Zobrazeno 1 - 7
of 7
pro vyhledávání: '"G. K. Bekenova"'
Publikováno v:
Geology of Ore Deposits. 63:830-841
Publikováno v:
Metallurgist. 64:75-81
Information is provided about prospects for vanadium ore deposits in Kazakhstan, the history of exploration of the deposits of Greater Karatau (Southern Kazakhstan), and mineralogical study indicating the potential for the involvement of vanadium raw
Autor:
G. K. Bekenova, M. Khakimzhanov, Kstu, Karaganda, Kazakhstan, V. G. Stepanets, E. S. Li, N. M. Zhukov, Kazakhstan Srk Consulting (Kazakhstan) Ltd, V. L. Levin
Publikováno v:
NEWS of National Academy of Sciences of the Republic of Kazakhstan. 2:21-29
Publikováno v:
Mineralogical Magazine. 76:37-44
Natrotitanite, ideally (Na0.5Y0.5)Ti(SiO4)O, is a new mineral from the Verkhnee Espe rare-element deposit at the northern exo-contact of the Akjailyautas granite massif in the northern part of the Tarbagatai mountain range, Eastern Kazakhstan. Both t
Autor:
S. Möckel, G. K. Bekenova, A. A. Mukhanova, D. I. Belakovsky, Nikita V. Chukanov, Igor V. Pekov, L. A. Levitskaya
Publikováno v:
Geology of Ore Deposits. 52:599-605
Kamarizaite, a new mineral species, has been identified in the dump of the Kamariza Mine, Lavrion mining district, Attica Region, Greece, in association with goethite, scorodite, and jarosite. It was named after type locality. Kamarizaite occurs as f
Autor:
G. K. Bekenova, P. E. Kotel'nikov, A. V. Stepanov, Yassir A. Abdu, Elena Sokolova, F. C. Hawthorne
Publikováno v:
Mineralogical Magazine. 73:847-854
Cámaraite, ideally Ba3NaTi4(Fe2+,Mn)8(Si2O7)4O4(OH,F)7, is a new mineral from the Verkhnee Espe deposit, Akjailyautas Mountains, Kazakhstan. It occurs as intergrowths with bafertisite and jinshajiangite in separate platy crystals up to 8 mm × 15 mm
Autor:
N. I. Krasnova, Alla N. Bogdanova, G. K. Bekenova, A. V. Antonov, M. A. Yagovkina, S. N. Britvin, Nikita V. Chukanov
Publikováno v:
Geology of Ore Deposits. 50:556-564
Karchevskyite, a new mineral related to the family of layered double hydroxides (LDHs), has been found in the Iron open pit at the Kovdor carbonatite massif, Kola Peninsula, Russia. The mineral occurs as spherulites of up to 1.5 mm in diameter compos