brittle. Its Mohs' hardness is ca 3. Cleavage is perfect on (010), fracture is stepped. Dmeas = 2.86(1), Dcalc = 2.88 g cm−3. Sanguite is optically biaxial (−), α 1.653(3), β 1.780(6), γ 1.900(8), 2Vmeas = 85(5)°. The Raman spectrum is reported. The chemical composition (wt.%, electron microprobe data) is: K 18.57, Cu 29.79, Cl 50.66, total 99.02. The empirical formula calculated on the sum of atoms = 5 pfu is: K1.00Cu0.99Cl3.01. Sanguite is monoclinic, P21/c, a 4.0281(2), b 13.7906(5), c 8.7335(4) Å, β 97.137(4)°, V 481.38(3) Å3, and Z = 4. The strongest reflections of the powder X-ray diffraction pattern [d, Å(I)(hkl)] are: 7.36(78)(011), 6.92(100)(020), 3.684(69)(111), 3.146(64)(032, 102), 3.068(63)(112), 2.857(73)(122), 2.709(82)(112, 042), and 2.574(56)(122). The crystal structure, solved from single-crystal X-ray diffraction data (R = 0.0545), contains almost planar, discrete dimers [Cu2+2Cl6]. The KCl9 polyhedra are connected via common faces to form interrupted layers. Neighboring layers are linked to each other by the common edges of the K-centered polyhedra. The mineral is named from the Latin sanguis (blood), alluding to its color.
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Research Article|
July 01, 2015
Sanguite, KCuCl3, a New Mineral from the Tolbachik Volcano, Kamchatka, Russia
Igor V. Pekov;
Igor V. Pekov
§
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
§Corresponding author e-mail address: [email protected]
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Natalia V. Zubkova;
Natalia V. Zubkova
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
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Dmitry I. Belakovskiy;
Dmitry I. Belakovskiy
Fersman Mineralogical Museum of Russian Academy of Sciences, Leninskiy Prospekt 18-2, 119071 Moscow, Russia
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Inna S. Lykova;
Inna S. Lykova
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
Fersman Mineralogical Museum of Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia
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Vasiliy O. Yapaskurt;
Vasiliy O. Yapaskurt
Faculty of Geology, Moscow State University, Leninskie Gory 119991, Moscow, Russia
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Marina F. Vigasina;
Marina F. Vigasina
Faculty of Geology, Moscow State University, Leninskie Gory 119991, Moscow, Russia
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Evgeny G. Sidorov;
Evgeny G. Sidorov
Institute of Volcanology and Seismology, Far Eastern Branch of the Russian Academy of Sciences, Piip Boulevard 9, 683006 Petropavlovsk-Kamchatsky, Russia
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Dmitry Yu. Pushcharovsky
Dmitry Yu. Pushcharovsky
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
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Igor V. Pekov
§
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
Natalia V. Zubkova
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
Dmitry I. Belakovskiy
Fersman Mineralogical Museum of Russian Academy of Sciences, Leninskiy Prospekt 18-2, 119071 Moscow, Russia
Inna S. Lykova
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
Fersman Mineralogical Museum of Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia
Vasiliy O. Yapaskurt
Faculty of Geology, Moscow State University, Leninskie Gory 119991, Moscow, Russia
Marina F. Vigasina
Faculty of Geology, Moscow State University, Leninskie Gory 119991, Moscow, Russia
Evgeny G. Sidorov
Institute of Volcanology and Seismology, Far Eastern Branch of the Russian Academy of Sciences, Piip Boulevard 9, 683006 Petropavlovsk-Kamchatsky, Russia
Dmitry Yu. Pushcharovsky
Faculty of Geology, Moscow State University, Leninskie Gory, 119991 Moscow, Russia
§Corresponding author e-mail address: [email protected]
Publisher: Mineralogical Association of Canada
Received:
26 Jan 2015
Accepted:
22 Jul 2015
First Online:
16 Feb 2018
Online ISSN: 1499-1276
Print ISSN: 0008-4476
© 2015 Mineralogical Association of Canada
The Canadian Mineralogist (2015) 53 (4): 633–641.
Article history
Received:
26 Jan 2015
Accepted:
22 Jul 2015
First Online:
16 Feb 2018
Citation
Igor V. Pekov, Natalia V. Zubkova, Dmitry I. Belakovskiy, Inna S. Lykova, Vasiliy O. Yapaskurt, Marina F. Vigasina, Evgeny G. Sidorov, Dmitry Yu. Pushcharovsky; Sanguite, KCuCl3, a New Mineral from the Tolbachik Volcano, Kamchatka, Russia. The Canadian Mineralogist 2015;; 53 (4): 633–641. doi: https://doi.org/10.3749/canmin.1500012
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Index Terms/Descriptors
- Asia
- carnallite
- chemical composition
- chlorides
- coexisting minerals
- Commonwealth of Independent States
- copper minerals
- crystal chemistry
- crystal structure
- electron probe data
- formula
- fumaroles
- gypsum
- halides
- halite
- igneous rocks
- kainite
- Kamchatka Peninsula
- lattice parameters
- new minerals
- polyhedra
- pyroclastics
- Russian Federation
- Russian Pacific region
- scoria
- space groups
- sulfates
- sylvite
- Tolbachik
- unit cell
- volcanic rocks
- volcanoes
- X-ray diffraction data
- mitscherlichite
- tenorite
- chlorothionite
- sellaite
- eriochalcite
- chalcocyanite
- avdoninite
- belloite
- chrysothallite
- sanguite
- romanorlovite
- mellizinkalite
Latitude & Longitude
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