VULCANITE, CUTE: HYDROTHERMAL SYNTHESIS AND CRYSTAL STRUCTURE REFINEMENT

dc.contributor.author	Pertlik F.
dc.date.accessioned	2021-04-03T01:40:00Z
dc.date.available	2021-04-03T01:40:00Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=884444
dc.identifier.citation	Mineralogy and Petrology, 2001, 71, 3-4, 149-154
dc.identifier.issn	0930-0708
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/27224
dc.description.abstract	The crystal structure of the mineral vulcanite, CuTe [a = 3.155(1), b = 4.092(1), c = 6.956(1) A; Z = 2; space group: Pmmn, No. 59] exhibits a pronounced layer structure with Te-Te distances between the CuTe layers of 4.019(1) A. Within a range up to 4.2 A the individual Cu atom is [4Te+4Cu+2Cu], the individual Te atom [4Cu+2Te+4Te] coordinated. Crystals of vulcanite suitable for the present structure investigation were synthesized under hydrothermal conditions.
dc.title	VULCANITE, CUTE: HYDROTHERMAL SYNTHESIS AND CRYSTAL STRUCTURE REFINEMENT
dc.type	Статья

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