Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence
Varieties of quartz at silver occurrence Aid and silver veins of gold-rare metals deposit Ergelyah are studied. New data on the textures of comb quartz and earlier not documented the late coarse-grained quartz is presented; the IR- and X-ray luminescence spectra are analyzed. The transitions in grow...
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Sergo Ordzhonikidze Russian State University for Geological Prospecting
2015
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ftdoajarticles:oai:doaj.org/article:5ef06ea68c7349fa94b5006fe18865a5 2023-05-15T18:45:04+02:00 Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence O. A. Sustavov 2015-12-01T00:00:00Z https://doaj.org/article/5ef06ea68c7349fa94b5006fe18865a5 RU rus Sergo Ordzhonikidze Russian State University for Geological Prospecting https://www.geology-mgri.ru/jour/article/view/87 https://doaj.org/toc/0016-7762 https://doaj.org/toc/2618-8708 0016-7762 2618-8708 https://doaj.org/article/5ef06ea68c7349fa94b5006fe18865a5 Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 6, Pp 45-49 (2015) восточная якутия серебряное оруденение гребенчатый кварц расщепление кварца инфракрасные спектры кварца рентгенолюминесценция кварца Geology QE1-996.5 article 2015 ftdoajarticles 2023-03-19T01:40:30Z Varieties of quartz at silver occurrence Aid and silver veins of gold-rare metals deposit Ergelyah are studied. New data on the textures of comb quartz and earlier not documented the late coarse-grained quartz is presented; the IR- and X-ray luminescence spectra are analyzed. The transitions in growth process of comb quartz from the nearselvedge small unsplit crystals to wider split parts of the individuals, elongated along the c-axis, and then to transparent heads of crystals is considered. The formation of transparent heads of comb quartz crystals is replaced by crystallization of coarse-grained unsplit faintly smoky quartz, filling the axial parts of veins. The OH (Li) absorption band is typical in the IR-spectmm of comb quartz, which is usual to radiation citrine quartz, and the X-ray luminescence is in the field of 390-415 nm. Later unsplit coarse-grained quartz is characterized by the absence of OH (Li) absorption band in the IR-spectmm, and X-ray luminescence in the field of 530-535 nm. Article in Journal/Newspaper Yakutia Якути* Якутия Directory of Open Access Journals: DOAJ Articles |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
восточная якутия серебряное оруденение гребенчатый кварц расщепление кварца инфракрасные спектры кварца рентгенолюминесценция кварца Geology QE1-996.5 |
spellingShingle |
восточная якутия серебряное оруденение гребенчатый кварц расщепление кварца инфракрасные спектры кварца рентгенолюминесценция кварца Geology QE1-996.5 O. A. Sustavov Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence |
topic_facet |
восточная якутия серебряное оруденение гребенчатый кварц расщепление кварца инфракрасные спектры кварца рентгенолюминесценция кварца Geology QE1-996.5 |
description |
Varieties of quartz at silver occurrence Aid and silver veins of gold-rare metals deposit Ergelyah are studied. New data on the textures of comb quartz and earlier not documented the late coarse-grained quartz is presented; the IR- and X-ray luminescence spectra are analyzed. The transitions in growth process of comb quartz from the nearselvedge small unsplit crystals to wider split parts of the individuals, elongated along the c-axis, and then to transparent heads of crystals is considered. The formation of transparent heads of comb quartz crystals is replaced by crystallization of coarse-grained unsplit faintly smoky quartz, filling the axial parts of veins. The OH (Li) absorption band is typical in the IR-spectmm of comb quartz, which is usual to radiation citrine quartz, and the X-ray luminescence is in the field of 390-415 nm. Later unsplit coarse-grained quartz is characterized by the absence of OH (Li) absorption band in the IR-spectmm, and X-ray luminescence in the field of 530-535 nm. |
format |
Article in Journal/Newspaper |
author |
O. A. Sustavov |
author_facet |
O. A. Sustavov |
author_sort |
O. A. Sustavov |
title |
Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence |
title_short |
Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence |
title_full |
Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence |
title_fullStr |
Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence |
title_full_unstemmed |
Some varieties of quartz at the epithermal silver occurrences of Tas-Kystabyt magmatic belt (Yakutia): textures, IR-spectra, X-ray luminescence |
title_sort |
some varieties of quartz at the epithermal silver occurrences of tas-kystabyt magmatic belt (yakutia): textures, ir-spectra, x-ray luminescence |
publisher |
Sergo Ordzhonikidze Russian State University for Geological Prospecting |
publishDate |
2015 |
url |
https://doaj.org/article/5ef06ea68c7349fa94b5006fe18865a5 |
genre |
Yakutia Якути* Якутия |
genre_facet |
Yakutia Якути* Якутия |
op_source |
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 6, Pp 45-49 (2015) |
op_relation |
https://www.geology-mgri.ru/jour/article/view/87 https://doaj.org/toc/0016-7762 https://doaj.org/toc/2618-8708 0016-7762 2618-8708 https://doaj.org/article/5ef06ea68c7349fa94b5006fe18865a5 |
_version_ |
1766236012857524224 |