Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color

In the Bazhenovskoye chrysotile–asbestos deposit (Middle Urals), nephrite bodies of the serpentinite type were found on the contact of after gabbro rodingites and serpentinites. The color is uniform to non-uniform, green to light green, bluish green, greyish green, and whitish. Spots, streaks, lenti...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Evgeniy V. Kislov, Yuriy V. Erokhin, Mikhail P. Popov, Anatoliy G. Nikolayev
Formato:	article
Lenguaje:	EN
Publicado:	MDPI AG 2021
Materias:	nephrite mineralogy ornamental stone Bazhenovskoye deposit Mineralogy QE351-399.2
Acceso en línea:	https://doaj.org/article/0261c98c15e04d8aac5200eb8779a94e
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:0261c98c15e04d8aac5200eb8779a94e
record_format	dspace
spelling	oai:doaj.org-article:0261c98c15e04d8aac5200eb8779a94e2021-11-25T18:26:25ZNephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color10.3390/min111112272075-163Xhttps://doaj.org/article/0261c98c15e04d8aac5200eb8779a94e2021-11-01T00:00:00Zhttps://www.mdpi.com/2075-163X/11/11/1227https://doaj.org/toc/2075-163XIn the Bazhenovskoye chrysotile–asbestos deposit (Middle Urals), nephrite bodies of the serpentinite type were found on the contact of after gabbro rodingites and serpentinites. The color is uniform to non-uniform, green to light green, bluish green, greyish green, and whitish. Spots, streaks, lenticules of bright bluish-green or, on the contrary, light green color are sometimes noted. The nephrite is mostly comprised of tremolite. Chromite decreases the quality of the ornamental stone, but it is replaced by chrome grossular, which gives the nephrite a brighter bluish-green color locally. Crushed grains of chromite contain increased concentrations of Zn and Mn. The quality of the nephrite is decreased by serpentine and talc, as well as by fractures due to drilling and blasting works. The specific feature of the nephrite in the Bazhenovskoye deposit is the formation of nickeline, maucherite, and uvarovite. The green color is associated with Fe<sup>2+</sup> ions. The nephrite of the Bazhenovskoye deposit meets the requirements for an ornamental stone. The origin of this nephrite includes a combination of metasomatic and metamorphic processes.Evgeniy V. KislovYuriy V. ErokhinMikhail P. PopovAnatoliy G. NikolayevMDPI AGarticlenephritemineralogyornamental stoneBazhenovskoye depositMineralogyQE351-399.2ENMinerals, Vol 11, Iss 1227, p 1227 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	nephrite mineralogy ornamental stone Bazhenovskoye deposit Mineralogy QE351-399.2
spellingShingle	nephrite mineralogy ornamental stone Bazhenovskoye deposit Mineralogy QE351-399.2 Evgeniy V. Kislov Yuriy V. Erokhin Mikhail P. Popov Anatoliy G. Nikolayev Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color
description	In the Bazhenovskoye chrysotile–asbestos deposit (Middle Urals), nephrite bodies of the serpentinite type were found on the contact of after gabbro rodingites and serpentinites. The color is uniform to non-uniform, green to light green, bluish green, greyish green, and whitish. Spots, streaks, lenticules of bright bluish-green or, on the contrary, light green color are sometimes noted. The nephrite is mostly comprised of tremolite. Chromite decreases the quality of the ornamental stone, but it is replaced by chrome grossular, which gives the nephrite a brighter bluish-green color locally. Crushed grains of chromite contain increased concentrations of Zn and Mn. The quality of the nephrite is decreased by serpentine and talc, as well as by fractures due to drilling and blasting works. The specific feature of the nephrite in the Bazhenovskoye deposit is the formation of nickeline, maucherite, and uvarovite. The green color is associated with Fe<sup>2+</sup> ions. The nephrite of the Bazhenovskoye deposit meets the requirements for an ornamental stone. The origin of this nephrite includes a combination of metasomatic and metamorphic processes.
format	article
author	Evgeniy V. Kislov Yuriy V. Erokhin Mikhail P. Popov Anatoliy G. Nikolayev
author_facet	Evgeniy V. Kislov Yuriy V. Erokhin Mikhail P. Popov Anatoliy G. Nikolayev
author_sort	Evgeniy V. Kislov
title	Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color
title_short	Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color
title_full	Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color
title_fullStr	Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color
title_full_unstemmed	Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color
title_sort	nephrite of bazhenovskoye chrysotile–asbestos deposit, middle urals: localization, mineral composition and color
publisher	MDPI AG
publishDate	2021
url	https://doaj.org/article/0261c98c15e04d8aac5200eb8779a94e
work_keys_str_mv	AT evgeniyvkislov nephriteofbazhenovskoyechrysotileasbestosdepositmiddleuralslocalizationmineralcompositionandcolor AT yuriyverokhin nephriteofbazhenovskoyechrysotileasbestosdepositmiddleuralslocalizationmineralcompositionandcolor AT mikhailppopov nephriteofbazhenovskoyechrysotileasbestosdepositmiddleuralslocalizationmineralcompositionandcolor AT anatoliygnikolayev nephriteofbazhenovskoyechrysotileasbestosdepositmiddleuralslocalizationmineralcompositionandcolor
_version_	1718411114923950080

Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color

Ejemplares similares