Genesis of Precious Metal Mineralization in Intrusions of Ultramafic, Alkaline Rocks and Carbonatites in the North of the Siberian Platform; Minerals; Vol. 11, iss. 4

Dades bibliogràfiques
Parent link:Minerals
Vol. 11, iss. 4.— 2021.— [354, 21 p.]
Autor corporatiu: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Altres autors: Sazonov A. M. Anatoly Maksimovich, Romanovsky A. E. Aleksey, Gertner I. F., Zvyagina E. A. Elena Aleksandrovna, Krasnova T. S., Grinev O. M., Siljyanov S. A., Kolmakov Yu. V. Yuriy Viktorovich
Sumari:Title screen
The gold and platinum-group elements (PGE) mineralization of the Guli and Kresty intrusions was formed in the process of polyphase magmatism of the central type during the Permian and Triassic age. It is suggested that native osmium and iridium crystal nuclei were formed in the mantle at earlier high-temperature events of magma generation of the mantle substratum in the interval of 765–545 Ma and were brought by meimechite melts to the area of development of magmatic bodies. The pulsating magmatism of the later phases assisted in particle enlargement. Native gold was crystallized at a temperature of 415–200 °C at the hydrothermal-metasomatic stages of the meimechite, melilite, foidolite and carbonatite magmatism. The association of minerals of precious metals with oily, resinous and asphaltene bitumen testifies to the genetic relation of the mineralization to carbonaceous metasomatism. Identifying the carbonaceous gold and platinoid ore formation associated genetically with the parental formation of ultramafic, alkaline rocks and carbonatites is suggested.
Idioma:anglès
Publicat: 2021
Matèries:
Accés en línia:http://earchive.tpu.ru/handle/11683/73255
https://doi.org/10.3390/min11040354
Format: Electrònic Capítol de llibre
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=664943

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200 1 |a Genesis of Precious Metal Mineralization in Intrusions of Ultramafic, Alkaline Rocks and Carbonatites in the North of the Siberian Platform  |f A. M. Sazonov, A. E. Romanovsky, I. F. Gertner [et al.] 
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300 |a Title screen 
320 |a [References: 45 tit.] 
330 |a The gold and platinum-group elements (PGE) mineralization of the Guli and Kresty intrusions was formed in the process of polyphase magmatism of the central type during the Permian and Triassic age. It is suggested that native osmium and iridium crystal nuclei were formed in the mantle at earlier high-temperature events of magma generation of the mantle substratum in the interval of 765–545 Ma and were brought by meimechite melts to the area of development of magmatic bodies. The pulsating magmatism of the later phases assisted in particle enlargement. Native gold was crystallized at a temperature of 415–200 °C at the hydrothermal-metasomatic stages of the meimechite, melilite, foidolite and carbonatite magmatism. The association of minerals of precious metals with oily, resinous and asphaltene bitumen testifies to the genetic relation of the mineralization to carbonaceous metasomatism. Identifying the carbonaceous gold and platinoid ore formation associated genetically with the parental formation of ultramafic, alkaline rocks and carbonatites is suggested. 
461 |t Minerals 
463 |t Vol. 11, iss. 4  |v [354, 21 p.]  |d 2021 
610 1 |a электронный ресурс 
610 1 |a труды учёных ТПУ 
610 1 |a carbonaceous-Au-PGM ore formation 
610 1 |a ultramafic 
610 1 |a alkaline and carbonatite magmatism 
701 1 |a Sazonov  |b A. M.  |g Anatoly Maksimovich 
701 1 |a Romanovsky  |b A. E.  |g Aleksey 
701 1 |a Gertner  |b I. F. 
701 1 |a Zvyagina  |b E. A.  |g Elena Aleksandrovna 
701 1 |a Krasnova  |b T. S. 
701 1 |a Grinev  |b O. M. 
701 1 |a Siljyanov  |b S. A. 
701 1 |a Kolmakov  |b Yu. V.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences  |f 1966-  |g Yuriy Viktorovich  |3 (RuTPU)RU\TPU\pers\35859  |9 19002 
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