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Mineralogical and geochemical features of fluorite as indicators of rare-metal mineralization. / Panova, Y. G.

в: Geochemistry International, Том 32, № 12, 1995, стр. 34-47.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Panova, YG 1995, 'Mineralogical and geochemical features of fluorite as indicators of rare-metal mineralization', Geochemistry International, Том. 32, № 12, стр. 34-47.

APA

Panova, Y. G. (1995). Mineralogical and geochemical features of fluorite as indicators of rare-metal mineralization. Geochemistry International, 32(12), 34-47.

Vancouver

Panova YG. Mineralogical and geochemical features of fluorite as indicators of rare-metal mineralization. Geochemistry International. 1995;32(12):34-47.

Author

Panova, Y. G. / Mineralogical and geochemical features of fluorite as indicators of rare-metal mineralization. в: Geochemistry International. 1995 ; Том 32, № 12. стр. 34-47.

BibTeX

@article{75023164feab4bc3876e967c1c8fa418,
title = "Mineralogical and geochemical features of fluorite as indicators of rare-metal mineralization",
abstract = "The distributions of the REE and Mn2+ have been examined in fluorites formed in the preore, ore, and postore stages of the formation of greisen tin and tungsten deposits by quantitative spectral analysis, electron spin resonance, thermoluminescence, and photoluminescence. There are regular variations in the relative indicators of acidity and redox potential during the formation of tin and tungsten mineralization. Ranges in these parameters are proposed for classifying ore (relative to tin and tungsten) and barren associations and zones. -from Journal summary",
author = "Panova, {Y. G.}",
year = "1995",
language = "English",
volume = "32",
pages = "34--47",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "12",

}

RIS

TY - JOUR

T1 - Mineralogical and geochemical features of fluorite as indicators of rare-metal mineralization

AU - Panova, Y. G.

PY - 1995

Y1 - 1995

N2 - The distributions of the REE and Mn2+ have been examined in fluorites formed in the preore, ore, and postore stages of the formation of greisen tin and tungsten deposits by quantitative spectral analysis, electron spin resonance, thermoluminescence, and photoluminescence. There are regular variations in the relative indicators of acidity and redox potential during the formation of tin and tungsten mineralization. Ranges in these parameters are proposed for classifying ore (relative to tin and tungsten) and barren associations and zones. -from Journal summary

AB - The distributions of the REE and Mn2+ have been examined in fluorites formed in the preore, ore, and postore stages of the formation of greisen tin and tungsten deposits by quantitative spectral analysis, electron spin resonance, thermoluminescence, and photoluminescence. There are regular variations in the relative indicators of acidity and redox potential during the formation of tin and tungsten mineralization. Ranges in these parameters are proposed for classifying ore (relative to tin and tungsten) and barren associations and zones. -from Journal summary

UR - http://www.scopus.com/inward/record.url?scp=0029501246&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0029501246

VL - 32

SP - 34

EP - 47

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 12

ER -

ID: 93226627