Isotope composition of greisen carbon deposits (Kalgutinsk deposit); Bulletin of the Tomsk Polytechnic University; Vol. 310, № 1

Bibliographic Details
Parent link:Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007
Vol. 310, № 1.— 2007.— [P. 16-20]
Main Author: Potseluev А. А.
Other Authors: Babkin D. I., Talibova А. G.
Summary:Заглавие с титульного листа
Электронная версия печатной публикации
Isotope composition of graphite carbon in the main industrial vein and near-vein greisens of the Kalgutinsk rare-metal deposit (Mountainous Altai) has been studied. Formation of graphite is connected with allocation of carbon during partial oxidation of primarily restored ore-forming metal-bearing fluid. The content of Сorg in a vein - 0,036 %, in greisens - 0,022 %. Carbon is characterized by «light» isotope composition, δ13Сorg in a vein-23,9, in greisens - 25,3 ‰. The «weighting» of the element upwards on revolt of the vein, which is explained by fluid evolution, is revealed. Regular fractionation of isotopes in the system vein - near-vein greisen is established. Isotope fractionation varies in vein's sections, differs by capacity and content of ore components. The conclusion is drawn on homogeneity and the deep nature of carbon.
Language:English
Published: 2007
Series:Earth science
Subjects:
Online Access:http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v310eng/i1/03.pdf
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=180469

MARC

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320 |a [Bibliography: p. 20 (19 titles)] 
330 |a Isotope composition of graphite carbon in the main industrial vein and near-vein greisens of the Kalgutinsk rare-metal deposit (Mountainous Altai) has been studied. Formation of graphite is connected with allocation of carbon during partial oxidation of primarily restored ore-forming metal-bearing fluid. The content of Сorg in a vein - 0,036 %, in greisens - 0,022 %. Carbon is characterized by «light» isotope composition, δ13Сorg in a vein-23,9, in greisens - 25,3 ‰. The «weighting» of the element upwards on revolt of the vein, which is explained by fluid evolution, is revealed. Regular fractionation of isotopes in the system vein - near-vein greisen is established. Isotope fractionation varies in vein's sections, differs by capacity and content of ore components. The conclusion is drawn on homogeneity and the deep nature of carbon. 
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463 1 |0 (RuTPU)RU\TPU\book\195457  |t Vol. 310, № 1  |v [P. 16-20]  |d 2007  |p 201 p. 
610 1 |a isotope composition 
610 1 |a carbon 
610 1 |a greisen deposits 
610 1 |a Kalgutinsk deposit 
610 1 |a graphites 
610 1 |a industrial veins 
610 1 |a near-vein greisen 
610 1 |a Mountainous Altai 
610 1 |a oxidation 
610 1 |a ore-forming fluid 
610 1 |a metal-bearing fluid 
610 1 |a fractionation 
610 1 |a isotopes 
610 1 |a capacity 
610 1 |a ore components 
610 1 |a homogeneity 
610 1 |a труды учёных ТПУ 
610 1 |a электронный ресурс 
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701 1 |a Talibova  |b А. G. 
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