Femic chemical elements in near-ore metasomatic haloes of the Kedrovskoye gold-ore deposit (the North Transbaikalia); Bulletin of the Tomsk Polytechnic University; Vol. 310, № 3

Dades bibliogràfiques
Parent link:Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007
Vol. 310, № 3.— 2007.— [P. 5-9]
Autor principal: Kucherenko I. V. Igor Vasilyevich
Sumari:Заглавие с титульного листа
Электронная версия печатной публикации
The results of studying geochemistry of phemophilous group in near-ore apogneiss and aposhale metasomatites of the Kedrovskoye mesothermal deposit in the North Tranbaikalia are presented. According to mineralogy-petrochemical data it was defined that metasomatic haloes belong to beresite metasomatic formation with propylite-like profile of transformations at the area periphery. Silica loss up to the half of its mass from the back zones was stated in the initial ores and conditions of this loss were determined. Silica removed from the ores served as a basis for formation of gold-bearing quartz veins. In the back zones of near-ore metasomatic haloes contrast anomalies of phosphorous, titanium, magnesium, manganese, iron, potassium and calcium were found. Femic orientation of gold-bearing metasomatites demonstrates the generation of metal-bearing fluids in mantle magmatic chambers.
Idioma:anglès
Publicat: 2007
Col·lecció:Earth science
Matèries:
Accés en línia:http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v310eng/i3/01.pdf
Format: MixedMaterials Electrònic Capítol de llibre
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=182047

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330 |a The results of studying geochemistry of phemophilous group in near-ore apogneiss and aposhale metasomatites of the Kedrovskoye mesothermal deposit in the North Tranbaikalia are presented. According to mineralogy-petrochemical data it was defined that metasomatic haloes belong to beresite metasomatic formation with propylite-like profile of transformations at the area periphery. Silica loss up to the half of its mass from the back zones was stated in the initial ores and conditions of this loss were determined. Silica removed from the ores served as a basis for formation of gold-bearing quartz veins. In the back zones of near-ore metasomatic haloes contrast anomalies of phosphorous, titanium, magnesium, manganese, iron, potassium and calcium were found. Femic orientation of gold-bearing metasomatites demonstrates the generation of metal-bearing fluids in mantle magmatic chambers. 
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463 1 |0 (RuTPU)RU\TPU\book\197326  |t Vol. 310, № 3  |v [P. 5-9]  |d 2007  |p 101 p. 
610 1 |a femic elements 
610 1 |a chemical elements 
610 1 |a near-ore haloes 
610 1 |a metasomatic haloes 
610 1 |a Kedrovskoye gold-ore deposit 
610 1 |a North Transbaikalia 
610 1 |a geochemistry 
610 1 |a aposhale metasomatites 
610 1 |a apogneiss metasomatites 
610 1 |a mineralogy-petrochemical data 
610 1 |a beresite formation 
610 1 |a metasomatic formation 
610 1 |a back zones 
610 1 |a silica 
610 1 |a masses 
610 1 |a initial ores 
610 1 |a loss up 
610 1 |a quartz veins 
610 1 |a gold-bearing veins 
610 1 |a anomalies 
610 1 |a phosphorous 
610 1 |a titanium 
610 1 |a magnesium 
610 1 |a manganese 
610 1 |a iron 
610 1 |a potassium 
610 1 |a calcium 
610 1 |a gold-bearing metasomatites 
610 1 |a generation 
610 1 |a metal-bearing fluids 
610 1 |a magmatic chambers 
610 1 |a mantle chambers 
610 1 |a труды учёных ТПУ 
610 1 |a электронный ресурс 
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700 1 |a Kucherenko  |b I. V.  |c Geologist  |c Professor and consultant of Tomsk Polytechnic University, Doctor of geological and mineralogical sciences  |f 1937-  |g Igor Vasilyevich  |2 stltpush  |3 (RuTPU)RU\TPU\pers\32569 
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