Standard

Chemical evolution of metasomatites in the formation of the Pravourmi tin deposit. / Panova, Y. G.; Gavrilenko, V. V.; Luchitskaya, M. I.

в: Geochemistry International, Том 30, № 12, 1993, стр. 130-139.

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

Harvard

Panova, YG, Gavrilenko, VV & Luchitskaya, MI 1993, 'Chemical evolution of metasomatites in the formation of the Pravourmi tin deposit', Geochemistry International, Том. 30, № 12, стр. 130-139.

APA

Panova, Y. G., Gavrilenko, V. V., & Luchitskaya, M. I. (1993). Chemical evolution of metasomatites in the formation of the Pravourmi tin deposit. Geochemistry International, 30(12), 130-139.

Vancouver

Panova YG, Gavrilenko VV, Luchitskaya MI. Chemical evolution of metasomatites in the formation of the Pravourmi tin deposit. Geochemistry International. 1993;30(12):130-139.

Author

Panova, Y. G. ; Gavrilenko, V. V. ; Luchitskaya, M. I. / Chemical evolution of metasomatites in the formation of the Pravourmi tin deposit. в: Geochemistry International. 1993 ; Том 30, № 12. стр. 130-139.

BibTeX

@article{5731b968cf564fd3b3ee940bda1c3fa8,
title = "Chemical evolution of metasomatites in the formation of the Pravourmi tin deposit",
abstract = "Hydrothermal metasomatites usually accompany all stages in the formation of greisen deposits. The products of the metasomatic reworking of the country rocks in the pre-ore, syn-ore, and post-ore stages provide important information on the hydrothermal processes. The Pravourmi displays a complicated combination of mineral assemblages, which are usually characteristic of tin-bearing objects in various associations, so it is particularly important to examine the mineralogy and geochemistry of the metasomatites from the various stages of mineralization. The paper examines the element assemblages and the type features of certain minerals in the successive metasomatic products. -from Journal summary",
author = "Panova, {Y. G.} and Gavrilenko, {V. V.} and Luchitskaya, {M. I.}",
year = "1993",
language = "English",
volume = "30",
pages = "130--139",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "12",

}

RIS

TY - JOUR

T1 - Chemical evolution of metasomatites in the formation of the Pravourmi tin deposit

AU - Panova, Y. G.

AU - Gavrilenko, V. V.

AU - Luchitskaya, M. I.

PY - 1993

Y1 - 1993

N2 - Hydrothermal metasomatites usually accompany all stages in the formation of greisen deposits. The products of the metasomatic reworking of the country rocks in the pre-ore, syn-ore, and post-ore stages provide important information on the hydrothermal processes. The Pravourmi displays a complicated combination of mineral assemblages, which are usually characteristic of tin-bearing objects in various associations, so it is particularly important to examine the mineralogy and geochemistry of the metasomatites from the various stages of mineralization. The paper examines the element assemblages and the type features of certain minerals in the successive metasomatic products. -from Journal summary

AB - Hydrothermal metasomatites usually accompany all stages in the formation of greisen deposits. The products of the metasomatic reworking of the country rocks in the pre-ore, syn-ore, and post-ore stages provide important information on the hydrothermal processes. The Pravourmi displays a complicated combination of mineral assemblages, which are usually characteristic of tin-bearing objects in various associations, so it is particularly important to examine the mineralogy and geochemistry of the metasomatites from the various stages of mineralization. The paper examines the element assemblages and the type features of certain minerals in the successive metasomatic products. -from Journal summary

UR - http://www.scopus.com/inward/record.url?scp=0027801338&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0027801338

VL - 30

SP - 130

EP - 139

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 12

ER -

ID: 93226718