Standard

Steklite, KAl(SO4)2: A finding at the Tolbachik Volcano, Kamchatka, Russia, validating its status as a mineral species and crystal structure. / Murashko, M.N.; Pekov, I.V.; Krivovichev, S.V.; Chernyatyeva, A.P.; Yapaskurt, V.O.; Zadov, A.E.; Zelensky, M.E.

в: Geology of Ore Deposits, № 7, 2013, стр. 594-600.

Результаты исследований: Научные публикации в периодических изданияхстатья

Harvard

Murashko, MN, Pekov, IV, Krivovichev, SV, Chernyatyeva, AP, Yapaskurt, VO, Zadov, AE & Zelensky, ME 2013, 'Steklite, KAl(SO4)2: A finding at the Tolbachik Volcano, Kamchatka, Russia, validating its status as a mineral species and crystal structure', Geology of Ore Deposits, № 7, стр. 594-600. https://doi.org/10.1134/S1075701513070088

APA

Murashko, M. N., Pekov, I. V., Krivovichev, S. V., Chernyatyeva, A. P., Yapaskurt, V. O., Zadov, A. E., & Zelensky, M. E. (2013). Steklite, KAl(SO4)2: A finding at the Tolbachik Volcano, Kamchatka, Russia, validating its status as a mineral species and crystal structure. Geology of Ore Deposits, (7), 594-600. https://doi.org/10.1134/S1075701513070088

Vancouver

Author

Murashko, M.N. ; Pekov, I.V. ; Krivovichev, S.V. ; Chernyatyeva, A.P. ; Yapaskurt, V.O. ; Zadov, A.E. ; Zelensky, M.E. / Steklite, KAl(SO4)2: A finding at the Tolbachik Volcano, Kamchatka, Russia, validating its status as a mineral species and crystal structure. в: Geology of Ore Deposits. 2013 ; № 7. стр. 594-600.

BibTeX

@article{75f9aa11bfee4e88996d313006d1365c,
title = "Steklite, KAl(SO4)2: A finding at the Tolbachik Volcano, Kamchatka, Russia, validating its status as a mineral species and crystal structure",
abstract = "Steklite KAl(SO4)2 has been found in sublimates of the Yadovitaya (Poisonous) fumarole at the second cinder cone of the northern breach of the Great Fissure Tolbachik Eruption, Tolbachik volcano, Kamchatka Peninsula, Russia. Steklite was approved as a valid mineral species by the Commission on New Minerals, Nomenclature, and Mineral Classification of the International Mineralogical Association on June 2, 2011 (IMA no. 2011-041). The name steklite is left for this mineral, as it was named by Chesnokov et al. (1995) for its technogenic analog from a burnt dump of coal mine no. 47 at Kopeisk, the Southern Urals, Russia. It is named after the Russian word steklo, meaning glass, in allusion to the visual similarity of its lamellae to thin glass platelets. At Tolbachik, steklite is associated with alumoklyuchevskite, langbeinite, euchlorine, fedotovite, chalcocyanite, hematite, and lyonsite. It occurs as hexagonal or irregular-shaped lamellar crystals with the major form {001} reaching 30 μm in thickness and 0.2 mm",
author = "M.N. Murashko and I.V. Pekov and S.V. Krivovichev and A.P. Chernyatyeva and V.O. Yapaskurt and A.E. Zadov and M.E. Zelensky",
year = "2013",
doi = "10.1134/S1075701513070088",
language = "English",
pages = "594--600",
journal = "Geology of Ore Deposits",
issn = "1075-7015",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "7",

}

RIS

TY - JOUR

T1 - Steklite, KAl(SO4)2: A finding at the Tolbachik Volcano, Kamchatka, Russia, validating its status as a mineral species and crystal structure

AU - Murashko, M.N.

AU - Pekov, I.V.

AU - Krivovichev, S.V.

AU - Chernyatyeva, A.P.

AU - Yapaskurt, V.O.

AU - Zadov, A.E.

AU - Zelensky, M.E.

PY - 2013

Y1 - 2013

N2 - Steklite KAl(SO4)2 has been found in sublimates of the Yadovitaya (Poisonous) fumarole at the second cinder cone of the northern breach of the Great Fissure Tolbachik Eruption, Tolbachik volcano, Kamchatka Peninsula, Russia. Steklite was approved as a valid mineral species by the Commission on New Minerals, Nomenclature, and Mineral Classification of the International Mineralogical Association on June 2, 2011 (IMA no. 2011-041). The name steklite is left for this mineral, as it was named by Chesnokov et al. (1995) for its technogenic analog from a burnt dump of coal mine no. 47 at Kopeisk, the Southern Urals, Russia. It is named after the Russian word steklo, meaning glass, in allusion to the visual similarity of its lamellae to thin glass platelets. At Tolbachik, steklite is associated with alumoklyuchevskite, langbeinite, euchlorine, fedotovite, chalcocyanite, hematite, and lyonsite. It occurs as hexagonal or irregular-shaped lamellar crystals with the major form {001} reaching 30 μm in thickness and 0.2 mm

AB - Steklite KAl(SO4)2 has been found in sublimates of the Yadovitaya (Poisonous) fumarole at the second cinder cone of the northern breach of the Great Fissure Tolbachik Eruption, Tolbachik volcano, Kamchatka Peninsula, Russia. Steklite was approved as a valid mineral species by the Commission on New Minerals, Nomenclature, and Mineral Classification of the International Mineralogical Association on June 2, 2011 (IMA no. 2011-041). The name steklite is left for this mineral, as it was named by Chesnokov et al. (1995) for its technogenic analog from a burnt dump of coal mine no. 47 at Kopeisk, the Southern Urals, Russia. It is named after the Russian word steklo, meaning glass, in allusion to the visual similarity of its lamellae to thin glass platelets. At Tolbachik, steklite is associated with alumoklyuchevskite, langbeinite, euchlorine, fedotovite, chalcocyanite, hematite, and lyonsite. It occurs as hexagonal or irregular-shaped lamellar crystals with the major form {001} reaching 30 μm in thickness and 0.2 mm

U2 - 10.1134/S1075701513070088

DO - 10.1134/S1075701513070088

M3 - Article

SP - 594

EP - 600

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 7

ER -

ID: 7520667